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	<id>https://soil.evs.buffalo.edu/api.php?action=feedcontributions&amp;feedformat=atom&amp;user=Elsbethd</id>
	<title>Soil Ecology Wiki - User contributions [en]</title>
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	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=3144</id>
		<title>Silt</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=3144"/>
		<updated>2018-05-18T10:40:34Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: /* Field Identification */&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;[[File:Silty.jpg|thumb|right|Silt [6]]]&lt;br /&gt;
&lt;br /&gt;
==Definition==&lt;br /&gt;
&lt;br /&gt;
Silt is a granular sediment that can be transported and deposited by water, ice, and wind. Silt particles are larger than clay, but smaller than sand. To be classified as silt, a particle must be between .002 to .05 mm [1]. Similarly to [[clay]], sand, and gravel, silt is found in [[soil]]. Silt can also occur as sediment mixed in suspension with water. Because of silt’s spherical shape, it retains a large amount of water. Silty soil is known to be more fertile than other soils, and many species of [[organisms]] thrive in it.&lt;br /&gt;
&lt;br /&gt;
[[File:loess.jpg|thumb|left|Loess [7]]]&lt;br /&gt;
==Formation==&lt;br /&gt;
&lt;br /&gt;
Silt-producing mechanisms include frost shattering (Freeze-Thaw Weathering), comminution during transport, eolian abrasion, salt weathering, and glacial grinding. Windblown silt blankets the land in many parts of the world [2]. Large deposits of silt, such as this, are known as loess. Loess landscapes are usually a sign of past glacial activity, including areas such as the Great Plains. Silt can accumulate quickly in areas that lack vegetation, which can disrupt ecosystems. Silt also settles in still water, resulting in build ups like deltas. The main mineral origin of silt is quartz and feldspar [3]. The formation and movement of silt are constantly altering ecosystems. &lt;br /&gt;
&lt;br /&gt;
==Identification==&lt;br /&gt;
&lt;br /&gt;
Silt soil is fine and feels like flour when dry. When silt is wet it becomes a smooth mud that can be easily molded into shapes. When silt soil is very wet, it blends seamlessly with water, and forms puddles of mud [4]. Silt particles are very small, so they have a very smooth [[soil texture]]. Silty soil drains well, but not as quickly as sand. Silts sparkly appearance can be observed using a hand lens. Pure silts are identified by their lack of cohesion. Silts and clays are distinguished by their plasticity [5].&lt;br /&gt;
&lt;br /&gt;
==Field Identification==&lt;br /&gt;
&lt;br /&gt;
*Dry Strength Test&lt;br /&gt;
&lt;br /&gt;
Mold a small briquette of the soil and allow to dry in the air. Break a small fragment about 1.0 cm in size and press between thumb and forefinger. The effort required to break the fragment provides a basis for describing the strength as ver low, low, medium, high or very high. A silt fragment crushes easily.&lt;br /&gt;
&lt;br /&gt;
*Dilatancy or Shaking Test&lt;br /&gt;
&lt;br /&gt;
Silts are considerably more permeable than clays. A small amount of soil is mixed with water to a very soft consistency in the palm of the hand. The back of the hand is then lightly tapped. If the soil is silty, water rises quickly to its surface and gives it a shiny or glistening appearance. Then if the soil pat is deformed, in some instances by squeezing and in others by stretching, the water flows back into it and leaves the surface with a dull appearance. The reaction is described as rapid, slow or none.&lt;br /&gt;
&lt;br /&gt;
*Roughness/Plasticity Test&lt;br /&gt;
&lt;br /&gt;
Silt can seldom be rolled into a thread with a diameter as small as 3mm without severe cracking, and lacks tensile strength. A simple plasticity test should indicate whether a plastic thread can be formed, and also the toughness of the thread as it nears the crumbling stage. This condition is described as weak and friable, medium, or tough.&lt;br /&gt;
&lt;br /&gt;
*Dispersion Test&lt;br /&gt;
&lt;br /&gt;
A small quantity of the soil is put in water in a glass cylinder or test tube and then allowed to settle. The coarser particles fall out first and the finest particles remain in suspension the longest. Materials of silt size settles in 15 to 60 min. [7]&lt;br /&gt;
&lt;br /&gt;
[[File:soilmodel.jpg|thumb|right|[8]]]&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
&lt;br /&gt;
*[[Clay]]&lt;br /&gt;
*[[Loam]]&lt;br /&gt;
*[[Founders of Soil Concepts]]&lt;br /&gt;
*[[Humus]]&lt;br /&gt;
*[[Microorganisms]]&lt;br /&gt;
*[[Pedogenesis]]&lt;br /&gt;
*[[Soil]]&lt;br /&gt;
*[[Soil Textures]]&lt;br /&gt;
*[[Soil Properties]] &lt;br /&gt;
*[[Jenny Equation]]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
National Geographic Society. “Silt.” National Geographic Society, 9 Oct. 2012, www.nationalgeographic.org/encyclopedia/silt/.&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
Wright, Janet S. &amp;quot;“Desert” loess versus “glacial” loess: quartz silt formation, source areas and sediment pathways in the formation of loess deposits.&amp;quot; Geomorphology 36.3-4 (2001): 231-256.&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
Wright, J. S., Smith, B. J. &amp;amp; Whalley, W. B. Mechanisms of loess-sized quartz silt production and their relative effectiveness: Laboratory simulations. Geomorphology 23, 15-34 (1998).&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
Wentworth, Chester K. &amp;quot;A scale of grade and class terms for clastic sediments.&amp;quot; The journal of geology 30.5 (1922): 377-392.&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
NRCS, USDA. &amp;quot;National soil survey handbook, title 430-VI.&amp;quot; (2007).&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
“Silt: Environmental Impact.” Rashid&#039;s Blog: An Educational Portal, 8 May 2016, rashidfaridi.com/2016/03/04/silt-environmental-impact/.&lt;br /&gt;
&lt;br /&gt;
[7]&lt;br /&gt;
“Loess Hills.” Iowa Geological Survey, 11 July 2017, www.iihr.uiowa.edu/igs/loess-hills/?doing_wp_cron=1525843720.4534800052642822265625.&lt;br /&gt;
&lt;br /&gt;
[8]&lt;br /&gt;
“Choosing a Topsoil Mix for Your Yard or Garden.” Washington Rock Quarries, 23 Mar. 2017, www.wa-rock.com/choosing-topsoil-mix-yard-garden/.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=3143</id>
		<title>Silt</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=3143"/>
		<updated>2018-05-18T10:39:25Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: /* Field Identification */&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;[[File:Silty.jpg|thumb|right|Silt [6]]]&lt;br /&gt;
&lt;br /&gt;
==Definition==&lt;br /&gt;
&lt;br /&gt;
Silt is a granular sediment that can be transported and deposited by water, ice, and wind. Silt particles are larger than clay, but smaller than sand. To be classified as silt, a particle must be between .002 to .05 mm [1]. Similarly to [[clay]], sand, and gravel, silt is found in [[soil]]. Silt can also occur as sediment mixed in suspension with water. Because of silt’s spherical shape, it retains a large amount of water. Silty soil is known to be more fertile than other soils, and many species of [[organisms]] thrive in it.&lt;br /&gt;
&lt;br /&gt;
[[File:loess.jpg|thumb|left|Loess [7]]]&lt;br /&gt;
==Formation==&lt;br /&gt;
&lt;br /&gt;
Silt-producing mechanisms include frost shattering (Freeze-Thaw Weathering), comminution during transport, eolian abrasion, salt weathering, and glacial grinding. Windblown silt blankets the land in many parts of the world [2]. Large deposits of silt, such as this, are known as loess. Loess landscapes are usually a sign of past glacial activity, including areas such as the Great Plains. Silt can accumulate quickly in areas that lack vegetation, which can disrupt ecosystems. Silt also settles in still water, resulting in build ups like deltas. The main mineral origin of silt is quartz and feldspar [3]. The formation and movement of silt are constantly altering ecosystems. &lt;br /&gt;
&lt;br /&gt;
==Identification==&lt;br /&gt;
&lt;br /&gt;
Silt soil is fine and feels like flour when dry. When silt is wet it becomes a smooth mud that can be easily molded into shapes. When silt soil is very wet, it blends seamlessly with water, and forms puddles of mud [4]. Silt particles are very small, so they have a very smooth [[soil texture]]. Silty soil drains well, but not as quickly as sand. Silts sparkly appearance can be observed using a hand lens. Pure silts are identified by their lack of cohesion. Silts and clays are distinguished by their plasticity [5].&lt;br /&gt;
&lt;br /&gt;
==Field Identification==&lt;br /&gt;
&lt;br /&gt;
*Dry Strength Test&lt;br /&gt;
&lt;br /&gt;
Mold a small briquette of the soil and allow to dry in the air. Break a small fragment about 1.0 cm in size and press between thumb and forefinger. The effort required to break the fragment provides a basis for describing the strength as ver low, low, medium, high or very high. A silt fragment crushes easily.&lt;br /&gt;
&lt;br /&gt;
*Dilatancy or Shaking Test&lt;br /&gt;
&lt;br /&gt;
Silts are considerably more permeable than clays. A small amount of soil is mixed with water to a very soft consistency in the palm of the hand. The back of the hand is then lightly tapped. If the soil is silty, water rises quickly to its surface and gives it a shiny or glistening appearance. Then if the soil pat is deformed, in some instances by squeezing and in others by stretching, the water flows back into it and leaves the surface with a dull appearance. The reaction is described as rapid, slow or none.&lt;br /&gt;
&lt;br /&gt;
*Roughness/Plasticity Test&lt;br /&gt;
&lt;br /&gt;
Silt can seldom be rolled into a thread with a diameter as small as 3mm without severe cracking, and lacks tensile strength. A simple plasticity test should indicate whether a plastic thread can be formed, and also the toughness of the thread as it nears the crumbling stage. This condition is described as weak and friable, medium, or tough.&lt;br /&gt;
&lt;br /&gt;
*Dispersion Test&lt;br /&gt;
&lt;br /&gt;
A small quantity of the soil is put in water in a glass cylinder or test tube and then allowed to settle. The coarser particles fall out first and the finest particles remain in suspension the longest. Materials of silt size settles in 15 to 60 min. &lt;br /&gt;
&lt;br /&gt;
[[File:soilmodel.jpg|thumb|right|[8]]]&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
&lt;br /&gt;
*[[Clay]]&lt;br /&gt;
*[[Loam]]&lt;br /&gt;
*[[Founders of Soil Concepts]]&lt;br /&gt;
*[[Humus]]&lt;br /&gt;
*[[Microorganisms]]&lt;br /&gt;
*[[Pedogenesis]]&lt;br /&gt;
*[[Soil]]&lt;br /&gt;
*[[Soil Textures]]&lt;br /&gt;
*[[Soil Properties]] &lt;br /&gt;
*[[Jenny Equation]]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
National Geographic Society. “Silt.” National Geographic Society, 9 Oct. 2012, www.nationalgeographic.org/encyclopedia/silt/.&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
Wright, Janet S. &amp;quot;“Desert” loess versus “glacial” loess: quartz silt formation, source areas and sediment pathways in the formation of loess deposits.&amp;quot; Geomorphology 36.3-4 (2001): 231-256.&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
Wright, J. S., Smith, B. J. &amp;amp; Whalley, W. B. Mechanisms of loess-sized quartz silt production and their relative effectiveness: Laboratory simulations. Geomorphology 23, 15-34 (1998).&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
Wentworth, Chester K. &amp;quot;A scale of grade and class terms for clastic sediments.&amp;quot; The journal of geology 30.5 (1922): 377-392.&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
NRCS, USDA. &amp;quot;National soil survey handbook, title 430-VI.&amp;quot; (2007).&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
“Silt: Environmental Impact.” Rashid&#039;s Blog: An Educational Portal, 8 May 2016, rashidfaridi.com/2016/03/04/silt-environmental-impact/.&lt;br /&gt;
&lt;br /&gt;
[7]&lt;br /&gt;
“Loess Hills.” Iowa Geological Survey, 11 July 2017, www.iihr.uiowa.edu/igs/loess-hills/?doing_wp_cron=1525843720.4534800052642822265625.&lt;br /&gt;
&lt;br /&gt;
[8]&lt;br /&gt;
“Choosing a Topsoil Mix for Your Yard or Garden.” Washington Rock Quarries, 23 Mar. 2017, www.wa-rock.com/choosing-topsoil-mix-yard-garden/.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=3142</id>
		<title>Silt</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=3142"/>
		<updated>2018-05-18T10:39:02Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;[[File:Silty.jpg|thumb|right|Silt [6]]]&lt;br /&gt;
&lt;br /&gt;
==Definition==&lt;br /&gt;
&lt;br /&gt;
Silt is a granular sediment that can be transported and deposited by water, ice, and wind. Silt particles are larger than clay, but smaller than sand. To be classified as silt, a particle must be between .002 to .05 mm [1]. Similarly to [[clay]], sand, and gravel, silt is found in [[soil]]. Silt can also occur as sediment mixed in suspension with water. Because of silt’s spherical shape, it retains a large amount of water. Silty soil is known to be more fertile than other soils, and many species of [[organisms]] thrive in it.&lt;br /&gt;
&lt;br /&gt;
[[File:loess.jpg|thumb|left|Loess [7]]]&lt;br /&gt;
==Formation==&lt;br /&gt;
&lt;br /&gt;
Silt-producing mechanisms include frost shattering (Freeze-Thaw Weathering), comminution during transport, eolian abrasion, salt weathering, and glacial grinding. Windblown silt blankets the land in many parts of the world [2]. Large deposits of silt, such as this, are known as loess. Loess landscapes are usually a sign of past glacial activity, including areas such as the Great Plains. Silt can accumulate quickly in areas that lack vegetation, which can disrupt ecosystems. Silt also settles in still water, resulting in build ups like deltas. The main mineral origin of silt is quartz and feldspar [3]. The formation and movement of silt are constantly altering ecosystems. &lt;br /&gt;
&lt;br /&gt;
==Identification==&lt;br /&gt;
&lt;br /&gt;
Silt soil is fine and feels like flour when dry. When silt is wet it becomes a smooth mud that can be easily molded into shapes. When silt soil is very wet, it blends seamlessly with water, and forms puddles of mud [4]. Silt particles are very small, so they have a very smooth [[soil texture]]. Silty soil drains well, but not as quickly as sand. Silts sparkly appearance can be observed using a hand lens. Pure silts are identified by their lack of cohesion. Silts and clays are distinguished by their plasticity [5].&lt;br /&gt;
&lt;br /&gt;
==Field Identification==&lt;br /&gt;
&lt;br /&gt;
Dry Strength Test&lt;br /&gt;
&lt;br /&gt;
Mold a small briquette of the soil and allow to dry in the air. Break a small fragment about 1.0 cm in size and press between thumb and forefinger. The effort required to break the fragment provides a basis for describing the strength as ver low, low, medium, high or very high. A silt fragment crushes easily.&lt;br /&gt;
&lt;br /&gt;
Dilatancy or Shaking Test&lt;br /&gt;
&lt;br /&gt;
Silts are considerably more permeable than clays. A small amount of soil is mixed with water to a very soft consistency in the palm of the hand. The back of the hand is then lightly tapped. If the soil is silty, water rises quickly to its surface and gives it a shiny or glistening appearance. Then if the soil pat is deformed, in some instances by squeezing and in others by stretching, the water flows back into it and leaves the surface with a dull appearance. The reaction is described as rapid, slow or none.&lt;br /&gt;
&lt;br /&gt;
Roughness/Plasticity Test&lt;br /&gt;
&lt;br /&gt;
Silt can seldom be rolled into a thread with a diameter as small as 3mm without severe cracking, and lacks tensile strength. A simple plasticity test should indicate whether a plastic thread can be formed, and also the toughness of the thread as it nears the crumbling stage. This condition is described as weak and friable, medium, or tough.&lt;br /&gt;
&lt;br /&gt;
Dispersion Test&lt;br /&gt;
&lt;br /&gt;
A small quantity of the soil is put in water in a glass cylinder or test tube and then allowed to settle. The coarser particles fall out first and the finest particles remain in suspension the longest. Materials of silt size settles in 15 to 60 min. &lt;br /&gt;
&lt;br /&gt;
[[File:soilmodel.jpg|thumb|right|[8]]]&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
&lt;br /&gt;
*[[Clay]]&lt;br /&gt;
*[[Loam]]&lt;br /&gt;
*[[Founders of Soil Concepts]]&lt;br /&gt;
*[[Humus]]&lt;br /&gt;
*[[Microorganisms]]&lt;br /&gt;
*[[Pedogenesis]]&lt;br /&gt;
*[[Soil]]&lt;br /&gt;
*[[Soil Textures]]&lt;br /&gt;
*[[Soil Properties]] &lt;br /&gt;
*[[Jenny Equation]]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
National Geographic Society. “Silt.” National Geographic Society, 9 Oct. 2012, www.nationalgeographic.org/encyclopedia/silt/.&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
Wright, Janet S. &amp;quot;“Desert” loess versus “glacial” loess: quartz silt formation, source areas and sediment pathways in the formation of loess deposits.&amp;quot; Geomorphology 36.3-4 (2001): 231-256.&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
Wright, J. S., Smith, B. J. &amp;amp; Whalley, W. B. Mechanisms of loess-sized quartz silt production and their relative effectiveness: Laboratory simulations. Geomorphology 23, 15-34 (1998).&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
Wentworth, Chester K. &amp;quot;A scale of grade and class terms for clastic sediments.&amp;quot; The journal of geology 30.5 (1922): 377-392.&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
NRCS, USDA. &amp;quot;National soil survey handbook, title 430-VI.&amp;quot; (2007).&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
“Silt: Environmental Impact.” Rashid&#039;s Blog: An Educational Portal, 8 May 2016, rashidfaridi.com/2016/03/04/silt-environmental-impact/.&lt;br /&gt;
&lt;br /&gt;
[7]&lt;br /&gt;
“Loess Hills.” Iowa Geological Survey, 11 July 2017, www.iihr.uiowa.edu/igs/loess-hills/?doing_wp_cron=1525843720.4534800052642822265625.&lt;br /&gt;
&lt;br /&gt;
[8]&lt;br /&gt;
“Choosing a Topsoil Mix for Your Yard or Garden.” Washington Rock Quarries, 23 Mar. 2017, www.wa-rock.com/choosing-topsoil-mix-yard-garden/.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=3141</id>
		<title>Silt</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=3141"/>
		<updated>2018-05-18T10:38:00Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: /* Field Identification */&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;[[File:Silty.jpg|thumb|right|Silt [6]]]&lt;br /&gt;
&lt;br /&gt;
==Definition==&lt;br /&gt;
&lt;br /&gt;
Silt is a granular sediment that can be transported and deposited by water, ice, and wind. Silt particles are larger than clay, but smaller than sand. To be classified as silt, a particle must be between .002 to .05 mm [1]. Similarly to [[clay]], sand, and gravel, silt is found in [[soil]]. Silt can also occur as sediment mixed in suspension with water. Because of silt’s spherical shape, it retains a large amount of water. Silty soil is known to be more fertile than other soils, and many species of [[organisms]] thrive in it.&lt;br /&gt;
&lt;br /&gt;
[[File:loess.jpg|thumb|left|Loess [7]]]&lt;br /&gt;
==Formation==&lt;br /&gt;
&lt;br /&gt;
Silt-producing mechanisms include frost shattering (Freeze-Thaw Weathering), comminution during transport, eolian abrasion, salt weathering, and glacial grinding. Windblown silt blankets the land in many parts of the world [2]. Large deposits of silt, such as this, are known as loess. Loess landscapes are usually a sign of past glacial activity, including areas such as the Great Plains. Silt can accumulate quickly in areas that lack vegetation, which can disrupt ecosystems. Silt also settles in still water, resulting in build ups like deltas. The main mineral origin of silt is quartz and feldspar [3]. The formation and movement of silt are constantly altering ecosystems. &lt;br /&gt;
&lt;br /&gt;
==Identification==&lt;br /&gt;
&lt;br /&gt;
Silt soil is fine and feels like flour when dry. When silt is wet it becomes a smooth mud that can be easily molded into shapes. When silt soil is very wet, it blends seamlessly with water, and forms puddles of mud [4]. Silt particles are very small, so they have a very smooth [[soil texture]]. Silty soil drains well, but not as quickly as sand. Silts sparkly appearance can be observed using a hand lens. Pure silts are identified by their lack of cohesion. Silts and clays are distinguished by their plasticity [5].&lt;br /&gt;
&lt;br /&gt;
==Field Identification==&lt;br /&gt;
&lt;br /&gt;
=Dry Strength Test=&lt;br /&gt;
&lt;br /&gt;
Mold a small briquette of the soil and allow to dry in the air. Break a small fragment about 1.0 cm in size and press between thumb and forefinger. The effort required to break the fragment provides a basis for describing the strength as ver low, low, medium, high or very high. A silt fragment crushes easily.&lt;br /&gt;
&lt;br /&gt;
=Dilatancy or Shaking Test=&lt;br /&gt;
&lt;br /&gt;
Silts are considerably more permeable than clays. A small amount of soil is mixed with water to a very soft consistency in the palm of the hand. The back of the hand is then lightly tapped. If the soil is silty, water rises quickly to its surface and gives it a shiny or glistening appearance. Then if the soil pat is deformed, in some instances by squeezing and in others by stretching, the water flows back into it and leaves the surface with a dull appearance. The reaction is described as rapid, slow or none.&lt;br /&gt;
&lt;br /&gt;
=Roughness/Plasticity Test=&lt;br /&gt;
&lt;br /&gt;
Silt can seldom be rolled into a thread with a diameter as small as 3mm without severe cracking, and lacks tensile strength. A simple plasticity test should indicate whether a plastic thread can be formed, and also the toughness of the thread as it nears the crumbling stage. This condition is described as weak and friable, medium, or tough.&lt;br /&gt;
&lt;br /&gt;
=Dispersion Test=&lt;br /&gt;
&lt;br /&gt;
A small quantity of the soil is put in water in a glass cylinder or test tube and then allowed to settle. The coarser particles fall out first and the finest particles remain in suspension the longest. Materials of silt size settles in 15 to 60 min. &lt;br /&gt;
&lt;br /&gt;
[[File:soilmodel.jpg|thumb|right|[8]]]&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
&lt;br /&gt;
*[[Clay]]&lt;br /&gt;
*[[Loam]]&lt;br /&gt;
*[[Founders of Soil Concepts]]&lt;br /&gt;
*[[Humus]]&lt;br /&gt;
*[[Microorganisms]]&lt;br /&gt;
*[[Pedogenesis]]&lt;br /&gt;
*[[Soil]]&lt;br /&gt;
*[[Soil Textures]]&lt;br /&gt;
*[[Soil Properties]] &lt;br /&gt;
*[[Jenny Equation]]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
National Geographic Society. “Silt.” National Geographic Society, 9 Oct. 2012, www.nationalgeographic.org/encyclopedia/silt/.&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
Wright, Janet S. &amp;quot;“Desert” loess versus “glacial” loess: quartz silt formation, source areas and sediment pathways in the formation of loess deposits.&amp;quot; Geomorphology 36.3-4 (2001): 231-256.&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
Wright, J. S., Smith, B. J. &amp;amp; Whalley, W. B. Mechanisms of loess-sized quartz silt production and their relative effectiveness: Laboratory simulations. Geomorphology 23, 15-34 (1998).&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
Wentworth, Chester K. &amp;quot;A scale of grade and class terms for clastic sediments.&amp;quot; The journal of geology 30.5 (1922): 377-392.&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
NRCS, USDA. &amp;quot;National soil survey handbook, title 430-VI.&amp;quot; (2007).&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
“Silt: Environmental Impact.” Rashid&#039;s Blog: An Educational Portal, 8 May 2016, rashidfaridi.com/2016/03/04/silt-environmental-impact/.&lt;br /&gt;
&lt;br /&gt;
[7]&lt;br /&gt;
“Loess Hills.” Iowa Geological Survey, 11 July 2017, www.iihr.uiowa.edu/igs/loess-hills/?doing_wp_cron=1525843720.4534800052642822265625.&lt;br /&gt;
&lt;br /&gt;
[8]&lt;br /&gt;
“Choosing a Topsoil Mix for Your Yard or Garden.” Washington Rock Quarries, 23 Mar. 2017, www.wa-rock.com/choosing-topsoil-mix-yard-garden/.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=3140</id>
		<title>Silt</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=3140"/>
		<updated>2018-05-18T10:28:59Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;[[File:Silty.jpg|thumb|right|Silt [6]]]&lt;br /&gt;
&lt;br /&gt;
==Definition==&lt;br /&gt;
&lt;br /&gt;
Silt is a granular sediment that can be transported and deposited by water, ice, and wind. Silt particles are larger than clay, but smaller than sand. To be classified as silt, a particle must be between .002 to .05 mm [1]. Similarly to [[clay]], sand, and gravel, silt is found in [[soil]]. Silt can also occur as sediment mixed in suspension with water. Because of silt’s spherical shape, it retains a large amount of water. Silty soil is known to be more fertile than other soils, and many species of [[organisms]] thrive in it.&lt;br /&gt;
&lt;br /&gt;
[[File:loess.jpg|thumb|left|Loess [7]]]&lt;br /&gt;
==Formation==&lt;br /&gt;
&lt;br /&gt;
Silt-producing mechanisms include frost shattering (Freeze-Thaw Weathering), comminution during transport, eolian abrasion, salt weathering, and glacial grinding. Windblown silt blankets the land in many parts of the world [2]. Large deposits of silt, such as this, are known as loess. Loess landscapes are usually a sign of past glacial activity, including areas such as the Great Plains. Silt can accumulate quickly in areas that lack vegetation, which can disrupt ecosystems. Silt also settles in still water, resulting in build ups like deltas. The main mineral origin of silt is quartz and feldspar [3]. The formation and movement of silt are constantly altering ecosystems. &lt;br /&gt;
&lt;br /&gt;
==Identification==&lt;br /&gt;
&lt;br /&gt;
Silt soil is fine and feels like flour when dry. When silt is wet it becomes a smooth mud that can be easily molded into shapes. When silt soil is very wet, it blends seamlessly with water, and forms puddles of mud [4]. Silt particles are very small, so they have a very smooth [[soil texture]]. Silty soil drains well, but not as quickly as sand. Silts sparkly appearance can be observed using a hand lens. Pure silts are identified by their lack of cohesion. Silts and clays are distinguished by their plasticity [5].&lt;br /&gt;
&lt;br /&gt;
==Field Identification==&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
[[File:soilmodel.jpg|thumb|right|[8]]]&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
&lt;br /&gt;
*[[Clay]]&lt;br /&gt;
*[[Loam]]&lt;br /&gt;
*[[Founders of Soil Concepts]]&lt;br /&gt;
*[[Humus]]&lt;br /&gt;
*[[Microorganisms]]&lt;br /&gt;
*[[Pedogenesis]]&lt;br /&gt;
*[[Soil]]&lt;br /&gt;
*[[Soil Textures]]&lt;br /&gt;
*[[Soil Properties]] &lt;br /&gt;
*[[Jenny Equation]]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
National Geographic Society. “Silt.” National Geographic Society, 9 Oct. 2012, www.nationalgeographic.org/encyclopedia/silt/.&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
Wright, Janet S. &amp;quot;“Desert” loess versus “glacial” loess: quartz silt formation, source areas and sediment pathways in the formation of loess deposits.&amp;quot; Geomorphology 36.3-4 (2001): 231-256.&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
Wright, J. S., Smith, B. J. &amp;amp; Whalley, W. B. Mechanisms of loess-sized quartz silt production and their relative effectiveness: Laboratory simulations. Geomorphology 23, 15-34 (1998).&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
Wentworth, Chester K. &amp;quot;A scale of grade and class terms for clastic sediments.&amp;quot; The journal of geology 30.5 (1922): 377-392.&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
NRCS, USDA. &amp;quot;National soil survey handbook, title 430-VI.&amp;quot; (2007).&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
“Silt: Environmental Impact.” Rashid&#039;s Blog: An Educational Portal, 8 May 2016, rashidfaridi.com/2016/03/04/silt-environmental-impact/.&lt;br /&gt;
&lt;br /&gt;
[7]&lt;br /&gt;
“Loess Hills.” Iowa Geological Survey, 11 July 2017, www.iihr.uiowa.edu/igs/loess-hills/?doing_wp_cron=1525843720.4534800052642822265625.&lt;br /&gt;
&lt;br /&gt;
[8]&lt;br /&gt;
“Choosing a Topsoil Mix for Your Yard or Garden.” Washington Rock Quarries, 23 Mar. 2017, www.wa-rock.com/choosing-topsoil-mix-yard-garden/.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2498</id>
		<title>Silt</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2498"/>
		<updated>2018-05-09T05:30:58Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;[[File:Silty.jpg|thumb|right|Silt [6]]]&lt;br /&gt;
&lt;br /&gt;
==Definition==&lt;br /&gt;
&lt;br /&gt;
Silt is a granular sediment that can be transported and deposited by water, ice, and wind. Silt particles are larger than clay, but smaller than sand. To be classified as silt, a particle must be between .002 to .05 mm [1]. Similarly to [[clay]], sand, and gravel, silt is found in [[soil]]. Silt can also occur as sediment mixed in suspension with water. Because of silt’s spherical shape, it retains a large amount of water. Silty soil is known to be more fertile than other soils, and many species of [[organisms]] thrive in it.&lt;br /&gt;
&lt;br /&gt;
[[File:loess.jpg|thumb|left|Loess [7]]]&lt;br /&gt;
==Formation==&lt;br /&gt;
&lt;br /&gt;
Silt-producing mechanisms include frost shattering (Freeze-Thaw Weathering), comminution during transport, eolian abrasion, salt weathering, and glacial grinding. Windblown silt blankets the land in many parts of the world [2]. Large deposits of silt, such as this, are known as loess. Loess landscapes are usually a sign of past glacial activity, including areas such as the Great Plains. Silt can accumulate quickly in areas that lack vegetation, which can disrupt ecosystems. Silt also settles in still water, resulting in build ups like deltas. The main mineral origin of silt is quartz and feldspar [3]. The formation and movement of silt are constantly altering ecosystems. &lt;br /&gt;
&lt;br /&gt;
==Identification==&lt;br /&gt;
&lt;br /&gt;
Silt soil is fine and feels like flour when dry. When silt is wet it becomes a smooth mud that can be easily molded into shapes. When silt soil is very wet, it blends seamlessly with water, and forms puddles of mud [4]. Silt particles are very small, so they have a very smooth [[soil texture]]. Silty soil drains well, but not as quickly as sand. Silts sparkly appearance can be observed using a hand lens. Pure silts are identified by their lack of cohesion. Silts and clays are distinguished by their plasticity [5].&lt;br /&gt;
&lt;br /&gt;
[[File:soilmodel.jpg|thumb|right|[8]]]&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
&lt;br /&gt;
*[[Clay]]&lt;br /&gt;
*[[Loam]]&lt;br /&gt;
*[[Founders of Soil Concepts]]&lt;br /&gt;
*[[Humus]]&lt;br /&gt;
*[[Microorganisms]]&lt;br /&gt;
*[[Pedogenesis]]&lt;br /&gt;
*[[Soil]]&lt;br /&gt;
*[[Soil Textures]]&lt;br /&gt;
*[[Soil Properties]] &lt;br /&gt;
*[[Jenny Equation]]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
National Geographic Society. “Silt.” National Geographic Society, 9 Oct. 2012, www.nationalgeographic.org/encyclopedia/silt/.&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
Wright, Janet S. &amp;quot;“Desert” loess versus “glacial” loess: quartz silt formation, source areas and sediment pathways in the formation of loess deposits.&amp;quot; Geomorphology 36.3-4 (2001): 231-256.&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
Wright, J. S., Smith, B. J. &amp;amp; Whalley, W. B. Mechanisms of loess-sized quartz silt production and their relative effectiveness: Laboratory simulations. Geomorphology 23, 15-34 (1998).&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
Wentworth, Chester K. &amp;quot;A scale of grade and class terms for clastic sediments.&amp;quot; The journal of geology 30.5 (1922): 377-392.&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
NRCS, USDA. &amp;quot;National soil survey handbook, title 430-VI.&amp;quot; (2007).&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
“Silt: Environmental Impact.” Rashid&#039;s Blog: An Educational Portal, 8 May 2016, rashidfaridi.com/2016/03/04/silt-environmental-impact/.&lt;br /&gt;
&lt;br /&gt;
[7]&lt;br /&gt;
“Loess Hills.” Iowa Geological Survey, 11 July 2017, www.iihr.uiowa.edu/igs/loess-hills/?doing_wp_cron=1525843720.4534800052642822265625.&lt;br /&gt;
&lt;br /&gt;
[8]&lt;br /&gt;
“Choosing a Topsoil Mix for Your Yard or Garden.” Washington Rock Quarries, 23 Mar. 2017, www.wa-rock.com/choosing-topsoil-mix-yard-garden/.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2486</id>
		<title>Silt</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2486"/>
		<updated>2018-05-09T05:21:52Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: /* Formation */&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==Definition==&lt;br /&gt;
&lt;br /&gt;
[[File:Silty.jpg|thumb|right|Silt [6]]]&lt;br /&gt;
&lt;br /&gt;
Silt is a granular sediment that can be transported and deposited by water, ice, and wind. Silt particles are larger than clay, but smaller than sand. To be classified as silt, a particle must be between .002 to .05 mm [1]. Similarly to [[clay]], sand, and gravel, silt is found in [[soil]]. Silt can also occur as sediment mixed in suspension with water. Because of silt’s spherical shape, it retains a large amount of water. Silty soil is known to be more fertile than other soils, and many species of [[organisms]] thrive in it.&lt;br /&gt;
&lt;br /&gt;
==Formation==&lt;br /&gt;
&lt;br /&gt;
Silt-producing mechanisms include frost shattering (Freeze-Thaw Weathering), comminution during transport, eolian abrasion, salt weathering, and glacial grinding. Windblown silt blankets the land in many parts of the world [2]. Large deposits of silt, such as this, are known as loess. Loess landscapes are usually a sign of past glacial activity, including areas such as the Great Plains. Silt can accumulate quickly in areas that lack vegetation, which can disrupt ecosystems. Silt also settles in still water, resulting in build ups like deltas. The main mineral origin of silt is quartz and feldspar [3].&lt;br /&gt;
&lt;br /&gt;
[[File:loess.jpg|thumb|right|Loess [7]]]&lt;br /&gt;
&lt;br /&gt;
==Identification==&lt;br /&gt;
&lt;br /&gt;
Silt soil is fine and feels like flour when dry. When silt is wet it becomes a smooth mud that can be easily molded into shapes. When silt soil is very wet, it blends seamlessly with water, and forms puddles of mud [4]. Silt particles are very small, so they have a very smooth [[soil texture]]. Silty soil drains well, but not as quickly as sand. Silts sparkly appearance can be observed using a hand lens. Pure silts are identified by their lack of cohesion. Silts and clays are distinguished by their plasticity [5].&lt;br /&gt;
&lt;br /&gt;
[[File:soilmodel.jpg|thumb|right|[8]]]&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
&lt;br /&gt;
*[[Clay]]&lt;br /&gt;
*[[Loam]]&lt;br /&gt;
*[[Founders of Soil Concepts]]&lt;br /&gt;
*[[Humus]]&lt;br /&gt;
*[[Microorganisms]]&lt;br /&gt;
*[[Pedogenesis]]&lt;br /&gt;
*[[Soil]]&lt;br /&gt;
*[[Soil Textures]]&lt;br /&gt;
*[[Soil Properties]] &lt;br /&gt;
*[[Jenny Equation]]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
National Geographic Society. “Silt.” National Geographic Society, 9 Oct. 2012, www.nationalgeographic.org/encyclopedia/silt/.&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
Wright, Janet S. &amp;quot;“Desert” loess versus “glacial” loess: quartz silt formation, source areas and sediment pathways in the formation of loess deposits.&amp;quot; Geomorphology 36.3-4 (2001): 231-256.&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
Wright, J. S., Smith, B. J. &amp;amp; Whalley, W. B. Mechanisms of loess-sized quartz silt production and their relative effectiveness: Laboratory simulations. Geomorphology 23, 15-34 (1998).&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
Wentworth, Chester K. &amp;quot;A scale of grade and class terms for clastic sediments.&amp;quot; The journal of geology 30.5 (1922): 377-392.&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
NRCS, USDA. &amp;quot;National soil survey handbook, title 430-VI.&amp;quot; (2007).&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
“Silt: Environmental Impact.” Rashid&#039;s Blog: An Educational Portal, 8 May 2016, rashidfaridi.com/2016/03/04/silt-environmental-impact/.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2482</id>
		<title>Silt</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2482"/>
		<updated>2018-05-09T05:20:44Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: /* Identification */&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==Definition==&lt;br /&gt;
&lt;br /&gt;
[[File:Silty.jpg|thumb|right|Silt [6]]]&lt;br /&gt;
&lt;br /&gt;
Silt is a granular sediment that can be transported and deposited by water, ice, and wind. Silt particles are larger than clay, but smaller than sand. To be classified as silt, a particle must be between .002 to .05 mm [1]. Similarly to [[clay]], sand, and gravel, silt is found in [[soil]]. Silt can also occur as sediment mixed in suspension with water. Because of silt’s spherical shape, it retains a large amount of water. Silty soil is known to be more fertile than other soils, and many species of [[organisms]] thrive in it.&lt;br /&gt;
&lt;br /&gt;
==Formation==&lt;br /&gt;
&lt;br /&gt;
Silt-producing mechanisms include frost shattering (Freeze-Thaw Weathering), comminution during transport, eolian abrasion, salt weathering, and glacial grinding. Windblown silt blankets the land in many parts of the world [2]. Large deposits of silt, such as this, are known as loess. Loess landscapes are usually a sign of past glacial activity, including areas such as the Great Plains. Silt can accumulate quickly in areas that lack vegetation, which can disrupt ecosystems. Silt also settles in still water, resulting in build ups like deltas. The main mineral origin of silt is quartz and feldspar [3].&lt;br /&gt;
&lt;br /&gt;
[[File:loess.jpg|thumb|left|Loess [7]]]&lt;br /&gt;
&lt;br /&gt;
==Identification==&lt;br /&gt;
&lt;br /&gt;
Silt soil is fine and feels like flour when dry. When silt is wet it becomes a smooth mud that can be easily molded into shapes. When silt soil is very wet, it blends seamlessly with water, and forms puddles of mud [4]. Silt particles are very small, so they have a very smooth [[soil texture]]. Silty soil drains well, but not as quickly as sand. Silts sparkly appearance can be observed using a hand lens. Pure silts are identified by their lack of cohesion. Silts and clays are distinguished by their plasticity [5].&lt;br /&gt;
&lt;br /&gt;
[[File:soilmodel.jpg|thumb|right|[8]]]&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
&lt;br /&gt;
*[[Clay]]&lt;br /&gt;
*[[Loam]]&lt;br /&gt;
*[[Founders of Soil Concepts]]&lt;br /&gt;
*[[Humus]]&lt;br /&gt;
*[[Microorganisms]]&lt;br /&gt;
*[[Pedogenesis]]&lt;br /&gt;
*[[Soil]]&lt;br /&gt;
*[[Soil Textures]]&lt;br /&gt;
*[[Soil Properties]] &lt;br /&gt;
*[[Jenny Equation]]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
National Geographic Society. “Silt.” National Geographic Society, 9 Oct. 2012, www.nationalgeographic.org/encyclopedia/silt/.&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
Wright, Janet S. &amp;quot;“Desert” loess versus “glacial” loess: quartz silt formation, source areas and sediment pathways in the formation of loess deposits.&amp;quot; Geomorphology 36.3-4 (2001): 231-256.&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
Wright, J. S., Smith, B. J. &amp;amp; Whalley, W. B. Mechanisms of loess-sized quartz silt production and their relative effectiveness: Laboratory simulations. Geomorphology 23, 15-34 (1998).&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
Wentworth, Chester K. &amp;quot;A scale of grade and class terms for clastic sediments.&amp;quot; The journal of geology 30.5 (1922): 377-392.&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
NRCS, USDA. &amp;quot;National soil survey handbook, title 430-VI.&amp;quot; (2007).&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
“Silt: Environmental Impact.” Rashid&#039;s Blog: An Educational Portal, 8 May 2016, rashidfaridi.com/2016/03/04/silt-environmental-impact/.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=File:Soilmodel.jpg&amp;diff=2480</id>
		<title>File:Soilmodel.jpg</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=File:Soilmodel.jpg&amp;diff=2480"/>
		<updated>2018-05-09T05:20:21Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=File:Soilchart.png&amp;diff=2477</id>
		<title>File:Soilchart.png</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=File:Soilchart.png&amp;diff=2477"/>
		<updated>2018-05-09T05:19:10Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2471</id>
		<title>Silt</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2471"/>
		<updated>2018-05-09T05:15:31Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: /* Identification */&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==Definition==&lt;br /&gt;
&lt;br /&gt;
[[File:Silty.jpg|thumb|right|Silt [6]]]&lt;br /&gt;
&lt;br /&gt;
Silt is a granular sediment that can be transported and deposited by water, ice, and wind. Silt particles are larger than clay, but smaller than sand. To be classified as silt, a particle must be between .002 to .05 mm [1]. Similarly to [[clay]], sand, and gravel, silt is found in [[soil]]. Silt can also occur as sediment mixed in suspension with water. Because of silt’s spherical shape, it retains a large amount of water. Silty soil is known to be more fertile than other soils, and many species of [[organisms]] thrive in it.&lt;br /&gt;
&lt;br /&gt;
==Formation==&lt;br /&gt;
&lt;br /&gt;
Silt-producing mechanisms include frost shattering (Freeze-Thaw Weathering), comminution during transport, eolian abrasion, salt weathering, and glacial grinding. Windblown silt blankets the land in many parts of the world [2]. Large deposits of silt, such as this, are known as loess. Loess landscapes are usually a sign of past glacial activity, including areas such as the Great Plains. Silt can accumulate quickly in areas that lack vegetation, which can disrupt ecosystems. Silt also settles in still water, resulting in build ups like deltas. The main mineral origin of silt is quartz and feldspar [3].&lt;br /&gt;
&lt;br /&gt;
[[File:loess.jpg|thumb|left|Loess [7]]]&lt;br /&gt;
&lt;br /&gt;
==Identification==&lt;br /&gt;
&lt;br /&gt;
Silt soil is fine and feels like flour when dry. When silt is wet it becomes a smooth mud that can be easily molded into shapes. When silt soil is very wet, it blends seamlessly with water, and forms puddles of mud [4]. Silt particles are very small, so they have a very smooth [[soil texture]]. Silty soil drains well, but not as quickly as sand. Silts sparkly appearance can be observed using a hand lens. Pure silts are identified by their lack of cohesion. Silts and clays are distinguished by their plasticity [5].&lt;br /&gt;
&lt;br /&gt;
[[File:identification.jpg|thumb|right|[8]]]&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
&lt;br /&gt;
*[[Clay]]&lt;br /&gt;
*[[Loam]]&lt;br /&gt;
*[[Founders of Soil Concepts]]&lt;br /&gt;
*[[Humus]]&lt;br /&gt;
*[[Microorganisms]]&lt;br /&gt;
*[[Pedogenesis]]&lt;br /&gt;
*[[Soil]]&lt;br /&gt;
*[[Soil Textures]]&lt;br /&gt;
*[[Soil Properties]] &lt;br /&gt;
*[[Jenny Equation]]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
National Geographic Society. “Silt.” National Geographic Society, 9 Oct. 2012, www.nationalgeographic.org/encyclopedia/silt/.&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
Wright, Janet S. &amp;quot;“Desert” loess versus “glacial” loess: quartz silt formation, source areas and sediment pathways in the formation of loess deposits.&amp;quot; Geomorphology 36.3-4 (2001): 231-256.&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
Wright, J. S., Smith, B. J. &amp;amp; Whalley, W. B. Mechanisms of loess-sized quartz silt production and their relative effectiveness: Laboratory simulations. Geomorphology 23, 15-34 (1998).&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
Wentworth, Chester K. &amp;quot;A scale of grade and class terms for clastic sediments.&amp;quot; The journal of geology 30.5 (1922): 377-392.&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
NRCS, USDA. &amp;quot;National soil survey handbook, title 430-VI.&amp;quot; (2007).&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
“Silt: Environmental Impact.” Rashid&#039;s Blog: An Educational Portal, 8 May 2016, rashidfaridi.com/2016/03/04/silt-environmental-impact/.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2466</id>
		<title>Silt</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2466"/>
		<updated>2018-05-09T05:11:16Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: /* Formation */&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==Definition==&lt;br /&gt;
&lt;br /&gt;
[[File:Silty.jpg|thumb|right|Silt [6]]]&lt;br /&gt;
&lt;br /&gt;
Silt is a granular sediment that can be transported and deposited by water, ice, and wind. Silt particles are larger than clay, but smaller than sand. To be classified as silt, a particle must be between .002 to .05 mm [1]. Similarly to [[clay]], sand, and gravel, silt is found in [[soil]]. Silt can also occur as sediment mixed in suspension with water. Because of silt’s spherical shape, it retains a large amount of water. Silty soil is known to be more fertile than other soils, and many species of [[organisms]] thrive in it.&lt;br /&gt;
&lt;br /&gt;
==Formation==&lt;br /&gt;
&lt;br /&gt;
Silt-producing mechanisms include frost shattering (Freeze-Thaw Weathering), comminution during transport, eolian abrasion, salt weathering, and glacial grinding. Windblown silt blankets the land in many parts of the world [2]. Large deposits of silt, such as this, are known as loess. Loess landscapes are usually a sign of past glacial activity, including areas such as the Great Plains. Silt can accumulate quickly in areas that lack vegetation, which can disrupt ecosystems. Silt also settles in still water, resulting in build ups like deltas. The main mineral origin of silt is quartz and feldspar [3].&lt;br /&gt;
&lt;br /&gt;
[[File:loess.jpg|thumb|left|Loess [7]]]&lt;br /&gt;
&lt;br /&gt;
==Identification==&lt;br /&gt;
&lt;br /&gt;
Silt soil is fine and feels like flour when dry. When silt is wet it becomes a smooth mud that can be easily molded into shapes. When silt soil is very wet, it blends seamlessly with water, and forms puddles of mud [4]. Silt particles are very small, so they have a very smooth [[soil texture]]. Silty soil drains well, but not as quickly as sand. Silts sparkly appearance can be observed using a hand lens. Pure silts are identified by their lack of cohesion. Silts and clays are distinguished by their plasticity [5].&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
&lt;br /&gt;
*[[Clay]]&lt;br /&gt;
*[[Loam]]&lt;br /&gt;
*[[Founders of Soil Concepts]]&lt;br /&gt;
*[[Humus]]&lt;br /&gt;
*[[Microorganisms]]&lt;br /&gt;
*[[Pedogenesis]]&lt;br /&gt;
*[[Soil]]&lt;br /&gt;
*[[Soil Textures]]&lt;br /&gt;
*[[Soil Properties]] &lt;br /&gt;
*[[Jenny Equation]]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
National Geographic Society. “Silt.” National Geographic Society, 9 Oct. 2012, www.nationalgeographic.org/encyclopedia/silt/.&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
Wright, Janet S. &amp;quot;“Desert” loess versus “glacial” loess: quartz silt formation, source areas and sediment pathways in the formation of loess deposits.&amp;quot; Geomorphology 36.3-4 (2001): 231-256.&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
Wright, J. S., Smith, B. J. &amp;amp; Whalley, W. B. Mechanisms of loess-sized quartz silt production and their relative effectiveness: Laboratory simulations. Geomorphology 23, 15-34 (1998).&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
Wentworth, Chester K. &amp;quot;A scale of grade and class terms for clastic sediments.&amp;quot; The journal of geology 30.5 (1922): 377-392.&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
NRCS, USDA. &amp;quot;National soil survey handbook, title 430-VI.&amp;quot; (2007).&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
“Silt: Environmental Impact.” Rashid&#039;s Blog: An Educational Portal, 8 May 2016, rashidfaridi.com/2016/03/04/silt-environmental-impact/.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=File:Loess.jpg&amp;diff=2464</id>
		<title>File:Loess.jpg</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=File:Loess.jpg&amp;diff=2464"/>
		<updated>2018-05-09T05:10:37Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2462</id>
		<title>Silt</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2462"/>
		<updated>2018-05-09T05:07:06Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: /* Identification */&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==Definition==&lt;br /&gt;
&lt;br /&gt;
[[File:Silty.jpg|thumb|right|Silt [6]]]&lt;br /&gt;
&lt;br /&gt;
Silt is a granular sediment that can be transported and deposited by water, ice, and wind. Silt particles are larger than clay, but smaller than sand. To be classified as silt, a particle must be between .002 to .05 mm [1]. Similarly to [[clay]], sand, and gravel, silt is found in [[soil]]. Silt can also occur as sediment mixed in suspension with water. Because of silt’s spherical shape, it retains a large amount of water. Silty soil is known to be more fertile than other soils, and many species of [[organisms]] thrive in it.&lt;br /&gt;
&lt;br /&gt;
==Formation==&lt;br /&gt;
&lt;br /&gt;
Silt-producing mechanisms include frost shattering (Freeze-Thaw Weathering), comminution during transport, eolian abrasion, salt weathering, and glacial grinding. Windblown silt blankets the land in many parts of the world [2]. Large deposits of silt, such as this, are known as loess. Loess landscapes are usually a sign of past glacial activity, including areas such as the Great Plains. Silt can accumulate quickly in areas that lack vegetation, which can disrupt ecosystems. Silt also settles in still water, resulting in build ups like deltas. The main mineral origin of silt is quartz and feldspar [3].&lt;br /&gt;
&lt;br /&gt;
==Identification==&lt;br /&gt;
&lt;br /&gt;
Silt soil is fine and feels like flour when dry. When silt is wet it becomes a smooth mud that can be easily molded into shapes. When silt soil is very wet, it blends seamlessly with water, and forms puddles of mud [4]. Silt particles are very small, so they have a very smooth [[soil texture]]. Silty soil drains well, but not as quickly as sand. Silts sparkly appearance can be observed using a hand lens. Pure silts are identified by their lack of cohesion. Silts and clays are distinguished by their plasticity [5].&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
&lt;br /&gt;
*[[Clay]]&lt;br /&gt;
*[[Loam]]&lt;br /&gt;
*[[Founders of Soil Concepts]]&lt;br /&gt;
*[[Humus]]&lt;br /&gt;
*[[Microorganisms]]&lt;br /&gt;
*[[Pedogenesis]]&lt;br /&gt;
*[[Soil]]&lt;br /&gt;
*[[Soil Textures]]&lt;br /&gt;
*[[Soil Properties]] &lt;br /&gt;
*[[Jenny Equation]]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
National Geographic Society. “Silt.” National Geographic Society, 9 Oct. 2012, www.nationalgeographic.org/encyclopedia/silt/.&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
Wright, Janet S. &amp;quot;“Desert” loess versus “glacial” loess: quartz silt formation, source areas and sediment pathways in the formation of loess deposits.&amp;quot; Geomorphology 36.3-4 (2001): 231-256.&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
Wright, J. S., Smith, B. J. &amp;amp; Whalley, W. B. Mechanisms of loess-sized quartz silt production and their relative effectiveness: Laboratory simulations. Geomorphology 23, 15-34 (1998).&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
Wentworth, Chester K. &amp;quot;A scale of grade and class terms for clastic sediments.&amp;quot; The journal of geology 30.5 (1922): 377-392.&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
NRCS, USDA. &amp;quot;National soil survey handbook, title 430-VI.&amp;quot; (2007).&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
“Silt: Environmental Impact.” Rashid&#039;s Blog: An Educational Portal, 8 May 2016, rashidfaridi.com/2016/03/04/silt-environmental-impact/.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2460</id>
		<title>Silt</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2460"/>
		<updated>2018-05-09T05:06:11Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: /* References */&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==Definition==&lt;br /&gt;
&lt;br /&gt;
[[File:Silty.jpg|thumb|right|Silt [6]]]&lt;br /&gt;
&lt;br /&gt;
Silt is a granular sediment that can be transported and deposited by water, ice, and wind. Silt particles are larger than clay, but smaller than sand. To be classified as silt, a particle must be between .002 to .05 mm [1]. Similarly to [[clay]], sand, and gravel, silt is found in [[soil]]. Silt can also occur as sediment mixed in suspension with water. Because of silt’s spherical shape, it retains a large amount of water. Silty soil is known to be more fertile than other soils, and many species of [[organisms]] thrive in it.&lt;br /&gt;
&lt;br /&gt;
==Formation==&lt;br /&gt;
&lt;br /&gt;
Silt-producing mechanisms include frost shattering (Freeze-Thaw Weathering), comminution during transport, eolian abrasion, salt weathering, and glacial grinding. Windblown silt blankets the land in many parts of the world [2]. Large deposits of silt, such as this, are known as loess. Loess landscapes are usually a sign of past glacial activity, including areas such as the Great Plains. Silt can accumulate quickly in areas that lack vegetation, which can disrupt ecosystems. Silt also settles in still water, resulting in build ups like deltas. The main mineral origin of silt is quartz and feldspar [3].&lt;br /&gt;
&lt;br /&gt;
==Identification==&lt;br /&gt;
&lt;br /&gt;
Silt soil is fine and feels like flour when dry. When silt is wet it becomes a smooth mud that can be easily molded into shapes. When silt soil is very wet, it blends seamlessly with water, and forms puddles of mud [4]. Silt particles are very small, so they have a very smooth texture. Silty soil drains well, but not as quickly as sand. Silts sparkly appearance can be observed using a hand lens. Pure silts are identified by their lack of cohesion. Silts and clays are distinguished by their plasticity [5].&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
&lt;br /&gt;
*[[Clay]]&lt;br /&gt;
*[[Loam]]&lt;br /&gt;
*[[Founders of Soil Concepts]]&lt;br /&gt;
*[[Humus]]&lt;br /&gt;
*[[Microorganisms]]&lt;br /&gt;
*[[Pedogenesis]]&lt;br /&gt;
*[[Soil]]&lt;br /&gt;
*[[Soil Textures]]&lt;br /&gt;
*[[Soil Properties]] &lt;br /&gt;
*[[Jenny Equation]]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
National Geographic Society. “Silt.” National Geographic Society, 9 Oct. 2012, www.nationalgeographic.org/encyclopedia/silt/.&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
Wright, Janet S. &amp;quot;“Desert” loess versus “glacial” loess: quartz silt formation, source areas and sediment pathways in the formation of loess deposits.&amp;quot; Geomorphology 36.3-4 (2001): 231-256.&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
Wright, J. S., Smith, B. J. &amp;amp; Whalley, W. B. Mechanisms of loess-sized quartz silt production and their relative effectiveness: Laboratory simulations. Geomorphology 23, 15-34 (1998).&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
Wentworth, Chester K. &amp;quot;A scale of grade and class terms for clastic sediments.&amp;quot; The journal of geology 30.5 (1922): 377-392.&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
NRCS, USDA. &amp;quot;National soil survey handbook, title 430-VI.&amp;quot; (2007).&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
“Silt: Environmental Impact.” Rashid&#039;s Blog: An Educational Portal, 8 May 2016, rashidfaridi.com/2016/03/04/silt-environmental-impact/.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2459</id>
		<title>Silt</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2459"/>
		<updated>2018-05-09T05:06:01Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: /* Identification */&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==Definition==&lt;br /&gt;
&lt;br /&gt;
[[File:Silty.jpg|thumb|right|Silt [6]]]&lt;br /&gt;
&lt;br /&gt;
Silt is a granular sediment that can be transported and deposited by water, ice, and wind. Silt particles are larger than clay, but smaller than sand. To be classified as silt, a particle must be between .002 to .05 mm [1]. Similarly to [[clay]], sand, and gravel, silt is found in [[soil]]. Silt can also occur as sediment mixed in suspension with water. Because of silt’s spherical shape, it retains a large amount of water. Silty soil is known to be more fertile than other soils, and many species of [[organisms]] thrive in it.&lt;br /&gt;
&lt;br /&gt;
==Formation==&lt;br /&gt;
&lt;br /&gt;
Silt-producing mechanisms include frost shattering (Freeze-Thaw Weathering), comminution during transport, eolian abrasion, salt weathering, and glacial grinding. Windblown silt blankets the land in many parts of the world [2]. Large deposits of silt, such as this, are known as loess. Loess landscapes are usually a sign of past glacial activity, including areas such as the Great Plains. Silt can accumulate quickly in areas that lack vegetation, which can disrupt ecosystems. Silt also settles in still water, resulting in build ups like deltas. The main mineral origin of silt is quartz and feldspar [3].&lt;br /&gt;
&lt;br /&gt;
==Identification==&lt;br /&gt;
&lt;br /&gt;
Silt soil is fine and feels like flour when dry. When silt is wet it becomes a smooth mud that can be easily molded into shapes. When silt soil is very wet, it blends seamlessly with water, and forms puddles of mud [4]. Silt particles are very small, so they have a very smooth texture. Silty soil drains well, but not as quickly as sand. Silts sparkly appearance can be observed using a hand lens. Pure silts are identified by their lack of cohesion. Silts and clays are distinguished by their plasticity [5].&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
&lt;br /&gt;
*[[Clay]]&lt;br /&gt;
*[[Loam]]&lt;br /&gt;
*[[Founders of Soil Concepts]]&lt;br /&gt;
*[[Humus]]&lt;br /&gt;
*[[Microorganisms]]&lt;br /&gt;
*[[Pedogenesis]]&lt;br /&gt;
*[[Soil]]&lt;br /&gt;
*[[Soil Textures]]&lt;br /&gt;
*[[Soil Properties]] &lt;br /&gt;
*[[Jenny Equation]]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
National Geographic Society. “Silt.” National Geographic Society, 9 Oct. 2012, www.nationalgeographic.org/encyclopedia/silt/.&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
Wright, Janet S. &amp;quot;“Desert” loess versus “glacial” loess: quartz silt formation, source areas and sediment pathways in the formation of loess deposits.&amp;quot; Geomorphology 36.3-4 (2001): 231-256.&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
Wright, J. S., Smith, B. J. &amp;amp; Whalley, W. B. Mechanisms of loess-sized quartz silt production and their relative effectiveness: Laboratory simulations. Geomorphology 23, 15-34 (1998).&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
Wentworth, Chester K. &amp;quot;A scale of grade and class terms for clastic sediments.&amp;quot; The journal of geology 30.5 (1922): 377-392.&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
“Silt: Environmental Impact.” Rashid&#039;s Blog: An Educational Portal, 8 May 2016, rashidfaridi.com/2016/03/04/silt-environmental-impact/.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2452</id>
		<title>Silt</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2452"/>
		<updated>2018-05-09T04:59:06Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: /* References */&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==Definition==&lt;br /&gt;
&lt;br /&gt;
[[File:Silty.jpg|thumb|right|Silt [6]]]&lt;br /&gt;
&lt;br /&gt;
Silt is a granular sediment that can be transported and deposited by water, ice, and wind. Silt particles are larger than clay, but smaller than sand. To be classified as silt, a particle must be between .002 to .05 mm [1]. Similarly to [[clay]], sand, and gravel, silt is found in [[soil]]. Silt can also occur as sediment mixed in suspension with water. Because of silt’s spherical shape, it retains a large amount of water. Silty soil is known to be more fertile than other soils, and many species of [[organisms]] thrive in it.&lt;br /&gt;
&lt;br /&gt;
==Formation==&lt;br /&gt;
&lt;br /&gt;
Silt-producing mechanisms include frost shattering (Freeze-Thaw Weathering), comminution during transport, eolian abrasion, salt weathering, and glacial grinding. Windblown silt blankets the land in many parts of the world [2]. Large deposits of silt, such as this, are known as loess. Loess landscapes are usually a sign of past glacial activity, including areas such as the Great Plains. Silt can accumulate quickly in areas that lack vegetation, which can disrupt ecosystems. Silt also settles in still water, resulting in build ups like deltas. The main mineral origin of silt is quartz and feldspar [3].&lt;br /&gt;
&lt;br /&gt;
==Identification==&lt;br /&gt;
&lt;br /&gt;
Silt soil is fine and feels like flour when dry. When silt is wet it becomes a smooth mud that can be easily molded into shapes. When silt soil is very wet, it blends seamlessly with water, and forms puddles of mud. Silt particles are very small, so they have a very smooth texture. Silty soil drains well, but not as quickly as sand.&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
&lt;br /&gt;
*[[Clay]]&lt;br /&gt;
*[[Loam]]&lt;br /&gt;
*[[Founders of Soil Concepts]]&lt;br /&gt;
*[[Humus]]&lt;br /&gt;
*[[Microorganisms]]&lt;br /&gt;
*[[Pedogenesis]]&lt;br /&gt;
*[[Soil]]&lt;br /&gt;
*[[Soil Textures]]&lt;br /&gt;
*[[Soil Properties]] &lt;br /&gt;
*[[Jenny Equation]]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
National Geographic Society. “Silt.” National Geographic Society, 9 Oct. 2012, www.nationalgeographic.org/encyclopedia/silt/.&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
Wright, Janet S. &amp;quot;“Desert” loess versus “glacial” loess: quartz silt formation, source areas and sediment pathways in the formation of loess deposits.&amp;quot; Geomorphology 36.3-4 (2001): 231-256.&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
Wright, J. S., Smith, B. J. &amp;amp; Whalley, W. B. Mechanisms of loess-sized quartz silt production and their relative effectiveness: Laboratory simulations. Geomorphology 23, 15-34 (1998).&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
Wentworth, Chester K. &amp;quot;A scale of grade and class terms for clastic sediments.&amp;quot; The journal of geology 30.5 (1922): 377-392.&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
“Silt: Environmental Impact.” Rashid&#039;s Blog: An Educational Portal, 8 May 2016, rashidfaridi.com/2016/03/04/silt-environmental-impact/.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2451</id>
		<title>Silt</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2451"/>
		<updated>2018-05-09T04:58:54Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: /* Classification */&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==Definition==&lt;br /&gt;
&lt;br /&gt;
[[File:Silty.jpg|thumb|right|Silt [6]]]&lt;br /&gt;
&lt;br /&gt;
Silt is a granular sediment that can be transported and deposited by water, ice, and wind. Silt particles are larger than clay, but smaller than sand. To be classified as silt, a particle must be between .002 to .05 mm [1]. Similarly to [[clay]], sand, and gravel, silt is found in [[soil]]. Silt can also occur as sediment mixed in suspension with water. Because of silt’s spherical shape, it retains a large amount of water. Silty soil is known to be more fertile than other soils, and many species of [[organisms]] thrive in it.&lt;br /&gt;
&lt;br /&gt;
==Formation==&lt;br /&gt;
&lt;br /&gt;
Silt-producing mechanisms include frost shattering (Freeze-Thaw Weathering), comminution during transport, eolian abrasion, salt weathering, and glacial grinding. Windblown silt blankets the land in many parts of the world [2]. Large deposits of silt, such as this, are known as loess. Loess landscapes are usually a sign of past glacial activity, including areas such as the Great Plains. Silt can accumulate quickly in areas that lack vegetation, which can disrupt ecosystems. Silt also settles in still water, resulting in build ups like deltas. The main mineral origin of silt is quartz and feldspar [3].&lt;br /&gt;
&lt;br /&gt;
==Identification==&lt;br /&gt;
&lt;br /&gt;
Silt soil is fine and feels like flour when dry. When silt is wet it becomes a smooth mud that can be easily molded into shapes. When silt soil is very wet, it blends seamlessly with water, and forms puddles of mud. Silt particles are very small, so they have a very smooth texture. Silty soil drains well, but not as quickly as sand.&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
&lt;br /&gt;
*[[Clay]]&lt;br /&gt;
*[[Loam]]&lt;br /&gt;
*[[Founders of Soil Concepts]]&lt;br /&gt;
*[[Humus]]&lt;br /&gt;
*[[Microorganisms]]&lt;br /&gt;
*[[Pedogenesis]]&lt;br /&gt;
*[[Soil]]&lt;br /&gt;
*[[Soil Textures]]&lt;br /&gt;
*[[Soil Properties]] &lt;br /&gt;
*[[Jenny Equation]]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
National Geographic Society. “Silt.” National Geographic Society, 9 Oct. 2012, www.nationalgeographic.org/encyclopedia/silt/.&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
Wright, Janet S. &amp;quot;“Desert” loess versus “glacial” loess: quartz silt formation, source areas and sediment pathways in the formation of loess deposits.&amp;quot; Geomorphology 36.3-4 (2001): 231-256.&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
Wright, J. S., Smith, B. J. &amp;amp; Whalley, W. B. Mechanisms of loess-sized quartz silt production and their relative effectiveness: Laboratory simulations. Geomorphology 23, 15-34 (1998).&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
“Silt: Environmental Impact.” Rashid&#039;s Blog: An Educational Portal, 8 May 2016, rashidfaridi.com/2016/03/04/silt-environmental-impact/.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2428</id>
		<title>Silt</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2428"/>
		<updated>2018-05-09T04:44:58Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==Definition==&lt;br /&gt;
&lt;br /&gt;
[[File:Silty.jpg|thumb|right|Silt [6]]]&lt;br /&gt;
&lt;br /&gt;
Silt is a granular sediment that can be transported and deposited by water, ice, and wind. Silt particles are larger than clay, but smaller than sand. To be classified as silt, a particle must be between .002 to .05 mm [1]. Similarly to [[clay]], sand, and gravel, silt is found in [[soil]]. Silt can also occur as sediment mixed in suspension with water. Because of silt’s spherical shape, it retains a large amount of water. Silty soil is known to be more fertile than other soils, and many species of [[organisms]] thrive in it.&lt;br /&gt;
&lt;br /&gt;
==Formation==&lt;br /&gt;
&lt;br /&gt;
Silt-producing mechanisms include frost shattering (Freeze-Thaw Weathering), comminution during transport, eolian abrasion, salt weathering, and glacial grinding. Windblown silt blankets the land in many parts of the world [2]. Large deposits of silt, such as this, are known as loess. Loess landscapes are usually a sign of past glacial activity, including areas such as the Great Plains. Silt can accumulate quickly in areas that lack vegetation, which can disrupt ecosystems. Silt also settles in still water, resulting in build ups like deltas. The main mineral origin of silt is quartz and feldspar [3].&lt;br /&gt;
&lt;br /&gt;
==Classification==&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
&lt;br /&gt;
*[[Clay]]&lt;br /&gt;
*[[Loam]]&lt;br /&gt;
*[[Founders of Soil Concepts]]&lt;br /&gt;
*[[Humus]]&lt;br /&gt;
*[[Microorganisms]]&lt;br /&gt;
*[[Pedogenesis]]&lt;br /&gt;
*[[Soil]]&lt;br /&gt;
*[[Soil Textures]]&lt;br /&gt;
*[[Soil Properties]] &lt;br /&gt;
*[[Jenny Equation]]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
National Geographic Society. “Silt.” National Geographic Society, 9 Oct. 2012, www.nationalgeographic.org/encyclopedia/silt/.&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
Wright, Janet S. &amp;quot;“Desert” loess versus “glacial” loess: quartz silt formation, source areas and sediment pathways in the formation of loess deposits.&amp;quot; Geomorphology 36.3-4 (2001): 231-256.&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
Wright, J. S., Smith, B. J. &amp;amp; Whalley, W. B. Mechanisms of loess-sized quartz silt production and their relative effectiveness: Laboratory simulations. Geomorphology 23, 15-34 (1998).&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
“Silt: Environmental Impact.” Rashid&#039;s Blog: An Educational Portal, 8 May 2016, rashidfaridi.com/2016/03/04/silt-environmental-impact/.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2427</id>
		<title>Silt</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2427"/>
		<updated>2018-05-09T04:44:39Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==Definition==&lt;br /&gt;
&lt;br /&gt;
[[File:Silty.jpg|thumb|left|Silt [6]]]&lt;br /&gt;
&lt;br /&gt;
Silt is a granular sediment that can be transported and deposited by water, ice, and wind. Silt particles are larger than clay, but smaller than sand. To be classified as silt, a particle must be between .002 to .05 mm [1]. Similarly to [[clay]], sand, and gravel, silt is found in [[soil]]. Silt can also occur as sediment mixed in suspension with water. Because of silt’s spherical shape, it retains a large amount of water. Silty soil is known to be more fertile than other soils, and many species of [[organisms]] thrive in it.&lt;br /&gt;
&lt;br /&gt;
==Formation==&lt;br /&gt;
&lt;br /&gt;
Silt-producing mechanisms include frost shattering (Freeze-Thaw Weathering), comminution during transport, eolian abrasion, salt weathering, and glacial grinding. Windblown silt blankets the land in many parts of the world [2]. Large deposits of silt, such as this, are known as loess. Loess landscapes are usually a sign of past glacial activity, including areas such as the Great Plains. Silt can accumulate quickly in areas that lack vegetation, which can disrupt ecosystems. Silt also settles in still water, resulting in build ups like deltas. The main mineral origin of silt is quartz and feldspar [3].&lt;br /&gt;
&lt;br /&gt;
==Classification==&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
&lt;br /&gt;
*[[Clay]]&lt;br /&gt;
*[[Loam]]&lt;br /&gt;
*[[Founders of Soil Concepts]]&lt;br /&gt;
*[[Humus]]&lt;br /&gt;
*[[Microorganisms]]&lt;br /&gt;
*[[Pedogenesis]]&lt;br /&gt;
*[[Soil]]&lt;br /&gt;
*[[Soil Textures]]&lt;br /&gt;
*[[Soil Properties]] &lt;br /&gt;
*[[Jenny Equation]]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
National Geographic Society. “Silt.” National Geographic Society, 9 Oct. 2012, www.nationalgeographic.org/encyclopedia/silt/.&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
Wright, Janet S. &amp;quot;“Desert” loess versus “glacial” loess: quartz silt formation, source areas and sediment pathways in the formation of loess deposits.&amp;quot; Geomorphology 36.3-4 (2001): 231-256.&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
Wright, J. S., Smith, B. J. &amp;amp; Whalley, W. B. Mechanisms of loess-sized quartz silt production and their relative effectiveness: Laboratory simulations. Geomorphology 23, 15-34 (1998).&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
“Silt: Environmental Impact.” Rashid&#039;s Blog: An Educational Portal, 8 May 2016, rashidfaridi.com/2016/03/04/silt-environmental-impact/.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2425</id>
		<title>Silt</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2425"/>
		<updated>2018-05-09T04:44:16Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: /* Formation */&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==Definition==&lt;br /&gt;
&lt;br /&gt;
[[File:Silty.jpg|thumb|right|Silt [6]]]&lt;br /&gt;
&lt;br /&gt;
Silt is a granular sediment that can be transported and deposited by water, ice, and wind. Silt particles are larger than clay, but smaller than sand. To be classified as silt, a particle must be between .002 to .05 mm [1]. Similarly to [[clay]], sand, and gravel, silt is found in [[soil]]. Silt can also occur as sediment mixed in suspension with water. Because of silt’s spherical shape, it retains a large amount of water. Silty soil is known to be more fertile than other soils, and many species of [[organisms]] thrive in it.&lt;br /&gt;
&lt;br /&gt;
==Formation==&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
Silt-producing mechanisms include frost shattering (Freeze-Thaw Weathering), comminution during transport, eolian abrasion, salt weathering, and glacial grinding. Windblown silt blankets the land in many parts of the world [2]. Large deposits of silt, such as this, are known as loess. Loess landscapes are usually a sign of past glacial activity, including areas such as the Great Plains. Silt can accumulate quickly in areas that lack vegetation, which can disrupt ecosystems. Silt also settles in still water, resulting in build ups like deltas. The main mineral origin of silt is quartz and feldspar [3].&lt;br /&gt;
&lt;br /&gt;
==Classification==&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
&lt;br /&gt;
*[[Clay]]&lt;br /&gt;
*[[Loam]]&lt;br /&gt;
*[[Founders of Soil Concepts]]&lt;br /&gt;
*[[Humus]]&lt;br /&gt;
*[[Microorganisms]]&lt;br /&gt;
*[[Pedogenesis]]&lt;br /&gt;
*[[Soil]]&lt;br /&gt;
*[[Soil Textures]]&lt;br /&gt;
*[[Soil Properties]] &lt;br /&gt;
*[[Jenny Equation]]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
National Geographic Society. “Silt.” National Geographic Society, 9 Oct. 2012, www.nationalgeographic.org/encyclopedia/silt/.&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
Wright, Janet S. &amp;quot;“Desert” loess versus “glacial” loess: quartz silt formation, source areas and sediment pathways in the formation of loess deposits.&amp;quot; Geomorphology 36.3-4 (2001): 231-256.&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
Wright, J. S., Smith, B. J. &amp;amp; Whalley, W. B. Mechanisms of loess-sized quartz silt production and their relative effectiveness: Laboratory simulations. Geomorphology 23, 15-34 (1998).&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
“Silt: Environmental Impact.” Rashid&#039;s Blog: An Educational Portal, 8 May 2016, rashidfaridi.com/2016/03/04/silt-environmental-impact/.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2423</id>
		<title>Silt</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2423"/>
		<updated>2018-05-09T04:44:02Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: /* References */&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==Definition==&lt;br /&gt;
&lt;br /&gt;
[[File:Silty.jpg|thumb|right|Silt [6]]]&lt;br /&gt;
&lt;br /&gt;
Silt is a granular sediment that can be transported and deposited by water, ice, and wind. Silt particles are larger than clay, but smaller than sand. To be classified as silt, a particle must be between .002 to .05 mm [1]. Similarly to [[clay]], sand, and gravel, silt is found in [[soil]]. Silt can also occur as sediment mixed in suspension with water. Because of silt’s spherical shape, it retains a large amount of water. Silty soil is known to be more fertile than other soils, and many species of [[organisms]] thrive in it.&lt;br /&gt;
&lt;br /&gt;
==Formation==&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
Silt-producing mechanisms include frost shattering (Freeze-Thaw Weathering), comminution during transport, eolian abrasion, salt weathering, and glacial grinding. Windblown silt blankets the land in many parts of the world [2]. Large deposits of silt, such as this, are known as loess. Loess landscapes are usually a sign of past glacial activity, including areas such as the Great Plains. Silt can accumulate quickly in areas that lack vegetation, which can disrupt ecosystems. Silt also settles in still water, resulting in build ups like deltas. The main mineral origin of silt is quartz and feldspar.&lt;br /&gt;
&lt;br /&gt;
==Classification==&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
&lt;br /&gt;
*[[Clay]]&lt;br /&gt;
*[[Loam]]&lt;br /&gt;
*[[Founders of Soil Concepts]]&lt;br /&gt;
*[[Humus]]&lt;br /&gt;
*[[Microorganisms]]&lt;br /&gt;
*[[Pedogenesis]]&lt;br /&gt;
*[[Soil]]&lt;br /&gt;
*[[Soil Textures]]&lt;br /&gt;
*[[Soil Properties]] &lt;br /&gt;
*[[Jenny Equation]]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
National Geographic Society. “Silt.” National Geographic Society, 9 Oct. 2012, www.nationalgeographic.org/encyclopedia/silt/.&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
Wright, Janet S. &amp;quot;“Desert” loess versus “glacial” loess: quartz silt formation, source areas and sediment pathways in the formation of loess deposits.&amp;quot; Geomorphology 36.3-4 (2001): 231-256.&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
Wright, J. S., Smith, B. J. &amp;amp; Whalley, W. B. Mechanisms of loess-sized quartz silt production and their relative effectiveness: Laboratory simulations. Geomorphology 23, 15-34 (1998).&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
“Silt: Environmental Impact.” Rashid&#039;s Blog: An Educational Portal, 8 May 2016, rashidfaridi.com/2016/03/04/silt-environmental-impact/.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2417</id>
		<title>Silt</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2417"/>
		<updated>2018-05-09T04:40:40Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: /* Formation */&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==Definition==&lt;br /&gt;
&lt;br /&gt;
[[File:Silty.jpg|thumb|right|Silt [6]]]&lt;br /&gt;
&lt;br /&gt;
Silt is a granular sediment that can be transported and deposited by water, ice, and wind. Silt particles are larger than clay, but smaller than sand. To be classified as silt, a particle must be between .002 to .05 mm [1]. Similarly to [[clay]], sand, and gravel, silt is found in [[soil]]. Silt can also occur as sediment mixed in suspension with water. Because of silt’s spherical shape, it retains a large amount of water. Silty soil is known to be more fertile than other soils, and many species of [[organisms]] thrive in it.&lt;br /&gt;
&lt;br /&gt;
==Formation==&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
Silt-producing mechanisms include frost shattering (Freeze-Thaw Weathering), comminution during transport, eolian abrasion, salt weathering, and glacial grinding. Windblown silt blankets the land in many parts of the world [2]. Large deposits of silt, such as this, are known as loess. Loess landscapes are usually a sign of past glacial activity, including areas such as the Great Plains. Silt can accumulate quickly in areas that lack vegetation, which can disrupt ecosystems. Silt also settles in still water, resulting in build ups like deltas. The main mineral origin of silt is quartz and feldspar.&lt;br /&gt;
&lt;br /&gt;
==Classification==&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
&lt;br /&gt;
*[[Clay]]&lt;br /&gt;
*[[Loam]]&lt;br /&gt;
*[[Founders of Soil Concepts]]&lt;br /&gt;
*[[Humus]]&lt;br /&gt;
*[[Microorganisms]]&lt;br /&gt;
*[[Pedogenesis]]&lt;br /&gt;
*[[Soil]]&lt;br /&gt;
*[[Soil Textures]]&lt;br /&gt;
*[[Soil Properties]] &lt;br /&gt;
*[[Jenny Equation]]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
National Geographic Society. “Silt.” National Geographic Society, 9 Oct. 2012, www.nationalgeographic.org/encyclopedia/silt/.&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
“Silt: Environmental Impact.” Rashid&#039;s Blog: An Educational Portal, 8 May 2016, rashidfaridi.com/2016/03/04/silt-environmental-impact/.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2392</id>
		<title>Silt</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2392"/>
		<updated>2018-05-09T04:23:56Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==Definition==&lt;br /&gt;
&lt;br /&gt;
[[File:Silty.jpg|thumb|right|Silt [6]]]&lt;br /&gt;
&lt;br /&gt;
Silt is a granular sediment that can be transported and deposited by water, ice, and wind. Silt particles are larger than clay, but smaller than sand. To be classified as silt, a particle must be between .002 to .05 mm [1]. Similarly to [[clay]], sand, and gravel, silt is found in [[soil]]. Silt can also occur as sediment mixed in suspension with water. Because of silt’s spherical shape, it retains a large amount of water. Silty soil is known to be more fertile than other soils, and many species of [[organisms]] thrive in it.&lt;br /&gt;
&lt;br /&gt;
==Formation==&lt;br /&gt;
&lt;br /&gt;
==Classification==&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
&lt;br /&gt;
*[[Clay]]&lt;br /&gt;
*[[Loam]]&lt;br /&gt;
*[[Founders of Soil Concepts]]&lt;br /&gt;
*[[Humus]]&lt;br /&gt;
*[[Microorganisms]]&lt;br /&gt;
*[[Pedogenesis]]&lt;br /&gt;
*[[Soil]]&lt;br /&gt;
*[[Soil Textures]]&lt;br /&gt;
*[[Soil Properties]] &lt;br /&gt;
*[[Jenny Equation]]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
National Geographic Society. “Silt.” National Geographic Society, 9 Oct. 2012, www.nationalgeographic.org/encyclopedia/silt/.&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
“Silt: Environmental Impact.” Rashid&#039;s Blog: An Educational Portal, 8 May 2016, rashidfaridi.com/2016/03/04/silt-environmental-impact/.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2385</id>
		<title>Silt</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2385"/>
		<updated>2018-05-09T04:12:48Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: /* Definition */&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==Definition==&lt;br /&gt;
&lt;br /&gt;
[[File:Silty.jpg|thumb|right|Silt [6]]]&lt;br /&gt;
&lt;br /&gt;
Silt is a granular sediment that can be transported and deposited by water, ice, and wind. Silt particles are larger than clay, but smaller than sand. To be classified as silt, a particle must be between .002 to .05 mm [1]. Similarly to [[clay]], sand, and gravel, silt is found in [[soil]]. Silt can also occur as sediment mixed in suspension with water. Because of silt’s spherical shape, it retains a large amount of water. Silty soil is known to be more fertile than other soils, and many species of [[organisms]] thrive in it.&lt;br /&gt;
&lt;br /&gt;
==Classification==&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
==Formation==&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
&lt;br /&gt;
*[[Clay]]&lt;br /&gt;
*[[Loam]]&lt;br /&gt;
*[[Founders of Soil Concepts]]&lt;br /&gt;
*[[Humus]]&lt;br /&gt;
*[[Microorganisms]]&lt;br /&gt;
*[[Pedogenesis]]&lt;br /&gt;
*[[Soil]]&lt;br /&gt;
*[[Soil Textures]]&lt;br /&gt;
*[[Soil Properties]] &lt;br /&gt;
*[[Jenny Equation]]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
National Geographic Society. “Silt.” National Geographic Society, 9 Oct. 2012, www.nationalgeographic.org/encyclopedia/silt/.&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
“Silt: Environmental Impact.” Rashid&#039;s Blog: An Educational Portal, 8 May 2016, rashidfaridi.com/2016/03/04/silt-environmental-impact/.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2384</id>
		<title>Silt</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2384"/>
		<updated>2018-05-09T04:12:19Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: /* References */&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==Definition==&lt;br /&gt;
&lt;br /&gt;
[[File:Silty.jpg|thumb|right|Silt [6]]]&lt;br /&gt;
&lt;br /&gt;
Silt is a granular sediment that can be transported and deposited by water, ice, and wind. Silt particles are larger than clay, but smaller than sand. To be classified as silt, a particle must be between .05 to .002 mm [1]. Similarly to [[clay]], sand, and gravel, silt is found in [[soil]]. Silt can also occur as sediment mixed in suspension with water. Because of silt’s spherical shape, it retains a large amount of water. Silty soil is known to be more fertile than other soils, and many species of [[organisms]] thrive in it.&lt;br /&gt;
&lt;br /&gt;
==Classification==&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
==Formation==&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
&lt;br /&gt;
*[[Clay]]&lt;br /&gt;
*[[Loam]]&lt;br /&gt;
*[[Founders of Soil Concepts]]&lt;br /&gt;
*[[Humus]]&lt;br /&gt;
*[[Microorganisms]]&lt;br /&gt;
*[[Pedogenesis]]&lt;br /&gt;
*[[Soil]]&lt;br /&gt;
*[[Soil Textures]]&lt;br /&gt;
*[[Soil Properties]] &lt;br /&gt;
*[[Jenny Equation]]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
National Geographic Society. “Silt.” National Geographic Society, 9 Oct. 2012, www.nationalgeographic.org/encyclopedia/silt/.&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
“Silt: Environmental Impact.” Rashid&#039;s Blog: An Educational Portal, 8 May 2016, rashidfaridi.com/2016/03/04/silt-environmental-impact/.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2376</id>
		<title>Silt</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2376"/>
		<updated>2018-05-09T04:02:03Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: /* Definition */&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==Definition==&lt;br /&gt;
&lt;br /&gt;
[[File:Silty.jpg|thumb|right|Silt [6]]]&lt;br /&gt;
&lt;br /&gt;
Silt is a granular sediment that can be transported and deposited by water, ice, and wind. Silt particles are larger than clay, but smaller than sand. To be classified as silt, a particle must be between .05 to .002 mm [1]. Similarly to [[clay]], sand, and gravel, silt is found in [[soil]]. Silt can also occur as sediment mixed in suspension with water. Because of silt’s spherical shape, it retains a large amount of water. Silty soil is known to be more fertile than other soils, and many species of [[organisms]] thrive in it.&lt;br /&gt;
&lt;br /&gt;
==Classification==&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
==Formation==&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
&lt;br /&gt;
*[[Clay]]&lt;br /&gt;
*[[Loam]]&lt;br /&gt;
*[[Founders of Soil Concepts]]&lt;br /&gt;
*[[Humus]]&lt;br /&gt;
*[[Microorganisms]]&lt;br /&gt;
*[[Pedogenesis]]&lt;br /&gt;
*[[Soil]]&lt;br /&gt;
*[[Soil Textures]]&lt;br /&gt;
*[[Soil Properties]] &lt;br /&gt;
*[[Jenny Equation]]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
Walter, David Evans, Gerald Krantz, and Evert Lindquist. 1996. Acari. The Mites. Version 13 December 1996. http://tolweb.org/Acari/2554/1996.12.13 inThe Tree of Life Web Project, http://tolweb.org/&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
Pepato, Almir R, et al. “Phylogenetic Position of the Acariform Mites: Sensitivity to Homology Assessment under Total Evidence.” BMC Evolutionary Biology, BioMed Central, 2 Aug. 2010, bmcevolbiol.biomedcentral.com/articles/10.1186/1471-2148-10-235.&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
Sanggaard, Kristian W.; Bechsgaard, Jesper S.; Fang, Xiaodong (6 May 2014). &amp;quot;Spider genomes provide insight into composition and evolution of venom and silk&amp;quot;. Nature Communications. 5: 3765. Bibcode:2014NatCo...5E3765S. doi:10.1038/ncomms4765. PMC 4273655 Freely accessible. PMID 24801114.&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
Dhooria M.S. (2016) Morphology and Anatomy of Acari. In: Fundamentals of Applied Acarology. Springer, Singapore&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
“Acari.” Acari - Entomologists&#039; Glossary - Amateur Entomologists&#039; Society (AES), www.amentsoc.org/insects/glossary/terms/acari.&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
Wilson, Nixon A. “Acarid.” Encyclopædia Britannica, Encyclopædia Britannica, Inc., 27 Dec. 2017, www.britannica.com/animal/acarid.&lt;br /&gt;
&lt;br /&gt;
[7]&lt;br /&gt;
NCSU Veterinary Parasitology, parasitology.cvm.ncsu.edu/vmp930/keys/mites/miteterms.html.&lt;br /&gt;
&lt;br /&gt;
[8]&lt;br /&gt;
Gulvik, M. &amp;quot;Mites (Acari) as indicators of soil biodiversity and land use monitoring: a review.&amp;quot; Polish Journal of Ecology 55.3 (2007): 415.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2373</id>
		<title>Silt</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2373"/>
		<updated>2018-05-09T03:58:37Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: /* Definition */&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==Definition==&lt;br /&gt;
&lt;br /&gt;
[[File:Silty.jpg|thumb|right|Silt [6]]]&lt;br /&gt;
&lt;br /&gt;
Silt is a dust-like sediment that can be transported and deposited by water, ice, and wind. Silt particles are larger than clay, but smaller than sand. To be classified as silt, a particle must be between .05 to .002 mm [1]. Similarly to [[clay]], sand, and gravel, silt is found in [[soil]]. Silt can also occur as sediment mixed in suspension with water. Because of silt’s spherical shape, it retains a large amount of water. Silty soil is known to be more fertile than other soils, and many species of [[organisms]] thrive in it.&lt;br /&gt;
&lt;br /&gt;
==Classification==&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
==Formation==&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
&lt;br /&gt;
*[[Clay]]&lt;br /&gt;
*[[Loam]]&lt;br /&gt;
*[[Founders of Soil Concepts]]&lt;br /&gt;
*[[Humus]]&lt;br /&gt;
*[[Microorganisms]]&lt;br /&gt;
*[[Pedogenesis]]&lt;br /&gt;
*[[Soil]]&lt;br /&gt;
*[[Soil Textures]]&lt;br /&gt;
*[[Soil Properties]] &lt;br /&gt;
*[[Jenny Equation]]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
Walter, David Evans, Gerald Krantz, and Evert Lindquist. 1996. Acari. The Mites. Version 13 December 1996. http://tolweb.org/Acari/2554/1996.12.13 inThe Tree of Life Web Project, http://tolweb.org/&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
Pepato, Almir R, et al. “Phylogenetic Position of the Acariform Mites: Sensitivity to Homology Assessment under Total Evidence.” BMC Evolutionary Biology, BioMed Central, 2 Aug. 2010, bmcevolbiol.biomedcentral.com/articles/10.1186/1471-2148-10-235.&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
Sanggaard, Kristian W.; Bechsgaard, Jesper S.; Fang, Xiaodong (6 May 2014). &amp;quot;Spider genomes provide insight into composition and evolution of venom and silk&amp;quot;. Nature Communications. 5: 3765. Bibcode:2014NatCo...5E3765S. doi:10.1038/ncomms4765. PMC 4273655 Freely accessible. PMID 24801114.&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
Dhooria M.S. (2016) Morphology and Anatomy of Acari. In: Fundamentals of Applied Acarology. Springer, Singapore&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
“Acari.” Acari - Entomologists&#039; Glossary - Amateur Entomologists&#039; Society (AES), www.amentsoc.org/insects/glossary/terms/acari.&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
Wilson, Nixon A. “Acarid.” Encyclopædia Britannica, Encyclopædia Britannica, Inc., 27 Dec. 2017, www.britannica.com/animal/acarid.&lt;br /&gt;
&lt;br /&gt;
[7]&lt;br /&gt;
NCSU Veterinary Parasitology, parasitology.cvm.ncsu.edu/vmp930/keys/mites/miteterms.html.&lt;br /&gt;
&lt;br /&gt;
[8]&lt;br /&gt;
Gulvik, M. &amp;quot;Mites (Acari) as indicators of soil biodiversity and land use monitoring: a review.&amp;quot; Polish Journal of Ecology 55.3 (2007): 415.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2370</id>
		<title>Silt</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2370"/>
		<updated>2018-05-09T03:56:45Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: /* Definition */&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==Definition==&lt;br /&gt;
&lt;br /&gt;
[[File:Silty.jpg|thumb|right|Silt [6]]]&lt;br /&gt;
&lt;br /&gt;
Silt is a dust-like sediment that can be transported and deposited by water, ice, and wind. Silt particles are larger than clay, but smaller than sand. To be classified as silt, a particle must be between .05 to .002 mm. Similarly to clay, sand, and gravel, silt is found in soil. Silt can also occur as sediment mixed in suspension with water. Because of silt’s spherical shape, it retains a large amount of water. Silty soil is known to be more fertile than other soils, and many species of organisms thrive in it.&lt;br /&gt;
&lt;br /&gt;
==Classification==&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
==Formation==&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
&lt;br /&gt;
*[[Clay]]&lt;br /&gt;
*[[Loam]]&lt;br /&gt;
*[[Founders of Soil Concepts]]&lt;br /&gt;
*[[Humus]]&lt;br /&gt;
*[[Microorganisms]]&lt;br /&gt;
*[[Pedogenesis]]&lt;br /&gt;
*[[Soil]]&lt;br /&gt;
*[[Soil Textures]]&lt;br /&gt;
*[[Soil Properties]] &lt;br /&gt;
*[[Jenny Equation]]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
Walter, David Evans, Gerald Krantz, and Evert Lindquist. 1996. Acari. The Mites. Version 13 December 1996. http://tolweb.org/Acari/2554/1996.12.13 inThe Tree of Life Web Project, http://tolweb.org/&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
Pepato, Almir R, et al. “Phylogenetic Position of the Acariform Mites: Sensitivity to Homology Assessment under Total Evidence.” BMC Evolutionary Biology, BioMed Central, 2 Aug. 2010, bmcevolbiol.biomedcentral.com/articles/10.1186/1471-2148-10-235.&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
Sanggaard, Kristian W.; Bechsgaard, Jesper S.; Fang, Xiaodong (6 May 2014). &amp;quot;Spider genomes provide insight into composition and evolution of venom and silk&amp;quot;. Nature Communications. 5: 3765. Bibcode:2014NatCo...5E3765S. doi:10.1038/ncomms4765. PMC 4273655 Freely accessible. PMID 24801114.&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
Dhooria M.S. (2016) Morphology and Anatomy of Acari. In: Fundamentals of Applied Acarology. Springer, Singapore&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
“Acari.” Acari - Entomologists&#039; Glossary - Amateur Entomologists&#039; Society (AES), www.amentsoc.org/insects/glossary/terms/acari.&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
Wilson, Nixon A. “Acarid.” Encyclopædia Britannica, Encyclopædia Britannica, Inc., 27 Dec. 2017, www.britannica.com/animal/acarid.&lt;br /&gt;
&lt;br /&gt;
[7]&lt;br /&gt;
NCSU Veterinary Parasitology, parasitology.cvm.ncsu.edu/vmp930/keys/mites/miteterms.html.&lt;br /&gt;
&lt;br /&gt;
[8]&lt;br /&gt;
Gulvik, M. &amp;quot;Mites (Acari) as indicators of soil biodiversity and land use monitoring: a review.&amp;quot; Polish Journal of Ecology 55.3 (2007): 415.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2368</id>
		<title>Silt</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2368"/>
		<updated>2018-05-09T03:56:26Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: /* Definition */&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==Definition==&lt;br /&gt;
&lt;br /&gt;
[[File:Silty.jpg|thumb|right|Silt [6]]]&lt;br /&gt;
&lt;br /&gt;
 Silt is a dust-like sediment that can be transported and deposited by water, ice, and wind. Silt particles are larger than clay, but smaller than sand. To be classified as silt, a particle must be between .05 to .002 mm. Similarly to clay, sand, and gravel, silt is found in soil. Silt can also occur as sediment mixed in suspension with water. Because of silt’s spherical shape, it retains a large amount of water. Silty soil is known to be more fertile than other soils, and many species of organisms thrive in it.&lt;br /&gt;
&lt;br /&gt;
==Classification==&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
==Formation==&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
&lt;br /&gt;
*[[Clay]]&lt;br /&gt;
*[[Loam]]&lt;br /&gt;
*[[Founders of Soil Concepts]]&lt;br /&gt;
*[[Humus]]&lt;br /&gt;
*[[Microorganisms]]&lt;br /&gt;
*[[Pedogenesis]]&lt;br /&gt;
*[[Soil]]&lt;br /&gt;
*[[Soil Textures]]&lt;br /&gt;
*[[Soil Properties]] &lt;br /&gt;
*[[Jenny Equation]]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
Walter, David Evans, Gerald Krantz, and Evert Lindquist. 1996. Acari. The Mites. Version 13 December 1996. http://tolweb.org/Acari/2554/1996.12.13 inThe Tree of Life Web Project, http://tolweb.org/&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
Pepato, Almir R, et al. “Phylogenetic Position of the Acariform Mites: Sensitivity to Homology Assessment under Total Evidence.” BMC Evolutionary Biology, BioMed Central, 2 Aug. 2010, bmcevolbiol.biomedcentral.com/articles/10.1186/1471-2148-10-235.&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
Sanggaard, Kristian W.; Bechsgaard, Jesper S.; Fang, Xiaodong (6 May 2014). &amp;quot;Spider genomes provide insight into composition and evolution of venom and silk&amp;quot;. Nature Communications. 5: 3765. Bibcode:2014NatCo...5E3765S. doi:10.1038/ncomms4765. PMC 4273655 Freely accessible. PMID 24801114.&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
Dhooria M.S. (2016) Morphology and Anatomy of Acari. In: Fundamentals of Applied Acarology. Springer, Singapore&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
“Acari.” Acari - Entomologists&#039; Glossary - Amateur Entomologists&#039; Society (AES), www.amentsoc.org/insects/glossary/terms/acari.&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
Wilson, Nixon A. “Acarid.” Encyclopædia Britannica, Encyclopædia Britannica, Inc., 27 Dec. 2017, www.britannica.com/animal/acarid.&lt;br /&gt;
&lt;br /&gt;
[7]&lt;br /&gt;
NCSU Veterinary Parasitology, parasitology.cvm.ncsu.edu/vmp930/keys/mites/miteterms.html.&lt;br /&gt;
&lt;br /&gt;
[8]&lt;br /&gt;
Gulvik, M. &amp;quot;Mites (Acari) as indicators of soil biodiversity and land use monitoring: a review.&amp;quot; Polish Journal of Ecology 55.3 (2007): 415.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=File:Silty.jpg&amp;diff=2367</id>
		<title>File:Silty.jpg</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=File:Silty.jpg&amp;diff=2367"/>
		<updated>2018-05-09T03:55:43Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2345</id>
		<title>Silt</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2345"/>
		<updated>2018-05-09T03:37:41Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: /* Definition */&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==Definition==&lt;br /&gt;
&lt;br /&gt;
[[File:lorryia-formosa-mite.jpg|thumb|right|Lorryia formosa mite [5]]]&lt;br /&gt;
&lt;br /&gt;
Silt particles are larger than clay, but smaller than sand. Silt is a dust-like sediment that can be transported and deposited by water, ice, and wind. To be classified as silt, a particle must be less than .005 centimeters across. Similarly to clay, sand, and gravel, silt is found in soil. Silt can also occur as sediment mixed in suspension with water. Because of silt’s spherical shape, it retains a large amount of water. Silty soil is known to be more fertile than other soils, and many species of organisms thrive in it.&lt;br /&gt;
&lt;br /&gt;
==Classification==&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
==Formation==&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
&lt;br /&gt;
*[[Clay]]&lt;br /&gt;
*[[Loam]]&lt;br /&gt;
*[[Founders of Soil Concepts]]&lt;br /&gt;
*[[Humus]]&lt;br /&gt;
*[[Microorganisms]]&lt;br /&gt;
*[[Pedogenesis]]&lt;br /&gt;
*[[Soil]]&lt;br /&gt;
*[[Soil Textures]]&lt;br /&gt;
*[[Soil Properties]] &lt;br /&gt;
*[[Jenny Equation]]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
Walter, David Evans, Gerald Krantz, and Evert Lindquist. 1996. Acari. The Mites. Version 13 December 1996. http://tolweb.org/Acari/2554/1996.12.13 inThe Tree of Life Web Project, http://tolweb.org/&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
Pepato, Almir R, et al. “Phylogenetic Position of the Acariform Mites: Sensitivity to Homology Assessment under Total Evidence.” BMC Evolutionary Biology, BioMed Central, 2 Aug. 2010, bmcevolbiol.biomedcentral.com/articles/10.1186/1471-2148-10-235.&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
Sanggaard, Kristian W.; Bechsgaard, Jesper S.; Fang, Xiaodong (6 May 2014). &amp;quot;Spider genomes provide insight into composition and evolution of venom and silk&amp;quot;. Nature Communications. 5: 3765. Bibcode:2014NatCo...5E3765S. doi:10.1038/ncomms4765. PMC 4273655 Freely accessible. PMID 24801114.&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
Dhooria M.S. (2016) Morphology and Anatomy of Acari. In: Fundamentals of Applied Acarology. Springer, Singapore&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
“Acari.” Acari - Entomologists&#039; Glossary - Amateur Entomologists&#039; Society (AES), www.amentsoc.org/insects/glossary/terms/acari.&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
Wilson, Nixon A. “Acarid.” Encyclopædia Britannica, Encyclopædia Britannica, Inc., 27 Dec. 2017, www.britannica.com/animal/acarid.&lt;br /&gt;
&lt;br /&gt;
[7]&lt;br /&gt;
NCSU Veterinary Parasitology, parasitology.cvm.ncsu.edu/vmp930/keys/mites/miteterms.html.&lt;br /&gt;
&lt;br /&gt;
[8]&lt;br /&gt;
Gulvik, M. &amp;quot;Mites (Acari) as indicators of soil biodiversity and land use monitoring: a review.&amp;quot; Polish Journal of Ecology 55.3 (2007): 415.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2333</id>
		<title>Silt</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2333"/>
		<updated>2018-05-09T03:26:51Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: /* Definition */&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==Definition==&lt;br /&gt;
&lt;br /&gt;
[[File:lorryia-formosa-mite.jpg|thumb|right|Lorryia formosa mite [5]]]&lt;br /&gt;
&lt;br /&gt;
Silt particles are larger than clay, but smaller than sand. To be classified as silt, a particle must be less than .005 centimeters across. Similarly to clay, sand, and gravel, silt is found in soil. Silt can also occur as sediment mixed in suspension with water. It is a dust-like sediment that can be transported and deposited by water, ice, and wind. Because of silt’s spherical shape, silt retains a large amount of water. Silty soil is known to be more fertile than other soils, and many species of organisms thrive in it.&lt;br /&gt;
&lt;br /&gt;
==Classification==&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
==Formation==&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
&lt;br /&gt;
*[[Clay]]&lt;br /&gt;
*[[Loam]]&lt;br /&gt;
*[[Founders of Soil Concepts]]&lt;br /&gt;
*[[Humus]]&lt;br /&gt;
*[[Microorganisms]]&lt;br /&gt;
*[[Pedogenesis]]&lt;br /&gt;
*[[Soil]]&lt;br /&gt;
*[[Soil Textures]]&lt;br /&gt;
*[[Soil Properties]] &lt;br /&gt;
*[[Jenny Equation]]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
Walter, David Evans, Gerald Krantz, and Evert Lindquist. 1996. Acari. The Mites. Version 13 December 1996. http://tolweb.org/Acari/2554/1996.12.13 inThe Tree of Life Web Project, http://tolweb.org/&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
Pepato, Almir R, et al. “Phylogenetic Position of the Acariform Mites: Sensitivity to Homology Assessment under Total Evidence.” BMC Evolutionary Biology, BioMed Central, 2 Aug. 2010, bmcevolbiol.biomedcentral.com/articles/10.1186/1471-2148-10-235.&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
Sanggaard, Kristian W.; Bechsgaard, Jesper S.; Fang, Xiaodong (6 May 2014). &amp;quot;Spider genomes provide insight into composition and evolution of venom and silk&amp;quot;. Nature Communications. 5: 3765. Bibcode:2014NatCo...5E3765S. doi:10.1038/ncomms4765. PMC 4273655 Freely accessible. PMID 24801114.&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
Dhooria M.S. (2016) Morphology and Anatomy of Acari. In: Fundamentals of Applied Acarology. Springer, Singapore&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
“Acari.” Acari - Entomologists&#039; Glossary - Amateur Entomologists&#039; Society (AES), www.amentsoc.org/insects/glossary/terms/acari.&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
Wilson, Nixon A. “Acarid.” Encyclopædia Britannica, Encyclopædia Britannica, Inc., 27 Dec. 2017, www.britannica.com/animal/acarid.&lt;br /&gt;
&lt;br /&gt;
[7]&lt;br /&gt;
NCSU Veterinary Parasitology, parasitology.cvm.ncsu.edu/vmp930/keys/mites/miteterms.html.&lt;br /&gt;
&lt;br /&gt;
[8]&lt;br /&gt;
Gulvik, M. &amp;quot;Mites (Acari) as indicators of soil biodiversity and land use monitoring: a review.&amp;quot; Polish Journal of Ecology 55.3 (2007): 415.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2313</id>
		<title>Silt</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Silt&amp;diff=2313"/>
		<updated>2018-05-09T03:16:18Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: Created page with &amp;quot;==Definition==  Lorryia formosa mite [5]  ==Classification==   ==Formation==   ==See also==  *Clay *Loam *Founders of S...&amp;quot;&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==Definition==&lt;br /&gt;
&lt;br /&gt;
[[File:lorryia-formosa-mite.jpg|thumb|right|Lorryia formosa mite [5]]]&lt;br /&gt;
&lt;br /&gt;
==Classification==&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
==Formation==&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
&lt;br /&gt;
*[[Clay]]&lt;br /&gt;
*[[Loam]]&lt;br /&gt;
*[[Founders of Soil Concepts]]&lt;br /&gt;
*[[Humus]]&lt;br /&gt;
*[[Microorganisms]]&lt;br /&gt;
*[[Pedogenesis]]&lt;br /&gt;
*[[Soil]]&lt;br /&gt;
*[[Soil Textures]]&lt;br /&gt;
*[[Soil Properties]] &lt;br /&gt;
*[[Jenny Equation]]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
Walter, David Evans, Gerald Krantz, and Evert Lindquist. 1996. Acari. The Mites. Version 13 December 1996. http://tolweb.org/Acari/2554/1996.12.13 inThe Tree of Life Web Project, http://tolweb.org/&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
Pepato, Almir R, et al. “Phylogenetic Position of the Acariform Mites: Sensitivity to Homology Assessment under Total Evidence.” BMC Evolutionary Biology, BioMed Central, 2 Aug. 2010, bmcevolbiol.biomedcentral.com/articles/10.1186/1471-2148-10-235.&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
Sanggaard, Kristian W.; Bechsgaard, Jesper S.; Fang, Xiaodong (6 May 2014). &amp;quot;Spider genomes provide insight into composition and evolution of venom and silk&amp;quot;. Nature Communications. 5: 3765. Bibcode:2014NatCo...5E3765S. doi:10.1038/ncomms4765. PMC 4273655 Freely accessible. PMID 24801114.&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
Dhooria M.S. (2016) Morphology and Anatomy of Acari. In: Fundamentals of Applied Acarology. Springer, Singapore&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
“Acari.” Acari - Entomologists&#039; Glossary - Amateur Entomologists&#039; Society (AES), www.amentsoc.org/insects/glossary/terms/acari.&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
Wilson, Nixon A. “Acarid.” Encyclopædia Britannica, Encyclopædia Britannica, Inc., 27 Dec. 2017, www.britannica.com/animal/acarid.&lt;br /&gt;
&lt;br /&gt;
[7]&lt;br /&gt;
NCSU Veterinary Parasitology, parasitology.cvm.ncsu.edu/vmp930/keys/mites/miteterms.html.&lt;br /&gt;
&lt;br /&gt;
[8]&lt;br /&gt;
Gulvik, M. &amp;quot;Mites (Acari) as indicators of soil biodiversity and land use monitoring: a review.&amp;quot; Polish Journal of Ecology 55.3 (2007): 415.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Vegetable_Mould&amp;diff=2283</id>
		<title>Vegetable Mould</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Vegetable_Mould&amp;diff=2283"/>
		<updated>2018-05-09T02:50:32Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: /* See also */&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==Definition==&lt;br /&gt;
&lt;br /&gt;
[[File:vegetable.jpg|thumb|right|Image from Darwin&#039;s book, The Formation of Vegetable Mould through the Action of Worms, with Observations on their Habits [7]]]&lt;br /&gt;
Vegetable mould is the layer of dark colored, uniformly fine soil particles that cover the surface of land in moderately humid climates. This layer of mould, known as a form of soil [[humus]], can reach a depth of 40 cm or more in the soil profile. Earthworm secretions (or castings) primarily compose vegetable mould, and the layer is a few inches thick. Vegetable mould is located in the O Horizon of the [[Soil Horizons]].&lt;br /&gt;
&lt;br /&gt;
==Earthworm Contribution==&lt;br /&gt;
&lt;br /&gt;
Earthworms sift the finer soils from the coarser, mix the soil with mineral particles, and saturate it with intestinal secretion. Earthworm burrowing, casting, grazing, and dispersal change the soil&#039;s physico-chemical and biological status and could cause drastic shifts in the density, [[diversity]], structure and activity within the drilosphere. [1] While feeding, earthworms promote microbial activity that accelerate the rates of breakdown and stabilization of humic portions of organic matter. &lt;br /&gt;
&lt;br /&gt;
[[File:wormss.jpg|frame|left|Drawing of earthworm castings [7]]]&lt;br /&gt;
&lt;br /&gt;
==Observations and Experiments== &lt;br /&gt;
&lt;br /&gt;
Charles Darwin first noted the importance of earthworm species in the creation of vegetable mould in his book, “The Formation of Vegetable Mould, through the Action of Worms, with Observations on their Habits”. [2] Darwin cited results from a number of his experiments which showed, annually, 0.5 cm of soil is brought to the surface in worm casts. Most earthworms live at a soil depth of 25-30 cm, and therefore, this surface soil is worked over most thoroughly. [3] Darwin has observed through experiemnts a value of 18.12 tons of earth per acre is brought to the surface in dry casts. The constant production of vegetable mould by earthworms can be observed by the estimated rate at which objects on the surface are buried and by weighing the earth brought up in a given time. Vegetable mould and worms are able to preserve ancient objects under the ground.&lt;br /&gt;
&lt;br /&gt;
[[File:Veggie.jpeg|frame|120x60px|[7]]]&lt;br /&gt;
&lt;br /&gt;
==Mould Benefits==&lt;br /&gt;
&lt;br /&gt;
Vegetable mould creates fertile soil. Earthworms prepare the ground for the growth of fibrous-rooted plants and many types of seedlings; they help to expose and sift the vegetable mould. With vegetable mould, soil is in a state fitted to retain moisture and absorb soluble substances. [4] Nitrification is possible with vegetable mould in soil, as well. The constant movement by worms in soil allows for materials to be buried beneath accumulated castings of worms, and then brought to a decayed state. [5] All humic substances are able to chelate soil nutrients and act as a storehouse of Nitrogen, Phosphorus, Sulphur and Zinc. Humic substances can also improve nutrient uptake, especially phosphorous, sulfur, and nitrogen. [6]&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
&lt;br /&gt;
*[[Soil]]&lt;br /&gt;
*[[Soil Horizons]]&lt;br /&gt;
*[[Soil Textures]]&lt;br /&gt;
*[[Founders of Soil Concepts]]&lt;br /&gt;
*[[Humus]]&lt;br /&gt;
*[[Annelids]]&lt;br /&gt;
*[[Animals]]&lt;br /&gt;
&lt;br /&gt;
==References== &lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
Edwards, Clive A., ed. Earthworm ecology. CRC press, 2004.&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
Darwin, Charles, 1809-1882. The Formation of Vegetable Mould, through the Action of Worms, with Observations on their Habits. J. Murray, London, 1892.&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
Hayes, M. B. &amp;quot;Darwin’s ‘vegetable mould’ and some modern concepts of humus structure and soil aggregation.&amp;quot; Earthworm Ecology. Springer, Dordrecht, 1983. 19-33.&lt;br /&gt;
&lt;br /&gt;
[4] &lt;br /&gt;
Martin, J. P., and K. Haider. &amp;quot;Microbial activity in relation to soil humus formation.&amp;quot; Soil Science 111.1 (1971): 54-63.&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
Wild, Alan. Soils and the Environment: An Introduction. Cambridge University Press, New York, NY, USA;Cambridge;, 1993.&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
Mayhew, Lawrence. &amp;quot;Humic substances in biological agriculture.&amp;quot; Rev ACRES 34.1-2 (2004): 80-88.&lt;br /&gt;
&lt;br /&gt;
[7]&lt;br /&gt;
“THE FORMATION OF VEGETABLE MOULD THROUGH THE ACTION OF WORMS WITH OBSERVATIONS ON THEIR HABITS.” The Formation of Vegetable Mould, by Charles Darwin, www.gutenberg.org/files/2355/2355-h/2355-h.htm.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Vegetable_Mould&amp;diff=2281</id>
		<title>Vegetable Mould</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Vegetable_Mould&amp;diff=2281"/>
		<updated>2018-05-09T02:49:37Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==Definition==&lt;br /&gt;
&lt;br /&gt;
[[File:vegetable.jpg|thumb|right|Image from Darwin&#039;s book, The Formation of Vegetable Mould through the Action of Worms, with Observations on their Habits [7]]]&lt;br /&gt;
Vegetable mould is the layer of dark colored, uniformly fine soil particles that cover the surface of land in moderately humid climates. This layer of mould, known as a form of soil [[humus]], can reach a depth of 40 cm or more in the soil profile. Earthworm secretions (or castings) primarily compose vegetable mould, and the layer is a few inches thick. Vegetable mould is located in the O Horizon of the [[Soil Horizons]].&lt;br /&gt;
&lt;br /&gt;
==Earthworm Contribution==&lt;br /&gt;
&lt;br /&gt;
Earthworms sift the finer soils from the coarser, mix the soil with mineral particles, and saturate it with intestinal secretion. Earthworm burrowing, casting, grazing, and dispersal change the soil&#039;s physico-chemical and biological status and could cause drastic shifts in the density, [[diversity]], structure and activity within the drilosphere. [1] While feeding, earthworms promote microbial activity that accelerate the rates of breakdown and stabilization of humic portions of organic matter. &lt;br /&gt;
&lt;br /&gt;
[[File:wormss.jpg|frame|left|Drawing of earthworm castings [7]]]&lt;br /&gt;
&lt;br /&gt;
==Observations and Experiments== &lt;br /&gt;
&lt;br /&gt;
Charles Darwin first noted the importance of earthworm species in the creation of vegetable mould in his book, “The Formation of Vegetable Mould, through the Action of Worms, with Observations on their Habits”. [2] Darwin cited results from a number of his experiments which showed, annually, 0.5 cm of soil is brought to the surface in worm casts. Most earthworms live at a soil depth of 25-30 cm, and therefore, this surface soil is worked over most thoroughly. [3] Darwin has observed through experiemnts a value of 18.12 tons of earth per acre is brought to the surface in dry casts. The constant production of vegetable mould by earthworms can be observed by the estimated rate at which objects on the surface are buried and by weighing the earth brought up in a given time. Vegetable mould and worms are able to preserve ancient objects under the ground.&lt;br /&gt;
&lt;br /&gt;
[[File:Veggie.jpeg|frame|120x60px|[7]]]&lt;br /&gt;
&lt;br /&gt;
==Mould Benefits==&lt;br /&gt;
&lt;br /&gt;
Vegetable mould creates fertile soil. Earthworms prepare the ground for the growth of fibrous-rooted plants and many types of seedlings; they help to expose and sift the vegetable mould. With vegetable mould, soil is in a state fitted to retain moisture and absorb soluble substances. [4] Nitrification is possible with vegetable mould in soil, as well. The constant movement by worms in soil allows for materials to be buried beneath accumulated castings of worms, and then brought to a decayed state. [5] All humic substances are able to chelate soil nutrients and act as a storehouse of Nitrogen, Phosphorus, Sulphur and Zinc. Humic substances can also improve nutrient uptake, especially phosphorous, sulfur, and nitrogen. [6]&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
&lt;br /&gt;
*[[Soil]]&lt;br /&gt;
*[[Soil Horizons]]&lt;br /&gt;
*[[Soil Texture]]&lt;br /&gt;
*[[Founders of Soil Concepts]]&lt;br /&gt;
*[[Humus]]&lt;br /&gt;
*[[Annelids]]&lt;br /&gt;
*[[Animals]]&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
==References== &lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
Edwards, Clive A., ed. Earthworm ecology. CRC press, 2004.&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
Darwin, Charles, 1809-1882. The Formation of Vegetable Mould, through the Action of Worms, with Observations on their Habits. J. Murray, London, 1892.&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
Hayes, M. B. &amp;quot;Darwin’s ‘vegetable mould’ and some modern concepts of humus structure and soil aggregation.&amp;quot; Earthworm Ecology. Springer, Dordrecht, 1983. 19-33.&lt;br /&gt;
&lt;br /&gt;
[4] &lt;br /&gt;
Martin, J. P., and K. Haider. &amp;quot;Microbial activity in relation to soil humus formation.&amp;quot; Soil Science 111.1 (1971): 54-63.&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
Wild, Alan. Soils and the Environment: An Introduction. Cambridge University Press, New York, NY, USA;Cambridge;, 1993.&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
Mayhew, Lawrence. &amp;quot;Humic substances in biological agriculture.&amp;quot; Rev ACRES 34.1-2 (2004): 80-88.&lt;br /&gt;
&lt;br /&gt;
[7]&lt;br /&gt;
“THE FORMATION OF VEGETABLE MOULD THROUGH THE ACTION OF WORMS WITH OBSERVATIONS ON THEIR HABITS.” The Formation of Vegetable Mould, by Charles Darwin, www.gutenberg.org/files/2355/2355-h/2355-h.htm.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Mites&amp;diff=2277</id>
		<title>Mites</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Mites&amp;diff=2277"/>
		<updated>2018-05-09T02:44:38Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: /* See also */&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==Definition==&lt;br /&gt;
&lt;br /&gt;
[[File:lorryia-formosa-mite.jpg|thumb|right|Lorryia formosa mite [5]]]&lt;br /&gt;
Mites are the most diverse of all arachnids, and among the oldest of all terrestrial animals. Fossils date mites from the early Devonian, nearly 400 million years ago [1.] Belonging to the class Archnida, the term &amp;quot;mite&amp;quot; refers to the several groups in the subclass Acari, but it is not a clade, and excludes the ticks. Mites and ticks are similarly characterized by their bodies being divided into two parts, named the gnathosoma and idiosoma. The three major lineages of mites are recognized as Opilioacariformes, Acariformes and Parasitiformes [1]. 45,000 species of mites have been described, which is believed to be only small 5% of the number of species estimated to be alive today. Mites can be found throughout the planet in every kind of habitat from the sea to freshwater, and in all terrestrial habitats, including soil, tree canopy, rotting woods, tree hollows, nests of vertebrates, dung and anthills [8].  In most studies, the scientists use the Berlese-Tullgren funnel to extract microarthropods from soil samples ([[Soil Sampling Methods]]). The soil sample size is often about 5 cm in diameter and 5 cm depth. Most mites in native soils occur in the top [[Soil Horizons]] [8].&lt;br /&gt;
&lt;br /&gt;
==Characteristics==&lt;br /&gt;
&lt;br /&gt;
&#039;&#039;A Manual of Acarology&#039;&#039; has defined Acari to have the following characteristics [1]:&lt;br /&gt;
&lt;br /&gt;
*Hexapod prelarva (lost in Parasitiformes and many derived Acariformes)&lt;br /&gt;
&lt;br /&gt;
*Hexapod larval stage&lt;br /&gt;
&lt;br /&gt;
*Three octopod nymphal stages (variously abbreviated in derived taxa)&lt;br /&gt;
&lt;br /&gt;
*Gnathosoma delimited by a circumcapitular suture&lt;br /&gt;
&lt;br /&gt;
*Palpcoxal endites fused medially forming a hypostome&lt;br /&gt;
&lt;br /&gt;
*Hypostome with rutella or corniculi (lost in many derived Acariformes)&lt;br /&gt;
&lt;br /&gt;
*Loss of external evidence of opisthosomal segmentation, i.e. without tergites or sternites&lt;br /&gt;
&lt;br /&gt;
*Ingestion of particulate food (lost in many derived taxa)&lt;br /&gt;
&lt;br /&gt;
==Taxonomy==&lt;br /&gt;
&lt;br /&gt;
[[File:diversity of acari.jpg|thumb|right|Diversity of Acari [6]]]&lt;br /&gt;
Acari have been variously ranked as a group made up of one to seven or more distinct orders. The orders comprise approximately half of the described arachnid [[diversity]]. Molecular information from ribosomal DNA is used to expose relationships between groups. The 18 S rRNA gene provides information on relationships among phyla and superphyla, while the ITS2, and the 18S ribosomal RNA and 28S ribosomal RNA genes, show relationships at deeper levels [2]. Recent research has suggested that Acari is polyphyletic [3]. &#039;&#039;A Manual of Acarology&#039;&#039; uses a system of six orders, grouped into three superorders to classify Acari [2]:&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
*Superorder Opilioacariformes – a small order of large mites with about 20 known species&lt;br /&gt;
*Superorder Parasitiformes – ticks and a variety of mites&lt;br /&gt;
**Holothyrida - predatory mites from the southern hemisphere&lt;br /&gt;
**Ixodida – hard ticks and soft ticks&lt;br /&gt;
**Mesostigmata – excess of 65 families and 10,000 described species, including bird mites, phytoseiid mites&lt;br /&gt;
***Trigynaspida - large, diverse order&lt;br /&gt;
***Monogynaspida - diverse order of parasitic and predatory mites&lt;br /&gt;
*Superorder Acariformes – contains over 300 families and over 30, 000 described species&lt;br /&gt;
**Trombidiformes – plant parasitic mites (spider mites, peacock mites, gall mites, red-legged earth mites, etc.), snout mites, chiggers, hair follicle mites, velvet mites, water mites, etc.&lt;br /&gt;
***Sphaerolichida - small order of mites containing two families&lt;br /&gt;
***Prostigmata - large order of sucking mites&lt;br /&gt;
**Sarcoptiformes&lt;br /&gt;
***Oribatida – oribatid mites, beetle mites, armored mites (also cryptostigmata)&lt;br /&gt;
***Astigmatina – stored product, fur, feather, dust, and human itch mites, etc.&lt;br /&gt;
&lt;br /&gt;
==Anatomy== &lt;br /&gt;
&lt;br /&gt;
[[File:mitie.jpg|thumb|right|Basic Mite Anatomy [7]]]&lt;br /&gt;
Mite size varies from 0.1 mm to 10 mm in length. They are most closely related to spiders than insects. They have the same characteristics of jointed legs and a chitinous exoskeleton. Acari have an open circulating system, ventral nerve cord, alimentary canal and striated muscles and may also possess Malpighian tubules. Acari lack antennae and mandibles [4]. The acarine body is divided into gnathosoma and idiosoma. The gnathosoma is the part of the body of the Acari comprising the mouth and feeding parts, and the idiosoma bears the legs, the genital and anal openings, and an assortment of tactile and sensory structures.&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
&lt;br /&gt;
*[[Microorganisms]]&lt;br /&gt;
*[[Organisms]]&lt;br /&gt;
*[[Smaller Creatures]]&lt;br /&gt;
*[[Animals]]&lt;br /&gt;
*[[Nematodes]]&lt;br /&gt;
*[[Springtail]]&lt;br /&gt;
*[[Soil organisms]]&lt;br /&gt;
*[[Tardigrades]]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
Walter, David Evans, Gerald Krantz, and Evert Lindquist. 1996. Acari. The Mites. Version 13 December 1996. http://tolweb.org/Acari/2554/1996.12.13 inThe Tree of Life Web Project, http://tolweb.org/&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
Pepato, Almir R, et al. “Phylogenetic Position of the Acariform Mites: Sensitivity to Homology Assessment under Total Evidence.” BMC Evolutionary Biology, BioMed Central, 2 Aug. 2010, bmcevolbiol.biomedcentral.com/articles/10.1186/1471-2148-10-235.&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
Sanggaard, Kristian W.; Bechsgaard, Jesper S.; Fang, Xiaodong (6 May 2014). &amp;quot;Spider genomes provide insight into composition and evolution of venom and silk&amp;quot;. Nature Communications. 5: 3765. Bibcode:2014NatCo...5E3765S. doi:10.1038/ncomms4765. PMC 4273655 Freely accessible. PMID 24801114.&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
Dhooria M.S. (2016) Morphology and Anatomy of Acari. In: Fundamentals of Applied Acarology. Springer, Singapore&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
“Acari.” Acari - Entomologists&#039; Glossary - Amateur Entomologists&#039; Society (AES), www.amentsoc.org/insects/glossary/terms/acari.&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
Wilson, Nixon A. “Acarid.” Encyclopædia Britannica, Encyclopædia Britannica, Inc., 27 Dec. 2017, www.britannica.com/animal/acarid.&lt;br /&gt;
&lt;br /&gt;
[7]&lt;br /&gt;
NCSU Veterinary Parasitology, parasitology.cvm.ncsu.edu/vmp930/keys/mites/miteterms.html.&lt;br /&gt;
&lt;br /&gt;
[8]&lt;br /&gt;
Gulvik, M. &amp;quot;Mites (Acari) as indicators of soil biodiversity and land use monitoring: a review.&amp;quot; Polish Journal of Ecology 55.3 (2007): 415.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Mites&amp;diff=2276</id>
		<title>Mites</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Mites&amp;diff=2276"/>
		<updated>2018-05-09T02:44:17Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: /* See also */&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==Definition==&lt;br /&gt;
&lt;br /&gt;
[[File:lorryia-formosa-mite.jpg|thumb|right|Lorryia formosa mite [5]]]&lt;br /&gt;
Mites are the most diverse of all arachnids, and among the oldest of all terrestrial animals. Fossils date mites from the early Devonian, nearly 400 million years ago [1.] Belonging to the class Archnida, the term &amp;quot;mite&amp;quot; refers to the several groups in the subclass Acari, but it is not a clade, and excludes the ticks. Mites and ticks are similarly characterized by their bodies being divided into two parts, named the gnathosoma and idiosoma. The three major lineages of mites are recognized as Opilioacariformes, Acariformes and Parasitiformes [1]. 45,000 species of mites have been described, which is believed to be only small 5% of the number of species estimated to be alive today. Mites can be found throughout the planet in every kind of habitat from the sea to freshwater, and in all terrestrial habitats, including soil, tree canopy, rotting woods, tree hollows, nests of vertebrates, dung and anthills [8].  In most studies, the scientists use the Berlese-Tullgren funnel to extract microarthropods from soil samples ([[Soil Sampling Methods]]). The soil sample size is often about 5 cm in diameter and 5 cm depth. Most mites in native soils occur in the top [[Soil Horizons]] [8].&lt;br /&gt;
&lt;br /&gt;
==Characteristics==&lt;br /&gt;
&lt;br /&gt;
&#039;&#039;A Manual of Acarology&#039;&#039; has defined Acari to have the following characteristics [1]:&lt;br /&gt;
&lt;br /&gt;
*Hexapod prelarva (lost in Parasitiformes and many derived Acariformes)&lt;br /&gt;
&lt;br /&gt;
*Hexapod larval stage&lt;br /&gt;
&lt;br /&gt;
*Three octopod nymphal stages (variously abbreviated in derived taxa)&lt;br /&gt;
&lt;br /&gt;
*Gnathosoma delimited by a circumcapitular suture&lt;br /&gt;
&lt;br /&gt;
*Palpcoxal endites fused medially forming a hypostome&lt;br /&gt;
&lt;br /&gt;
*Hypostome with rutella or corniculi (lost in many derived Acariformes)&lt;br /&gt;
&lt;br /&gt;
*Loss of external evidence of opisthosomal segmentation, i.e. without tergites or sternites&lt;br /&gt;
&lt;br /&gt;
*Ingestion of particulate food (lost in many derived taxa)&lt;br /&gt;
&lt;br /&gt;
==Taxonomy==&lt;br /&gt;
&lt;br /&gt;
[[File:diversity of acari.jpg|thumb|right|Diversity of Acari [6]]]&lt;br /&gt;
Acari have been variously ranked as a group made up of one to seven or more distinct orders. The orders comprise approximately half of the described arachnid [[diversity]]. Molecular information from ribosomal DNA is used to expose relationships between groups. The 18 S rRNA gene provides information on relationships among phyla and superphyla, while the ITS2, and the 18S ribosomal RNA and 28S ribosomal RNA genes, show relationships at deeper levels [2]. Recent research has suggested that Acari is polyphyletic [3]. &#039;&#039;A Manual of Acarology&#039;&#039; uses a system of six orders, grouped into three superorders to classify Acari [2]:&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
*Superorder Opilioacariformes – a small order of large mites with about 20 known species&lt;br /&gt;
*Superorder Parasitiformes – ticks and a variety of mites&lt;br /&gt;
**Holothyrida - predatory mites from the southern hemisphere&lt;br /&gt;
**Ixodida – hard ticks and soft ticks&lt;br /&gt;
**Mesostigmata – excess of 65 families and 10,000 described species, including bird mites, phytoseiid mites&lt;br /&gt;
***Trigynaspida - large, diverse order&lt;br /&gt;
***Monogynaspida - diverse order of parasitic and predatory mites&lt;br /&gt;
*Superorder Acariformes – contains over 300 families and over 30, 000 described species&lt;br /&gt;
**Trombidiformes – plant parasitic mites (spider mites, peacock mites, gall mites, red-legged earth mites, etc.), snout mites, chiggers, hair follicle mites, velvet mites, water mites, etc.&lt;br /&gt;
***Sphaerolichida - small order of mites containing two families&lt;br /&gt;
***Prostigmata - large order of sucking mites&lt;br /&gt;
**Sarcoptiformes&lt;br /&gt;
***Oribatida – oribatid mites, beetle mites, armored mites (also cryptostigmata)&lt;br /&gt;
***Astigmatina – stored product, fur, feather, dust, and human itch mites, etc.&lt;br /&gt;
&lt;br /&gt;
==Anatomy== &lt;br /&gt;
&lt;br /&gt;
[[File:mitie.jpg|thumb|right|Basic Mite Anatomy [7]]]&lt;br /&gt;
Mite size varies from 0.1 mm to 10 mm in length. They are most closely related to spiders than insects. They have the same characteristics of jointed legs and a chitinous exoskeleton. Acari have an open circulating system, ventral nerve cord, alimentary canal and striated muscles and may also possess Malpighian tubules. Acari lack antennae and mandibles [4]. The acarine body is divided into gnathosoma and idiosoma. The gnathosoma is the part of the body of the Acari comprising the mouth and feeding parts, and the idiosoma bears the legs, the genital and anal openings, and an assortment of tactile and sensory structures.&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
&lt;br /&gt;
*[[Microorganisms]]&lt;br /&gt;
*[[Organisms]]&lt;br /&gt;
*[[Smaller Creatures]]&lt;br /&gt;
*[[Animals]]&lt;br /&gt;
*[[Nematodes]]&lt;br /&gt;
*[[Springtail]]&lt;br /&gt;
*[[Soil Organisms]]&lt;br /&gt;
*[[Tardigrades]]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
Walter, David Evans, Gerald Krantz, and Evert Lindquist. 1996. Acari. The Mites. Version 13 December 1996. http://tolweb.org/Acari/2554/1996.12.13 inThe Tree of Life Web Project, http://tolweb.org/&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
Pepato, Almir R, et al. “Phylogenetic Position of the Acariform Mites: Sensitivity to Homology Assessment under Total Evidence.” BMC Evolutionary Biology, BioMed Central, 2 Aug. 2010, bmcevolbiol.biomedcentral.com/articles/10.1186/1471-2148-10-235.&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
Sanggaard, Kristian W.; Bechsgaard, Jesper S.; Fang, Xiaodong (6 May 2014). &amp;quot;Spider genomes provide insight into composition and evolution of venom and silk&amp;quot;. Nature Communications. 5: 3765. Bibcode:2014NatCo...5E3765S. doi:10.1038/ncomms4765. PMC 4273655 Freely accessible. PMID 24801114.&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
Dhooria M.S. (2016) Morphology and Anatomy of Acari. In: Fundamentals of Applied Acarology. Springer, Singapore&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
“Acari.” Acari - Entomologists&#039; Glossary - Amateur Entomologists&#039; Society (AES), www.amentsoc.org/insects/glossary/terms/acari.&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
Wilson, Nixon A. “Acarid.” Encyclopædia Britannica, Encyclopædia Britannica, Inc., 27 Dec. 2017, www.britannica.com/animal/acarid.&lt;br /&gt;
&lt;br /&gt;
[7]&lt;br /&gt;
NCSU Veterinary Parasitology, parasitology.cvm.ncsu.edu/vmp930/keys/mites/miteterms.html.&lt;br /&gt;
&lt;br /&gt;
[8]&lt;br /&gt;
Gulvik, M. &amp;quot;Mites (Acari) as indicators of soil biodiversity and land use monitoring: a review.&amp;quot; Polish Journal of Ecology 55.3 (2007): 415.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Mites&amp;diff=2275</id>
		<title>Mites</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Mites&amp;diff=2275"/>
		<updated>2018-05-09T02:43:28Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==Definition==&lt;br /&gt;
&lt;br /&gt;
[[File:lorryia-formosa-mite.jpg|thumb|right|Lorryia formosa mite [5]]]&lt;br /&gt;
Mites are the most diverse of all arachnids, and among the oldest of all terrestrial animals. Fossils date mites from the early Devonian, nearly 400 million years ago [1.] Belonging to the class Archnida, the term &amp;quot;mite&amp;quot; refers to the several groups in the subclass Acari, but it is not a clade, and excludes the ticks. Mites and ticks are similarly characterized by their bodies being divided into two parts, named the gnathosoma and idiosoma. The three major lineages of mites are recognized as Opilioacariformes, Acariformes and Parasitiformes [1]. 45,000 species of mites have been described, which is believed to be only small 5% of the number of species estimated to be alive today. Mites can be found throughout the planet in every kind of habitat from the sea to freshwater, and in all terrestrial habitats, including soil, tree canopy, rotting woods, tree hollows, nests of vertebrates, dung and anthills [8].  In most studies, the scientists use the Berlese-Tullgren funnel to extract microarthropods from soil samples ([[Soil Sampling Methods]]). The soil sample size is often about 5 cm in diameter and 5 cm depth. Most mites in native soils occur in the top [[Soil Horizons]] [8].&lt;br /&gt;
&lt;br /&gt;
==Characteristics==&lt;br /&gt;
&lt;br /&gt;
&#039;&#039;A Manual of Acarology&#039;&#039; has defined Acari to have the following characteristics [1]:&lt;br /&gt;
&lt;br /&gt;
*Hexapod prelarva (lost in Parasitiformes and many derived Acariformes)&lt;br /&gt;
&lt;br /&gt;
*Hexapod larval stage&lt;br /&gt;
&lt;br /&gt;
*Three octopod nymphal stages (variously abbreviated in derived taxa)&lt;br /&gt;
&lt;br /&gt;
*Gnathosoma delimited by a circumcapitular suture&lt;br /&gt;
&lt;br /&gt;
*Palpcoxal endites fused medially forming a hypostome&lt;br /&gt;
&lt;br /&gt;
*Hypostome with rutella or corniculi (lost in many derived Acariformes)&lt;br /&gt;
&lt;br /&gt;
*Loss of external evidence of opisthosomal segmentation, i.e. without tergites or sternites&lt;br /&gt;
&lt;br /&gt;
*Ingestion of particulate food (lost in many derived taxa)&lt;br /&gt;
&lt;br /&gt;
==Taxonomy==&lt;br /&gt;
&lt;br /&gt;
[[File:diversity of acari.jpg|thumb|right|Diversity of Acari [6]]]&lt;br /&gt;
Acari have been variously ranked as a group made up of one to seven or more distinct orders. The orders comprise approximately half of the described arachnid [[diversity]]. Molecular information from ribosomal DNA is used to expose relationships between groups. The 18 S rRNA gene provides information on relationships among phyla and superphyla, while the ITS2, and the 18S ribosomal RNA and 28S ribosomal RNA genes, show relationships at deeper levels [2]. Recent research has suggested that Acari is polyphyletic [3]. &#039;&#039;A Manual of Acarology&#039;&#039; uses a system of six orders, grouped into three superorders to classify Acari [2]:&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
*Superorder Opilioacariformes – a small order of large mites with about 20 known species&lt;br /&gt;
*Superorder Parasitiformes – ticks and a variety of mites&lt;br /&gt;
**Holothyrida - predatory mites from the southern hemisphere&lt;br /&gt;
**Ixodida – hard ticks and soft ticks&lt;br /&gt;
**Mesostigmata – excess of 65 families and 10,000 described species, including bird mites, phytoseiid mites&lt;br /&gt;
***Trigynaspida - large, diverse order&lt;br /&gt;
***Monogynaspida - diverse order of parasitic and predatory mites&lt;br /&gt;
*Superorder Acariformes – contains over 300 families and over 30, 000 described species&lt;br /&gt;
**Trombidiformes – plant parasitic mites (spider mites, peacock mites, gall mites, red-legged earth mites, etc.), snout mites, chiggers, hair follicle mites, velvet mites, water mites, etc.&lt;br /&gt;
***Sphaerolichida - small order of mites containing two families&lt;br /&gt;
***Prostigmata - large order of sucking mites&lt;br /&gt;
**Sarcoptiformes&lt;br /&gt;
***Oribatida – oribatid mites, beetle mites, armored mites (also cryptostigmata)&lt;br /&gt;
***Astigmatina – stored product, fur, feather, dust, and human itch mites, etc.&lt;br /&gt;
&lt;br /&gt;
==Anatomy== &lt;br /&gt;
&lt;br /&gt;
[[File:mitie.jpg|thumb|right|Basic Mite Anatomy [7]]]&lt;br /&gt;
Mite size varies from 0.1 mm to 10 mm in length. They are most closely related to spiders than insects. They have the same characteristics of jointed legs and a chitinous exoskeleton. Acari have an open circulating system, ventral nerve cord, alimentary canal and striated muscles and may also possess Malpighian tubules. Acari lack antennae and mandibles [4]. The acarine body is divided into gnathosoma and idiosoma. The gnathosoma is the part of the body of the Acari comprising the mouth and feeding parts, and the idiosoma bears the legs, the genital and anal openings, and an assortment of tactile and sensory structures.&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
&lt;br /&gt;
*[[Microorganisms]]&lt;br /&gt;
*[[Organisms]]&lt;br /&gt;
*[[Smaller Creatures]]&lt;br /&gt;
*[[Animals]]&lt;br /&gt;
*[[Nematodes]]&lt;br /&gt;
*[[Springtails]]&lt;br /&gt;
*[[Soil Organisms]]&lt;br /&gt;
*[[Tardigrades]]&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
Walter, David Evans, Gerald Krantz, and Evert Lindquist. 1996. Acari. The Mites. Version 13 December 1996. http://tolweb.org/Acari/2554/1996.12.13 inThe Tree of Life Web Project, http://tolweb.org/&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
Pepato, Almir R, et al. “Phylogenetic Position of the Acariform Mites: Sensitivity to Homology Assessment under Total Evidence.” BMC Evolutionary Biology, BioMed Central, 2 Aug. 2010, bmcevolbiol.biomedcentral.com/articles/10.1186/1471-2148-10-235.&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
Sanggaard, Kristian W.; Bechsgaard, Jesper S.; Fang, Xiaodong (6 May 2014). &amp;quot;Spider genomes provide insight into composition and evolution of venom and silk&amp;quot;. Nature Communications. 5: 3765. Bibcode:2014NatCo...5E3765S. doi:10.1038/ncomms4765. PMC 4273655 Freely accessible. PMID 24801114.&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
Dhooria M.S. (2016) Morphology and Anatomy of Acari. In: Fundamentals of Applied Acarology. Springer, Singapore&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
“Acari.” Acari - Entomologists&#039; Glossary - Amateur Entomologists&#039; Society (AES), www.amentsoc.org/insects/glossary/terms/acari.&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
Wilson, Nixon A. “Acarid.” Encyclopædia Britannica, Encyclopædia Britannica, Inc., 27 Dec. 2017, www.britannica.com/animal/acarid.&lt;br /&gt;
&lt;br /&gt;
[7]&lt;br /&gt;
NCSU Veterinary Parasitology, parasitology.cvm.ncsu.edu/vmp930/keys/mites/miteterms.html.&lt;br /&gt;
&lt;br /&gt;
[8]&lt;br /&gt;
Gulvik, M. &amp;quot;Mites (Acari) as indicators of soil biodiversity and land use monitoring: a review.&amp;quot; Polish Journal of Ecology 55.3 (2007): 415.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Mites&amp;diff=2127</id>
		<title>Mites</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Mites&amp;diff=2127"/>
		<updated>2018-05-08T04:01:11Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: /* Taxonomy */&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==Definition==&lt;br /&gt;
&lt;br /&gt;
[[File:lorryia-formosa-mite.jpg|thumb|right|Lorryia formosa mite [5]]]&lt;br /&gt;
Mites are the most diverse of all arachnids, and among the oldest of all terrestrial animals. Fossils date mites from the early Devonian, nearly 400 million years ago [1.] Belonging to the class Archnida, the term &amp;quot;mite&amp;quot; refers to the several groups in the subclass Acari, but it is not a clade, and excludes the ticks. Mites and ticks are similarly characterized by their bodies being divided into two parts, named the gnathosoma and idiosoma. The three major lineages of mites are recognized as Opilioacariformes, Acariformes and Parasitiformes [1]. 45,000 species of mites have been described, which is believed to be only small 5% of the number of species estimated to be alive today. Mites can be found throughout the planet in every kind of habitat from the sea to freshwater, and in all terrestrial habitats, including soil, tree canopy, rotting woods, tree hollows, nests of vertebrates, dung and anthills [8].  In most studies, the scientists use the Berlese-Tullgren funnel to extract microarthropods from soil samples ([[Soil Sampling Methods]]). The soil sample size is often about 5 cm in diameter and 5 cm depth. Most mites in native soils occur in the top [[Soil Horizons]] [8].&lt;br /&gt;
&lt;br /&gt;
==Characteristics==&lt;br /&gt;
&lt;br /&gt;
&#039;&#039;A Manual of Acarology&#039;&#039; has defined Acari to have the following characteristics [1]:&lt;br /&gt;
&lt;br /&gt;
*Hexapod prelarva (lost in Parasitiformes and many derived Acariformes)&lt;br /&gt;
&lt;br /&gt;
*Hexapod larval stage&lt;br /&gt;
&lt;br /&gt;
*Three octopod nymphal stages (variously abbreviated in derived taxa)&lt;br /&gt;
&lt;br /&gt;
*Gnathosoma delimited by a circumcapitular suture&lt;br /&gt;
&lt;br /&gt;
*Palpcoxal endites fused medially forming a hypostome&lt;br /&gt;
&lt;br /&gt;
*Hypostome with rutella or corniculi (lost in many derived Acariformes)&lt;br /&gt;
&lt;br /&gt;
*Loss of external evidence of opisthosomal segmentation, i.e. without tergites or sternites&lt;br /&gt;
&lt;br /&gt;
*Ingestion of particulate food (lost in many derived taxa)&lt;br /&gt;
&lt;br /&gt;
==Taxonomy==&lt;br /&gt;
&lt;br /&gt;
[[File:diversity of acari.jpg|thumb|right|Diversity of Acari [6]]]&lt;br /&gt;
Acari have been variously ranked as a group made up of one to seven or more distinct orders. The orders comprise approximately half of the described arachnid [[diversity]]. Molecular information from ribosomal DNA is used to expose relationships between groups. The 18 S rRNA gene provides information on relationships among phyla and superphyla, while the ITS2, and the 18S ribosomal RNA and 28S ribosomal RNA genes, show relationships at deeper levels [2]. Recent research has suggested that Acari is polyphyletic [3]. &#039;&#039;A Manual of Acarology&#039;&#039; uses a system of six orders, grouped into three superorders to classify Acari [2]:&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
*Superorder Opilioacariformes – a small order of large mites with about 20 known species&lt;br /&gt;
*Superorder Parasitiformes – ticks and a variety of mites&lt;br /&gt;
**Holothyrida - predatory mites from the southern hemisphere&lt;br /&gt;
**Ixodida – hard ticks and soft ticks&lt;br /&gt;
**Mesostigmata – excess of 65 families and 10,000 described species, including bird mites, phytoseiid mites&lt;br /&gt;
***Trigynaspida - large, diverse order&lt;br /&gt;
***Monogynaspida - diverse order of parasitic and predatory mites&lt;br /&gt;
*Superorder Acariformes – contains over 300 families and over 30, 000 described species&lt;br /&gt;
**Trombidiformes – plant parasitic mites (spider mites, peacock mites, gall mites, red-legged earth mites, etc.), snout mites, chiggers, hair follicle mites, velvet mites, water mites, etc.&lt;br /&gt;
***Sphaerolichida - small order of mites containing two families&lt;br /&gt;
***Prostigmata - large order of sucking mites&lt;br /&gt;
**Sarcoptiformes&lt;br /&gt;
***Oribatida – oribatid mites, beetle mites, armored mites (also cryptostigmata)&lt;br /&gt;
***Astigmatina – stored product, fur, feather, dust, and human itch mites, etc.&lt;br /&gt;
&lt;br /&gt;
==Anatomy== &lt;br /&gt;
&lt;br /&gt;
[[File:mitie.jpg|thumb|right|Basic Mite Anatomy [7]]]&lt;br /&gt;
Mite size varies from 0.1 mm to 10 mm in length. They are most closely related to spiders than insects. They have the same characteristics of jointed legs and a chitinous exoskeleton. Acari have an open circulating system, ventral nerve cord, alimentary canal and striated muscles and may also possess Malpighian tubules. Acari lack antennae and mandibles [4]. The acarine body is divided into gnathosoma and idiosoma. The gnathosoma is the part of the body of the Acari comprising the mouth and feeding parts, and the idiosoma bears the legs, the genital and anal openings, and an assortment of tactile and sensory structures.&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
Walter, David Evans, Gerald Krantz, and Evert Lindquist. 1996. Acari. The Mites. Version 13 December 1996. http://tolweb.org/Acari/2554/1996.12.13 inThe Tree of Life Web Project, http://tolweb.org/&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
Pepato, Almir R, et al. “Phylogenetic Position of the Acariform Mites: Sensitivity to Homology Assessment under Total Evidence.” BMC Evolutionary Biology, BioMed Central, 2 Aug. 2010, bmcevolbiol.biomedcentral.com/articles/10.1186/1471-2148-10-235.&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
Sanggaard, Kristian W.; Bechsgaard, Jesper S.; Fang, Xiaodong (6 May 2014). &amp;quot;Spider genomes provide insight into composition and evolution of venom and silk&amp;quot;. Nature Communications. 5: 3765. Bibcode:2014NatCo...5E3765S. doi:10.1038/ncomms4765. PMC 4273655 Freely accessible. PMID 24801114.&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
Dhooria M.S. (2016) Morphology and Anatomy of Acari. In: Fundamentals of Applied Acarology. Springer, Singapore&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
“Acari.” Acari - Entomologists&#039; Glossary - Amateur Entomologists&#039; Society (AES), www.amentsoc.org/insects/glossary/terms/acari.&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
Wilson, Nixon A. “Acarid.” Encyclopædia Britannica, Encyclopædia Britannica, Inc., 27 Dec. 2017, www.britannica.com/animal/acarid.&lt;br /&gt;
&lt;br /&gt;
[7]&lt;br /&gt;
NCSU Veterinary Parasitology, parasitology.cvm.ncsu.edu/vmp930/keys/mites/miteterms.html.&lt;br /&gt;
&lt;br /&gt;
[8]&lt;br /&gt;
Gulvik, M. &amp;quot;Mites (Acari) as indicators of soil biodiversity and land use monitoring: a review.&amp;quot; Polish Journal of Ecology 55.3 (2007): 415.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Mites&amp;diff=2126</id>
		<title>Mites</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Mites&amp;diff=2126"/>
		<updated>2018-05-08T03:56:50Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: /* Definition */&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==Definition==&lt;br /&gt;
&lt;br /&gt;
[[File:lorryia-formosa-mite.jpg|thumb|right|Lorryia formosa mite [5]]]&lt;br /&gt;
Mites are the most diverse of all arachnids, and among the oldest of all terrestrial animals. Fossils date mites from the early Devonian, nearly 400 million years ago [1.] Belonging to the class Archnida, the term &amp;quot;mite&amp;quot; refers to the several groups in the subclass Acari, but it is not a clade, and excludes the ticks. Mites and ticks are similarly characterized by their bodies being divided into two parts, named the gnathosoma and idiosoma. The three major lineages of mites are recognized as Opilioacariformes, Acariformes and Parasitiformes [1]. 45,000 species of mites have been described, which is believed to be only small 5% of the number of species estimated to be alive today. Mites can be found throughout the planet in every kind of habitat from the sea to freshwater, and in all terrestrial habitats, including soil, tree canopy, rotting woods, tree hollows, nests of vertebrates, dung and anthills [8].  In most studies, the scientists use the Berlese-Tullgren funnel to extract microarthropods from soil samples ([[Soil Sampling Methods]]). The soil sample size is often about 5 cm in diameter and 5 cm depth. Most mites in native soils occur in the top [[Soil Horizons]] [8].&lt;br /&gt;
&lt;br /&gt;
==Characteristics==&lt;br /&gt;
&lt;br /&gt;
&#039;&#039;A Manual of Acarology&#039;&#039; has defined Acari to have the following characteristics [1]:&lt;br /&gt;
&lt;br /&gt;
*Hexapod prelarva (lost in Parasitiformes and many derived Acariformes)&lt;br /&gt;
&lt;br /&gt;
*Hexapod larval stage&lt;br /&gt;
&lt;br /&gt;
*Three octopod nymphal stages (variously abbreviated in derived taxa)&lt;br /&gt;
&lt;br /&gt;
*Gnathosoma delimited by a circumcapitular suture&lt;br /&gt;
&lt;br /&gt;
*Palpcoxal endites fused medially forming a hypostome&lt;br /&gt;
&lt;br /&gt;
*Hypostome with rutella or corniculi (lost in many derived Acariformes)&lt;br /&gt;
&lt;br /&gt;
*Loss of external evidence of opisthosomal segmentation, i.e. without tergites or sternites&lt;br /&gt;
&lt;br /&gt;
*Ingestion of particulate food (lost in many derived taxa)&lt;br /&gt;
&lt;br /&gt;
==Taxonomy==&lt;br /&gt;
&lt;br /&gt;
[[File:diversity of acari.jpg|thumb|right|Diversity of Acari [6]]]&lt;br /&gt;
Acari have been variously ranked as a group made up of one to seven or more distinct orders. The orders comprise approximately half of the described arachnid diversity. Molecular information from ribosomal DNA is used to expose relationships between groups. The 18 S rRNA gene provides information on relationships among phyla and superphyla, while the ITS2, and the 18S ribosomal RNA and 28S ribosomal RNA genes, show relationships at deeper levels [2]. Recent research has suggested that Acari is polyphyletic [3]. &#039;&#039;A Manual of Acarology&#039;&#039; uses a system of six orders, grouped into three superorders to classify Acari [2]:&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
*Superorder Opilioacariformes – a small order of large mites with about 20 known species&lt;br /&gt;
*Superorder Parasitiformes – ticks and a variety of mites&lt;br /&gt;
**Holothyrida - predatory mites from the southern hemisphere&lt;br /&gt;
**Ixodida – hard ticks and soft ticks&lt;br /&gt;
**Mesostigmata – excess of 65 families and 10,000 described species, including bird mites, phytoseiid mites&lt;br /&gt;
***Trigynaspida - large, diverse order&lt;br /&gt;
***Monogynaspida - diverse order of parasitic and predatory mites&lt;br /&gt;
*Superorder Acariformes – contains over 300 families and over 30, 000 described species&lt;br /&gt;
**Trombidiformes – plant parasitic mites (spider mites, peacock mites, gall mites, red-legged earth mites, etc.), snout mites, chiggers, hair follicle mites, velvet mites, water mites, etc.&lt;br /&gt;
***Sphaerolichida - small order of mites containing two families&lt;br /&gt;
***Prostigmata - large order of sucking mites&lt;br /&gt;
**Sarcoptiformes&lt;br /&gt;
***Oribatida – oribatid mites, beetle mites, armored mites (also cryptostigmata)&lt;br /&gt;
***Astigmatina – stored product, fur, feather, dust, and human itch mites, etc.&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
==Anatomy== &lt;br /&gt;
&lt;br /&gt;
[[File:mitie.jpg|thumb|right|Basic Mite Anatomy [7]]]&lt;br /&gt;
Mite size varies from 0.1 mm to 10 mm in length. They are most closely related to spiders than insects. They have the same characteristics of jointed legs and a chitinous exoskeleton. Acari have an open circulating system, ventral nerve cord, alimentary canal and striated muscles and may also possess Malpighian tubules. Acari lack antennae and mandibles [4]. The acarine body is divided into gnathosoma and idiosoma. The gnathosoma is the part of the body of the Acari comprising the mouth and feeding parts, and the idiosoma bears the legs, the genital and anal openings, and an assortment of tactile and sensory structures.&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
Walter, David Evans, Gerald Krantz, and Evert Lindquist. 1996. Acari. The Mites. Version 13 December 1996. http://tolweb.org/Acari/2554/1996.12.13 inThe Tree of Life Web Project, http://tolweb.org/&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
Pepato, Almir R, et al. “Phylogenetic Position of the Acariform Mites: Sensitivity to Homology Assessment under Total Evidence.” BMC Evolutionary Biology, BioMed Central, 2 Aug. 2010, bmcevolbiol.biomedcentral.com/articles/10.1186/1471-2148-10-235.&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
Sanggaard, Kristian W.; Bechsgaard, Jesper S.; Fang, Xiaodong (6 May 2014). &amp;quot;Spider genomes provide insight into composition and evolution of venom and silk&amp;quot;. Nature Communications. 5: 3765. Bibcode:2014NatCo...5E3765S. doi:10.1038/ncomms4765. PMC 4273655 Freely accessible. PMID 24801114.&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
Dhooria M.S. (2016) Morphology and Anatomy of Acari. In: Fundamentals of Applied Acarology. Springer, Singapore&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
“Acari.” Acari - Entomologists&#039; Glossary - Amateur Entomologists&#039; Society (AES), www.amentsoc.org/insects/glossary/terms/acari.&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
Wilson, Nixon A. “Acarid.” Encyclopædia Britannica, Encyclopædia Britannica, Inc., 27 Dec. 2017, www.britannica.com/animal/acarid.&lt;br /&gt;
&lt;br /&gt;
[7]&lt;br /&gt;
NCSU Veterinary Parasitology, parasitology.cvm.ncsu.edu/vmp930/keys/mites/miteterms.html.&lt;br /&gt;
&lt;br /&gt;
[8]&lt;br /&gt;
Gulvik, M. &amp;quot;Mites (Acari) as indicators of soil biodiversity and land use monitoring: a review.&amp;quot; Polish Journal of Ecology 55.3 (2007): 415.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Mites&amp;diff=2125</id>
		<title>Mites</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Mites&amp;diff=2125"/>
		<updated>2018-05-08T03:56:35Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: /* Definition */&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==Definition==&lt;br /&gt;
&lt;br /&gt;
[[File:lorryia-formosa-mite.jpg|thumb|right|Lorryia formosa mite [5]]]&lt;br /&gt;
Mites are the most diverse of all arachnids, and among the oldest of all terrestrial animals. Fossils date mites from the early Devonian, nearly 400 million years ago [1.] Belonging to the class Archnida, the term &amp;quot;mite&amp;quot; refers to the several groups in the subclass Acari, but it is not a clade, and excludes the ticks. Mites and ticks are similarly characterized by their bodies being divided into two parts, named the gnathosoma and idiosoma. The three major lineages of mites are recognized as Opilioacariformes, Acariformes and Parasitiformes [1]. 45,000 species of mites have been described, which is believed to be only small 5% of the number of species estimated to be alive today. Mites can be found throughout the planet in every kind of habitat from the sea to freshwater, and in all terrestrial habitats, including soil, tree canopy, rotting woods, tree hollows, nests of vertebrates, dung and anthills [8].  In most studies, the scientists use the Berlese-Tullgren funnel to extract microarthropods from soil samples ([[Soil Sampling Mehtods]]). The soil sample size is often about 5 cm in diameter and 5 cm depth. Most mites in native soils occur in the top [[Soil Horizons]] [8].&lt;br /&gt;
&lt;br /&gt;
==Characteristics==&lt;br /&gt;
&lt;br /&gt;
&#039;&#039;A Manual of Acarology&#039;&#039; has defined Acari to have the following characteristics [1]:&lt;br /&gt;
&lt;br /&gt;
*Hexapod prelarva (lost in Parasitiformes and many derived Acariformes)&lt;br /&gt;
&lt;br /&gt;
*Hexapod larval stage&lt;br /&gt;
&lt;br /&gt;
*Three octopod nymphal stages (variously abbreviated in derived taxa)&lt;br /&gt;
&lt;br /&gt;
*Gnathosoma delimited by a circumcapitular suture&lt;br /&gt;
&lt;br /&gt;
*Palpcoxal endites fused medially forming a hypostome&lt;br /&gt;
&lt;br /&gt;
*Hypostome with rutella or corniculi (lost in many derived Acariformes)&lt;br /&gt;
&lt;br /&gt;
*Loss of external evidence of opisthosomal segmentation, i.e. without tergites or sternites&lt;br /&gt;
&lt;br /&gt;
*Ingestion of particulate food (lost in many derived taxa)&lt;br /&gt;
&lt;br /&gt;
==Taxonomy==&lt;br /&gt;
&lt;br /&gt;
[[File:diversity of acari.jpg|thumb|right|Diversity of Acari [6]]]&lt;br /&gt;
Acari have been variously ranked as a group made up of one to seven or more distinct orders. The orders comprise approximately half of the described arachnid diversity. Molecular information from ribosomal DNA is used to expose relationships between groups. The 18 S rRNA gene provides information on relationships among phyla and superphyla, while the ITS2, and the 18S ribosomal RNA and 28S ribosomal RNA genes, show relationships at deeper levels [2]. Recent research has suggested that Acari is polyphyletic [3]. &#039;&#039;A Manual of Acarology&#039;&#039; uses a system of six orders, grouped into three superorders to classify Acari [2]:&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
*Superorder Opilioacariformes – a small order of large mites with about 20 known species&lt;br /&gt;
*Superorder Parasitiformes – ticks and a variety of mites&lt;br /&gt;
**Holothyrida - predatory mites from the southern hemisphere&lt;br /&gt;
**Ixodida – hard ticks and soft ticks&lt;br /&gt;
**Mesostigmata – excess of 65 families and 10,000 described species, including bird mites, phytoseiid mites&lt;br /&gt;
***Trigynaspida - large, diverse order&lt;br /&gt;
***Monogynaspida - diverse order of parasitic and predatory mites&lt;br /&gt;
*Superorder Acariformes – contains over 300 families and over 30, 000 described species&lt;br /&gt;
**Trombidiformes – plant parasitic mites (spider mites, peacock mites, gall mites, red-legged earth mites, etc.), snout mites, chiggers, hair follicle mites, velvet mites, water mites, etc.&lt;br /&gt;
***Sphaerolichida - small order of mites containing two families&lt;br /&gt;
***Prostigmata - large order of sucking mites&lt;br /&gt;
**Sarcoptiformes&lt;br /&gt;
***Oribatida – oribatid mites, beetle mites, armored mites (also cryptostigmata)&lt;br /&gt;
***Astigmatina – stored product, fur, feather, dust, and human itch mites, etc.&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
==Anatomy== &lt;br /&gt;
&lt;br /&gt;
[[File:mitie.jpg|thumb|right|Basic Mite Anatomy [7]]]&lt;br /&gt;
Mite size varies from 0.1 mm to 10 mm in length. They are most closely related to spiders than insects. They have the same characteristics of jointed legs and a chitinous exoskeleton. Acari have an open circulating system, ventral nerve cord, alimentary canal and striated muscles and may also possess Malpighian tubules. Acari lack antennae and mandibles [4]. The acarine body is divided into gnathosoma and idiosoma. The gnathosoma is the part of the body of the Acari comprising the mouth and feeding parts, and the idiosoma bears the legs, the genital and anal openings, and an assortment of tactile and sensory structures.&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
Walter, David Evans, Gerald Krantz, and Evert Lindquist. 1996. Acari. The Mites. Version 13 December 1996. http://tolweb.org/Acari/2554/1996.12.13 inThe Tree of Life Web Project, http://tolweb.org/&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
Pepato, Almir R, et al. “Phylogenetic Position of the Acariform Mites: Sensitivity to Homology Assessment under Total Evidence.” BMC Evolutionary Biology, BioMed Central, 2 Aug. 2010, bmcevolbiol.biomedcentral.com/articles/10.1186/1471-2148-10-235.&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
Sanggaard, Kristian W.; Bechsgaard, Jesper S.; Fang, Xiaodong (6 May 2014). &amp;quot;Spider genomes provide insight into composition and evolution of venom and silk&amp;quot;. Nature Communications. 5: 3765. Bibcode:2014NatCo...5E3765S. doi:10.1038/ncomms4765. PMC 4273655 Freely accessible. PMID 24801114.&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
Dhooria M.S. (2016) Morphology and Anatomy of Acari. In: Fundamentals of Applied Acarology. Springer, Singapore&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
“Acari.” Acari - Entomologists&#039; Glossary - Amateur Entomologists&#039; Society (AES), www.amentsoc.org/insects/glossary/terms/acari.&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
Wilson, Nixon A. “Acarid.” Encyclopædia Britannica, Encyclopædia Britannica, Inc., 27 Dec. 2017, www.britannica.com/animal/acarid.&lt;br /&gt;
&lt;br /&gt;
[7]&lt;br /&gt;
NCSU Veterinary Parasitology, parasitology.cvm.ncsu.edu/vmp930/keys/mites/miteterms.html.&lt;br /&gt;
&lt;br /&gt;
[8]&lt;br /&gt;
Gulvik, M. &amp;quot;Mites (Acari) as indicators of soil biodiversity and land use monitoring: a review.&amp;quot; Polish Journal of Ecology 55.3 (2007): 415.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Mites&amp;diff=2124</id>
		<title>Mites</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Mites&amp;diff=2124"/>
		<updated>2018-05-08T03:52:33Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: /* References */&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==Definition==&lt;br /&gt;
&lt;br /&gt;
[[File:lorryia-formosa-mite.jpg|thumb|right|Lorryia formosa mite [5]]]&lt;br /&gt;
Mites are the most diverse of all arachnids, and among the oldest of all terrestrial animals. Fossils date mites from the early Devonian, nearly 400 million years ago [1.] Belonging to the class Archnida, the term &amp;quot;mite&amp;quot; refers to the several groups in the subclass Acari, but it is not a clade, and excludes the ticks. Mites and ticks are similarly characterized by their bodies being divided into two parts, named the gnathosoma and idiosoma. The three major lineages of mites are recognized as Opilioacariformes, Acariformes and Parasitiformes [1]. 45,000 species of mites have been described, which is believed to be only small 5% of the number of species estimated to be alive today. Mites can be found throughout the planet in every kind of habitat from the sea to freshwater, and in all terrestrial habitats, including soil, tree canopy, rotting woods, tree hollows, nests of vertebrates, dung and anthills [8].&lt;br /&gt;
&lt;br /&gt;
==Characteristics==&lt;br /&gt;
&lt;br /&gt;
&#039;&#039;A Manual of Acarology&#039;&#039; has defined Acari to have the following characteristics [1]:&lt;br /&gt;
&lt;br /&gt;
*Hexapod prelarva (lost in Parasitiformes and many derived Acariformes)&lt;br /&gt;
&lt;br /&gt;
*Hexapod larval stage&lt;br /&gt;
&lt;br /&gt;
*Three octopod nymphal stages (variously abbreviated in derived taxa)&lt;br /&gt;
&lt;br /&gt;
*Gnathosoma delimited by a circumcapitular suture&lt;br /&gt;
&lt;br /&gt;
*Palpcoxal endites fused medially forming a hypostome&lt;br /&gt;
&lt;br /&gt;
*Hypostome with rutella or corniculi (lost in many derived Acariformes)&lt;br /&gt;
&lt;br /&gt;
*Loss of external evidence of opisthosomal segmentation, i.e. without tergites or sternites&lt;br /&gt;
&lt;br /&gt;
*Ingestion of particulate food (lost in many derived taxa)&lt;br /&gt;
&lt;br /&gt;
==Taxonomy==&lt;br /&gt;
&lt;br /&gt;
[[File:diversity of acari.jpg|thumb|right|Diversity of Acari [6]]]&lt;br /&gt;
Acari have been variously ranked as a group made up of one to seven or more distinct orders. The orders comprise approximately half of the described arachnid diversity. Molecular information from ribosomal DNA is used to expose relationships between groups. The 18 S rRNA gene provides information on relationships among phyla and superphyla, while the ITS2, and the 18S ribosomal RNA and 28S ribosomal RNA genes, show relationships at deeper levels [2]. Recent research has suggested that Acari is polyphyletic [3]. &#039;&#039;A Manual of Acarology&#039;&#039; uses a system of six orders, grouped into three superorders to classify Acari [2]:&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
*Superorder Opilioacariformes – a small order of large mites with about 20 known species&lt;br /&gt;
*Superorder Parasitiformes – ticks and a variety of mites&lt;br /&gt;
**Holothyrida - predatory mites from the southern hemisphere&lt;br /&gt;
**Ixodida – hard ticks and soft ticks&lt;br /&gt;
**Mesostigmata – excess of 65 families and 10,000 described species, including bird mites, phytoseiid mites&lt;br /&gt;
***Trigynaspida - large, diverse order&lt;br /&gt;
***Monogynaspida - diverse order of parasitic and predatory mites&lt;br /&gt;
*Superorder Acariformes – contains over 300 families and over 30, 000 described species&lt;br /&gt;
**Trombidiformes – plant parasitic mites (spider mites, peacock mites, gall mites, red-legged earth mites, etc.), snout mites, chiggers, hair follicle mites, velvet mites, water mites, etc.&lt;br /&gt;
***Sphaerolichida - small order of mites containing two families&lt;br /&gt;
***Prostigmata - large order of sucking mites&lt;br /&gt;
**Sarcoptiformes&lt;br /&gt;
***Oribatida – oribatid mites, beetle mites, armored mites (also cryptostigmata)&lt;br /&gt;
***Astigmatina – stored product, fur, feather, dust, and human itch mites, etc.&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
==Anatomy== &lt;br /&gt;
&lt;br /&gt;
[[File:mitie.jpg|thumb|right|Basic Mite Anatomy [7]]]&lt;br /&gt;
Mite size varies from 0.1 mm to 10 mm in length. They are most closely related to spiders than insects. They have the same characteristics of jointed legs and a chitinous exoskeleton. Acari have an open circulating system, ventral nerve cord, alimentary canal and striated muscles and may also possess Malpighian tubules. Acari lack antennae and mandibles [4]. The acarine body is divided into gnathosoma and idiosoma. The gnathosoma is the part of the body of the Acari comprising the mouth and feeding parts, and the idiosoma bears the legs, the genital and anal openings, and an assortment of tactile and sensory structures.&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
Walter, David Evans, Gerald Krantz, and Evert Lindquist. 1996. Acari. The Mites. Version 13 December 1996. http://tolweb.org/Acari/2554/1996.12.13 inThe Tree of Life Web Project, http://tolweb.org/&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
Pepato, Almir R, et al. “Phylogenetic Position of the Acariform Mites: Sensitivity to Homology Assessment under Total Evidence.” BMC Evolutionary Biology, BioMed Central, 2 Aug. 2010, bmcevolbiol.biomedcentral.com/articles/10.1186/1471-2148-10-235.&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
Sanggaard, Kristian W.; Bechsgaard, Jesper S.; Fang, Xiaodong (6 May 2014). &amp;quot;Spider genomes provide insight into composition and evolution of venom and silk&amp;quot;. Nature Communications. 5: 3765. Bibcode:2014NatCo...5E3765S. doi:10.1038/ncomms4765. PMC 4273655 Freely accessible. PMID 24801114.&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
Dhooria M.S. (2016) Morphology and Anatomy of Acari. In: Fundamentals of Applied Acarology. Springer, Singapore&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
“Acari.” Acari - Entomologists&#039; Glossary - Amateur Entomologists&#039; Society (AES), www.amentsoc.org/insects/glossary/terms/acari.&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
Wilson, Nixon A. “Acarid.” Encyclopædia Britannica, Encyclopædia Britannica, Inc., 27 Dec. 2017, www.britannica.com/animal/acarid.&lt;br /&gt;
&lt;br /&gt;
[7]&lt;br /&gt;
NCSU Veterinary Parasitology, parasitology.cvm.ncsu.edu/vmp930/keys/mites/miteterms.html.&lt;br /&gt;
&lt;br /&gt;
[8]&lt;br /&gt;
Gulvik, M. &amp;quot;Mites (Acari) as indicators of soil biodiversity and land use monitoring: a review.&amp;quot; Polish Journal of Ecology 55.3 (2007): 415.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Mites&amp;diff=2123</id>
		<title>Mites</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Mites&amp;diff=2123"/>
		<updated>2018-05-08T03:52:00Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: /* Definition */&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==Definition==&lt;br /&gt;
&lt;br /&gt;
[[File:lorryia-formosa-mite.jpg|thumb|right|Lorryia formosa mite [5]]]&lt;br /&gt;
Mites are the most diverse of all arachnids, and among the oldest of all terrestrial animals. Fossils date mites from the early Devonian, nearly 400 million years ago [1.] Belonging to the class Archnida, the term &amp;quot;mite&amp;quot; refers to the several groups in the subclass Acari, but it is not a clade, and excludes the ticks. Mites and ticks are similarly characterized by their bodies being divided into two parts, named the gnathosoma and idiosoma. The three major lineages of mites are recognized as Opilioacariformes, Acariformes and Parasitiformes [1]. 45,000 species of mites have been described, which is believed to be only small 5% of the number of species estimated to be alive today. Mites can be found throughout the planet in every kind of habitat from the sea to freshwater, and in all terrestrial habitats, including soil, tree canopy, rotting woods, tree hollows, nests of vertebrates, dung and anthills [8].&lt;br /&gt;
&lt;br /&gt;
==Characteristics==&lt;br /&gt;
&lt;br /&gt;
&#039;&#039;A Manual of Acarology&#039;&#039; has defined Acari to have the following characteristics [1]:&lt;br /&gt;
&lt;br /&gt;
*Hexapod prelarva (lost in Parasitiformes and many derived Acariformes)&lt;br /&gt;
&lt;br /&gt;
*Hexapod larval stage&lt;br /&gt;
&lt;br /&gt;
*Three octopod nymphal stages (variously abbreviated in derived taxa)&lt;br /&gt;
&lt;br /&gt;
*Gnathosoma delimited by a circumcapitular suture&lt;br /&gt;
&lt;br /&gt;
*Palpcoxal endites fused medially forming a hypostome&lt;br /&gt;
&lt;br /&gt;
*Hypostome with rutella or corniculi (lost in many derived Acariformes)&lt;br /&gt;
&lt;br /&gt;
*Loss of external evidence of opisthosomal segmentation, i.e. without tergites or sternites&lt;br /&gt;
&lt;br /&gt;
*Ingestion of particulate food (lost in many derived taxa)&lt;br /&gt;
&lt;br /&gt;
==Taxonomy==&lt;br /&gt;
&lt;br /&gt;
[[File:diversity of acari.jpg|thumb|right|Diversity of Acari [6]]]&lt;br /&gt;
Acari have been variously ranked as a group made up of one to seven or more distinct orders. The orders comprise approximately half of the described arachnid diversity. Molecular information from ribosomal DNA is used to expose relationships between groups. The 18 S rRNA gene provides information on relationships among phyla and superphyla, while the ITS2, and the 18S ribosomal RNA and 28S ribosomal RNA genes, show relationships at deeper levels [2]. Recent research has suggested that Acari is polyphyletic [3]. &#039;&#039;A Manual of Acarology&#039;&#039; uses a system of six orders, grouped into three superorders to classify Acari [2]:&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
*Superorder Opilioacariformes – a small order of large mites with about 20 known species&lt;br /&gt;
*Superorder Parasitiformes – ticks and a variety of mites&lt;br /&gt;
**Holothyrida - predatory mites from the southern hemisphere&lt;br /&gt;
**Ixodida – hard ticks and soft ticks&lt;br /&gt;
**Mesostigmata – excess of 65 families and 10,000 described species, including bird mites, phytoseiid mites&lt;br /&gt;
***Trigynaspida - large, diverse order&lt;br /&gt;
***Monogynaspida - diverse order of parasitic and predatory mites&lt;br /&gt;
*Superorder Acariformes – contains over 300 families and over 30, 000 described species&lt;br /&gt;
**Trombidiformes – plant parasitic mites (spider mites, peacock mites, gall mites, red-legged earth mites, etc.), snout mites, chiggers, hair follicle mites, velvet mites, water mites, etc.&lt;br /&gt;
***Sphaerolichida - small order of mites containing two families&lt;br /&gt;
***Prostigmata - large order of sucking mites&lt;br /&gt;
**Sarcoptiformes&lt;br /&gt;
***Oribatida – oribatid mites, beetle mites, armored mites (also cryptostigmata)&lt;br /&gt;
***Astigmatina – stored product, fur, feather, dust, and human itch mites, etc.&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
==Anatomy== &lt;br /&gt;
&lt;br /&gt;
[[File:mitie.jpg|thumb|right|Basic Mite Anatomy [7]]]&lt;br /&gt;
Mite size varies from 0.1 mm to 10 mm in length. They are most closely related to spiders than insects. They have the same characteristics of jointed legs and a chitinous exoskeleton. Acari have an open circulating system, ventral nerve cord, alimentary canal and striated muscles and may also possess Malpighian tubules. Acari lack antennae and mandibles [4]. The acarine body is divided into gnathosoma and idiosoma. The gnathosoma is the part of the body of the Acari comprising the mouth and feeding parts, and the idiosoma bears the legs, the genital and anal openings, and an assortment of tactile and sensory structures.&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
Walter, David Evans, Gerald Krantz, and Evert Lindquist. 1996. Acari. The Mites. Version 13 December 1996. http://tolweb.org/Acari/2554/1996.12.13 inThe Tree of Life Web Project, http://tolweb.org/&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
Pepato, Almir R, et al. “Phylogenetic Position of the Acariform Mites: Sensitivity to Homology Assessment under Total Evidence.” BMC Evolutionary Biology, BioMed Central, 2 Aug. 2010, bmcevolbiol.biomedcentral.com/articles/10.1186/1471-2148-10-235.&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
Sanggaard, Kristian W.; Bechsgaard, Jesper S.; Fang, Xiaodong (6 May 2014). &amp;quot;Spider genomes provide insight into composition and evolution of venom and silk&amp;quot;. Nature Communications. 5: 3765. Bibcode:2014NatCo...5E3765S. doi:10.1038/ncomms4765. PMC 4273655 Freely accessible. PMID 24801114.&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
Dhooria M.S. (2016) Morphology and Anatomy of Acari. In: Fundamentals of Applied Acarology. Springer, Singapore&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
“Acari.” Acari - Entomologists&#039; Glossary - Amateur Entomologists&#039; Society (AES), www.amentsoc.org/insects/glossary/terms/acari.&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
Wilson, Nixon A. “Acarid.” Encyclopædia Britannica, Encyclopædia Britannica, Inc., 27 Dec. 2017, www.britannica.com/animal/acarid.&lt;br /&gt;
&lt;br /&gt;
[7]&lt;br /&gt;
NCSU Veterinary Parasitology, parasitology.cvm.ncsu.edu/vmp930/keys/mites/miteterms.html.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Mites&amp;diff=1626</id>
		<title>Mites</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Mites&amp;diff=1626"/>
		<updated>2018-04-20T06:10:22Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: /* Characteristics */&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==Definition==&lt;br /&gt;
&lt;br /&gt;
[[File:lorryia-formosa-mite.jpg|thumb|right|Lorryia formosa mite [5]]]&lt;br /&gt;
Mites are the most diverse of all arachnids, and among the oldest of all terrestrial animals. Fossils date mites from the early Devonian, nearly 400 million years ago [1.] Belonging to the class Archnida, the term &amp;quot;mite&amp;quot; refers to the several groups in the subclass Acari, but it is not a clade, and excludes the ticks. Mites and ticks are similarly characterized by their bodies being divided into two parts, named the gnathosoma and idiosoma. The three major lineages of mites are recognized as Opilioacariformes, Acariformes and Parasitiformes [1]. 45,000 species of mites have been described, which is believed to be only small 5% of the number of species estimated to be alive today.&lt;br /&gt;
&lt;br /&gt;
==Characteristics==&lt;br /&gt;
&lt;br /&gt;
&#039;&#039;A Manual of Acarology&#039;&#039; has defined Acari to have the following characteristics [1]:&lt;br /&gt;
&lt;br /&gt;
*Hexapod prelarva (lost in Parasitiformes and many derived Acariformes)&lt;br /&gt;
&lt;br /&gt;
*Hexapod larval stage&lt;br /&gt;
&lt;br /&gt;
*Three octopod nymphal stages (variously abbreviated in derived taxa)&lt;br /&gt;
&lt;br /&gt;
*Gnathosoma delimited by a circumcapitular suture&lt;br /&gt;
&lt;br /&gt;
*Palpcoxal endites fused medially forming a hypostome&lt;br /&gt;
&lt;br /&gt;
*Hypostome with rutella or corniculi (lost in many derived Acariformes)&lt;br /&gt;
&lt;br /&gt;
*Loss of external evidence of opisthosomal segmentation, i.e. without tergites or sternites&lt;br /&gt;
&lt;br /&gt;
*Ingestion of particulate food (lost in many derived taxa)&lt;br /&gt;
&lt;br /&gt;
==Taxonomy==&lt;br /&gt;
&lt;br /&gt;
[[File:diversity of acari.jpg|thumb|right|Diversity of Acari [6]]]&lt;br /&gt;
Acari have been variously ranked as a group made up of one to seven or more distinct orders. The orders comprise approximately half of the described arachnid diversity. Molecular information from ribosomal DNA is used to expose relationships between groups. The 18 S rRNA gene provides information on relationships among phyla and superphyla, while the ITS2, and the 18S ribosomal RNA and 28S ribosomal RNA genes, show relationships at deeper levels [2]. Recent research has suggested that Acari is polyphyletic [3]. &#039;&#039;A Manual of Acarology&#039;&#039; uses a system of six orders, grouped into three superorders to classify Acari [2]:&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
*Superorder Opilioacariformes – a small order of large mites with about 20 known species&lt;br /&gt;
*Superorder Parasitiformes – ticks and a variety of mites&lt;br /&gt;
**Holothyrida - predatory mites from the southern hemisphere&lt;br /&gt;
**Ixodida – hard ticks and soft ticks&lt;br /&gt;
**Mesostigmata – excess of 65 families and 10,000 described species, including bird mites, phytoseiid mites&lt;br /&gt;
***Trigynaspida - large, diverse order&lt;br /&gt;
***Monogynaspida - diverse order of parasitic and predatory mites&lt;br /&gt;
*Superorder Acariformes – contains over 300 families and over 30, 000 described species&lt;br /&gt;
**Trombidiformes – plant parasitic mites (spider mites, peacock mites, gall mites, red-legged earth mites, etc.), snout mites, chiggers, hair follicle mites, velvet mites, water mites, etc.&lt;br /&gt;
***Sphaerolichida - small order of mites containing two families&lt;br /&gt;
***Prostigmata - large order of sucking mites&lt;br /&gt;
**Sarcoptiformes&lt;br /&gt;
***Oribatida – oribatid mites, beetle mites, armored mites (also cryptostigmata)&lt;br /&gt;
***Astigmatina – stored product, fur, feather, dust, and human itch mites, etc.&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
==Anatomy== &lt;br /&gt;
&lt;br /&gt;
[[File:mitie.jpg|thumb|right|Basic Mite Anatomy [7]]]&lt;br /&gt;
Mite size varies from 0.1 mm to 10 mm in length. They are most closely related to spiders than insects. They have the same characteristics of jointed legs and a chitinous exoskeleton. Acari have an open circulating system, ventral nerve cord, alimentary canal and striated muscles and may also possess Malpighian tubules. Acari lack antennae and mandibles [4]. The acarine body is divided into gnathosoma and idiosoma. The gnathosoma is the part of the body of the Acari comprising the mouth and feeding parts, and the idiosoma bears the legs, the genital and anal openings, and an assortment of tactile and sensory structures.&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
Walter, David Evans, Gerald Krantz, and Evert Lindquist. 1996. Acari. The Mites. Version 13 December 1996. http://tolweb.org/Acari/2554/1996.12.13 inThe Tree of Life Web Project, http://tolweb.org/&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
Pepato, Almir R, et al. “Phylogenetic Position of the Acariform Mites: Sensitivity to Homology Assessment under Total Evidence.” BMC Evolutionary Biology, BioMed Central, 2 Aug. 2010, bmcevolbiol.biomedcentral.com/articles/10.1186/1471-2148-10-235.&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
Sanggaard, Kristian W.; Bechsgaard, Jesper S.; Fang, Xiaodong (6 May 2014). &amp;quot;Spider genomes provide insight into composition and evolution of venom and silk&amp;quot;. Nature Communications. 5: 3765. Bibcode:2014NatCo...5E3765S. doi:10.1038/ncomms4765. PMC 4273655 Freely accessible. PMID 24801114.&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
Dhooria M.S. (2016) Morphology and Anatomy of Acari. In: Fundamentals of Applied Acarology. Springer, Singapore&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
“Acari.” Acari - Entomologists&#039; Glossary - Amateur Entomologists&#039; Society (AES), www.amentsoc.org/insects/glossary/terms/acari.&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
Wilson, Nixon A. “Acarid.” Encyclopædia Britannica, Encyclopædia Britannica, Inc., 27 Dec. 2017, www.britannica.com/animal/acarid.&lt;br /&gt;
&lt;br /&gt;
[7]&lt;br /&gt;
NCSU Veterinary Parasitology, parasitology.cvm.ncsu.edu/vmp930/keys/mites/miteterms.html.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Mites&amp;diff=1625</id>
		<title>Mites</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Mites&amp;diff=1625"/>
		<updated>2018-04-20T06:03:25Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==Definition==&lt;br /&gt;
&lt;br /&gt;
[[File:lorryia-formosa-mite.jpg|thumb|right|Lorryia formosa mite [5]]]&lt;br /&gt;
Mites are the most diverse of all arachnids, and among the oldest of all terrestrial animals. Fossils date mites from the early Devonian, nearly 400 million years ago [1.] Belonging to the class Archnida, the term &amp;quot;mite&amp;quot; refers to the several groups in the subclass Acari, but it is not a clade, and excludes the ticks. Mites and ticks are similarly characterized by their bodies being divided into two parts, named the gnathosoma and idiosoma. The three major lineages of mites are recognized as Opilioacariformes, Acariformes and Parasitiformes [1]. 45,000 species of mites have been described, which is believed to be only small 5% of the number of species estimated to be alive today.&lt;br /&gt;
&lt;br /&gt;
==Characteristics==&lt;br /&gt;
&lt;br /&gt;
The Acari have been defined by &#039;&#039;A Manual of Acarology&#039;&#039; to have the following characteristics [1]:&lt;br /&gt;
&lt;br /&gt;
*Hexapod prelarva (lost in Parasitiformes and many derived Acariformes)&lt;br /&gt;
&lt;br /&gt;
*Hexapod larval stage&lt;br /&gt;
&lt;br /&gt;
*Three octopod nymphal stages (variously abbreviated in derived taxa)&lt;br /&gt;
&lt;br /&gt;
*Gnathosoma delimited by a circumcapitular suture&lt;br /&gt;
&lt;br /&gt;
*Palpcoxal endites fused medially forming a hypostome&lt;br /&gt;
&lt;br /&gt;
*Hypostome with rutella or corniculi (lost in many derived Acariformes)&lt;br /&gt;
&lt;br /&gt;
*Loss of external evidence of opisthosomal segmentation, i.e. without tergites or sternites&lt;br /&gt;
&lt;br /&gt;
*Ingestion of particulate food (lost in many derived taxa)&lt;br /&gt;
&lt;br /&gt;
==Taxonomy==&lt;br /&gt;
&lt;br /&gt;
[[File:diversity of acari.jpg|thumb|right|Diversity of Acari [6]]]&lt;br /&gt;
Acari have been variously ranked as a group made up of one to seven or more distinct orders. The orders comprise approximately half of the described arachnid diversity. Molecular information from ribosomal DNA is used to expose relationships between groups. The 18 S rRNA gene provides information on relationships among phyla and superphyla, while the ITS2, and the 18S ribosomal RNA and 28S ribosomal RNA genes, show relationships at deeper levels [2]. Recent research has suggested that Acari is polyphyletic [3]. &#039;&#039;A Manual of Acarology&#039;&#039; uses a system of six orders, grouped into three superorders to classify Acari [2]:&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
*Superorder Opilioacariformes – a small order of large mites with about 20 known species&lt;br /&gt;
*Superorder Parasitiformes – ticks and a variety of mites&lt;br /&gt;
**Holothyrida - predatory mites from the southern hemisphere&lt;br /&gt;
**Ixodida – hard ticks and soft ticks&lt;br /&gt;
**Mesostigmata – excess of 65 families and 10,000 described species, including bird mites, phytoseiid mites&lt;br /&gt;
***Trigynaspida - large, diverse order&lt;br /&gt;
***Monogynaspida - diverse order of parasitic and predatory mites&lt;br /&gt;
*Superorder Acariformes – contains over 300 families and over 30, 000 described species&lt;br /&gt;
**Trombidiformes – plant parasitic mites (spider mites, peacock mites, gall mites, red-legged earth mites, etc.), snout mites, chiggers, hair follicle mites, velvet mites, water mites, etc.&lt;br /&gt;
***Sphaerolichida - small order of mites containing two families&lt;br /&gt;
***Prostigmata - large order of sucking mites&lt;br /&gt;
**Sarcoptiformes&lt;br /&gt;
***Oribatida – oribatid mites, beetle mites, armored mites (also cryptostigmata)&lt;br /&gt;
***Astigmatina – stored product, fur, feather, dust, and human itch mites, etc.&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
==Anatomy== &lt;br /&gt;
&lt;br /&gt;
[[File:mitie.jpg|thumb|right|Basic Mite Anatomy [7]]]&lt;br /&gt;
Mite size varies from 0.1 mm to 10 mm in length. They are most closely related to spiders than insects. They have the same characteristics of jointed legs and a chitinous exoskeleton. Acari have an open circulating system, ventral nerve cord, alimentary canal and striated muscles and may also possess Malpighian tubules. Acari lack antennae and mandibles [4]. The acarine body is divided into gnathosoma and idiosoma. The gnathosoma is the part of the body of the Acari comprising the mouth and feeding parts, and the idiosoma bears the legs, the genital and anal openings, and an assortment of tactile and sensory structures.&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
Walter, David Evans, Gerald Krantz, and Evert Lindquist. 1996. Acari. The Mites. Version 13 December 1996. http://tolweb.org/Acari/2554/1996.12.13 inThe Tree of Life Web Project, http://tolweb.org/&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
Pepato, Almir R, et al. “Phylogenetic Position of the Acariform Mites: Sensitivity to Homology Assessment under Total Evidence.” BMC Evolutionary Biology, BioMed Central, 2 Aug. 2010, bmcevolbiol.biomedcentral.com/articles/10.1186/1471-2148-10-235.&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
Sanggaard, Kristian W.; Bechsgaard, Jesper S.; Fang, Xiaodong (6 May 2014). &amp;quot;Spider genomes provide insight into composition and evolution of venom and silk&amp;quot;. Nature Communications. 5: 3765. Bibcode:2014NatCo...5E3765S. doi:10.1038/ncomms4765. PMC 4273655 Freely accessible. PMID 24801114.&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
Dhooria M.S. (2016) Morphology and Anatomy of Acari. In: Fundamentals of Applied Acarology. Springer, Singapore&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
“Acari.” Acari - Entomologists&#039; Glossary - Amateur Entomologists&#039; Society (AES), www.amentsoc.org/insects/glossary/terms/acari.&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
Wilson, Nixon A. “Acarid.” Encyclopædia Britannica, Encyclopædia Britannica, Inc., 27 Dec. 2017, www.britannica.com/animal/acarid.&lt;br /&gt;
&lt;br /&gt;
[7]&lt;br /&gt;
NCSU Veterinary Parasitology, parasitology.cvm.ncsu.edu/vmp930/keys/mites/miteterms.html.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Mites&amp;diff=1624</id>
		<title>Mites</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Mites&amp;diff=1624"/>
		<updated>2018-04-20T06:02:22Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==Definition==&lt;br /&gt;
&lt;br /&gt;
[[File:lorryia-formosa-mite.jpg|thumb|right|Lorryia formosa mite [5]]]&lt;br /&gt;
Mites are the most diverse of all arachnids, and among the oldest of all terrestrial animals. Fossils date mites from the early Devonian, nearly 400 million years ago [1.] Belonging to the class Archnida, the term &amp;quot;mite&amp;quot; refers to the several groups in the subclass Acari, but it is not a clade, and excludes the ticks. Mites and ticks are similarly characterized by their bodies being divided into two parts, named the gnathosoma and idiosoma. The three major lineages of mites are recognized as Opilioacariformes, Acariformes and Parasitiformes [1]. 45,000 species of mites have been described, which is believed to be only small 5% of the number of species estimated to be alive today.&lt;br /&gt;
&lt;br /&gt;
==Characteristics==&lt;br /&gt;
&lt;br /&gt;
The Acari have been defined by &#039;&#039;A Manual of Acarology&#039;&#039; to have the following characteristics [1]:&lt;br /&gt;
&lt;br /&gt;
*Hexapod prelarva (lost in Parasitiformes and many derived Acariformes)&lt;br /&gt;
&lt;br /&gt;
*Hexapod larval stage&lt;br /&gt;
&lt;br /&gt;
*Three octopod nymphal stages (variously abbreviated in derived taxa)&lt;br /&gt;
&lt;br /&gt;
*Gnathosoma delimited by a circumcapitular suture&lt;br /&gt;
&lt;br /&gt;
*Palpcoxal endites fused medially forming a hypostome&lt;br /&gt;
&lt;br /&gt;
*Hypostome with rutella or corniculi (lost in many derived Acariformes)&lt;br /&gt;
&lt;br /&gt;
*Loss of external evidence of opisthosomal segmentation, i.e. without tergites or sternites&lt;br /&gt;
&lt;br /&gt;
*Ingestion of particulate food (lost in many derived taxa)&lt;br /&gt;
&lt;br /&gt;
==Taxonomy==&lt;br /&gt;
&lt;br /&gt;
[[File:diversity of acari.jpg|thumb|right|Diversity of Acari [6]]]&lt;br /&gt;
Acari have been variously ranked as a group made up of one to seven or more distinct orders. The orders comprise approximately half of the described arachnid diversity. Molecular information from ribosomal DNA is used to expose relationships between groups. The 18 S rRNA gene provides information on relationships among phyla and superphyla, while the ITS2, and the 18S ribosomal RNA and 28S ribosomal RNA genes, show relationships at deeper levels [2]. Recent research has suggested that Acari is polyphyletic [3]. &#039;&#039;A Manual of Acarology&#039;&#039; uses a system of six orders, grouped into three superorders to classify Acari [2]:&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
*Superorder Opilioacariformes – a small order of large mites with about 20 known species&lt;br /&gt;
*Superorder Parasitiformes – ticks and a variety of mites&lt;br /&gt;
**Holothyrida - predatory mites from the southern hemisphere&lt;br /&gt;
**Ixodida – hard ticks and soft ticks&lt;br /&gt;
**Mesostigmata – excess of 65 families and 10,000 described species, including bird mites, phytoseiid mites&lt;br /&gt;
***Trigynaspida - large, diverse order&lt;br /&gt;
***Monogynaspida - diverse order of parasitic and predatory mites&lt;br /&gt;
*Superorder Acariformes – contains over 300 families and over 30, 000 described species&lt;br /&gt;
**Trombidiformes – plant parasitic mites (spider mites, peacock mites, gall mites, red-legged earth mites, etc.), snout mites, chiggers, hair follicle mites, velvet mites, water mites, etc.&lt;br /&gt;
***Sphaerolichida - small order of mites containing two families&lt;br /&gt;
***Prostigmata - large order of sucking mites&lt;br /&gt;
**Sarcoptiformes&lt;br /&gt;
***Oribatida – oribatid mites, beetle mites, armored mites (also cryptostigmata)&lt;br /&gt;
***Astigmatina – stored product, fur, feather, dust, and human itch mites, etc.&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
==Anatomy== &lt;br /&gt;
&lt;br /&gt;
[[File:mitie.jpg|thumb|right|Lorryia formosa mite [5]]]&lt;br /&gt;
Mite size varies from 0.1 mm to 10 mm in length. They are most closely related to spiders than insects. They have the same characteristics of jointed legs and a chitinous exoskeleton. Acari have an open circulating system, ventral nerve cord, alimentary canal and striated muscles and may also possess Malpighian tubules. Acari lack antennae and mandibles [4]. The acarine body is divided into gnathosoma and idiosoma. The gnathosoma is the part of the body of the Acari comprising the mouth and feeding parts, and the idiosoma bears the legs, the genital and anal openings, and an assortment of tactile and sensory structures.&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
Walter, David Evans, Gerald Krantz, and Evert Lindquist. 1996. Acari. The Mites. Version 13 December 1996. http://tolweb.org/Acari/2554/1996.12.13 inThe Tree of Life Web Project, http://tolweb.org/&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
Pepato, Almir R, et al. “Phylogenetic Position of the Acariform Mites: Sensitivity to Homology Assessment under Total Evidence.” BMC Evolutionary Biology, BioMed Central, 2 Aug. 2010, bmcevolbiol.biomedcentral.com/articles/10.1186/1471-2148-10-235.&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
Sanggaard, Kristian W.; Bechsgaard, Jesper S.; Fang, Xiaodong (6 May 2014). &amp;quot;Spider genomes provide insight into composition and evolution of venom and silk&amp;quot;. Nature Communications. 5: 3765. Bibcode:2014NatCo...5E3765S. doi:10.1038/ncomms4765. PMC 4273655 Freely accessible. PMID 24801114.&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
Dhooria M.S. (2016) Morphology and Anatomy of Acari. In: Fundamentals of Applied Acarology. Springer, Singapore&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
“Acari.” Acari - Entomologists&#039; Glossary - Amateur Entomologists&#039; Society (AES), www.amentsoc.org/insects/glossary/terms/acari.&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
Wilson, Nixon A. “Acarid.” Encyclopædia Britannica, Encyclopædia Britannica, Inc., 27 Dec. 2017, www.britannica.com/animal/acarid.&lt;br /&gt;
&lt;br /&gt;
[7]&lt;br /&gt;
NCSU Veterinary Parasitology, parasitology.cvm.ncsu.edu/vmp930/keys/mites/miteterms.html.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=File:Mitie.jpg&amp;diff=1623</id>
		<title>File:Mitie.jpg</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=File:Mitie.jpg&amp;diff=1623"/>
		<updated>2018-04-20T06:00:28Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Mites&amp;diff=1622</id>
		<title>Mites</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Mites&amp;diff=1622"/>
		<updated>2018-04-20T05:58:41Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==Definition==&lt;br /&gt;
&lt;br /&gt;
[[File:lorryia-formosa-mite.jpg|thumb|left|Lorryia formosa mite [5]]]&lt;br /&gt;
Mites are the most diverse of all arachnids, and among the oldest of all terrestrial animals. Fossils date mites from the early Devonian, nearly 400 million years ago [1.] Belonging to the class Archnida, the term &amp;quot;mite&amp;quot; refers to the several groups in the subclass Acari, but it is not a clade, and excludes the ticks. Mites and ticks are similarly characterized by their bodies being divided into two parts, named the gnathosoma and idiosoma. The three major lineages of mites are recognized as Opilioacariformes, Acariformes and Parasitiformes [1]. 45,000 species of mites have been described, which is believed to be only small 5% of the number of species estimated to be alive today.&lt;br /&gt;
&lt;br /&gt;
==Characteristics==&lt;br /&gt;
&lt;br /&gt;
The Acari have been defined by &#039;&#039;A Manual of Acarology&#039;&#039; to have the following characteristics [1]:&lt;br /&gt;
&lt;br /&gt;
*Hexapod prelarva (lost in Parasitiformes and many derived Acariformes)&lt;br /&gt;
&lt;br /&gt;
*Hexapod larval stage&lt;br /&gt;
&lt;br /&gt;
*Three octopod nymphal stages (variously abbreviated in derived taxa)&lt;br /&gt;
&lt;br /&gt;
*Gnathosoma delimited by a circumcapitular suture&lt;br /&gt;
&lt;br /&gt;
*Palpcoxal endites fused medially forming a hypostome&lt;br /&gt;
&lt;br /&gt;
*Hypostome with rutella or corniculi (lost in many derived Acariformes)&lt;br /&gt;
&lt;br /&gt;
*Loss of external evidence of opisthosomal segmentation, i.e. without tergites or sternites&lt;br /&gt;
&lt;br /&gt;
*Ingestion of particulate food (lost in many derived taxa)&lt;br /&gt;
&lt;br /&gt;
==Taxonomy==&lt;br /&gt;
&lt;br /&gt;
[[File:diversity of acari.jpg|thumb|right|Diversity of Acari [6]]]&lt;br /&gt;
Acari have been variously ranked as a group made up of one to seven or more distinct orders. The orders comprise approximately half of the described arachnid diversity. Molecular information from ribosomal DNA is used to expose relationships between groups. The 18 S rRNA gene provides information on relationships among phyla and superphyla, while the ITS2, and the 18S ribosomal RNA and 28S ribosomal RNA genes, show relationships at deeper levels [2]. Recent research has suggested that Acari is polyphyletic [3]. &#039;&#039;A Manual of Acarology&#039;&#039; uses a system of six orders, grouped into three superorders to classify Acari [2]:&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
*Superorder Opilioacariformes – a small order of large mites with about 20 known species&lt;br /&gt;
*Superorder Parasitiformes – ticks and a variety of mites&lt;br /&gt;
**Holothyrida - predatory mites from the southern hemisphere&lt;br /&gt;
**Ixodida – hard ticks and soft ticks&lt;br /&gt;
**Mesostigmata – excess of 65 families and 10,000 described species, including bird mites, phytoseiid mites&lt;br /&gt;
***Trigynaspida - large, diverse order&lt;br /&gt;
***Monogynaspida - diverse order of parasitic and predatory mites&lt;br /&gt;
*Superorder Acariformes – contains over 300 families and over 30, 000 described species&lt;br /&gt;
**Trombidiformes – plant parasitic mites (spider mites, peacock mites, gall mites, red-legged earth mites, etc.), snout mites, chiggers, hair follicle mites, velvet mites, water mites, etc.&lt;br /&gt;
***Sphaerolichida - small order of mites containing two families&lt;br /&gt;
***Prostigmata - large order of sucking mites&lt;br /&gt;
**Sarcoptiformes&lt;br /&gt;
***Oribatida – oribatid mites, beetle mites, armored mites (also cryptostigmata)&lt;br /&gt;
***Astigmatina – stored product, fur, feather, dust, and human itch mites, etc.&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
==Anatomy== &lt;br /&gt;
&lt;br /&gt;
Mite size varies from 0.1 mm to 10 mm in length. They are most closely related to spiders than insects. They have the same characteristics of jointed legs and a chitinous exoskeleton. Acari have an open circulating system, ventral nerve cord, alimentary canal and striated muscles and may also possess Malpighian tubules. Acari lack antennae and mandibles [4]. The acarine body is divided into gnathosoma and idiosoma. The gnathosoma is the part of the body of the Acari comprising the mouth and feeding parts, and the idiosoma bears the legs, the genital and anal openings, and an assortment of tactile and sensory structures.&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
Walter, David Evans, Gerald Krantz, and Evert Lindquist. 1996. Acari. The Mites. Version 13 December 1996. http://tolweb.org/Acari/2554/1996.12.13 inThe Tree of Life Web Project, http://tolweb.org/&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
Pepato, Almir R, et al. “Phylogenetic Position of the Acariform Mites: Sensitivity to Homology Assessment under Total Evidence.” BMC Evolutionary Biology, BioMed Central, 2 Aug. 2010, bmcevolbiol.biomedcentral.com/articles/10.1186/1471-2148-10-235.&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
Sanggaard, Kristian W.; Bechsgaard, Jesper S.; Fang, Xiaodong (6 May 2014). &amp;quot;Spider genomes provide insight into composition and evolution of venom and silk&amp;quot;. Nature Communications. 5: 3765. Bibcode:2014NatCo...5E3765S. doi:10.1038/ncomms4765. PMC 4273655 Freely accessible. PMID 24801114.&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
Dhooria M.S. (2016) Morphology and Anatomy of Acari. In: Fundamentals of Applied Acarology. Springer, Singapore&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
“Acari.” Acari - Entomologists&#039; Glossary - Amateur Entomologists&#039; Society (AES), www.amentsoc.org/insects/glossary/terms/acari.&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
Wilson, Nixon A. “Acarid.” Encyclopædia Britannica, Encyclopædia Britannica, Inc., 27 Dec. 2017, www.britannica.com/animal/acarid.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Mites&amp;diff=1621</id>
		<title>Mites</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Mites&amp;diff=1621"/>
		<updated>2018-04-20T05:57:38Z</updated>

		<summary type="html">&lt;p&gt;Elsbethd: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==Definition==&lt;br /&gt;
&lt;br /&gt;
[[File:lorryia-formosa-mite.jpg|thumb|right|Lorryia formosa mite [5]]]&lt;br /&gt;
Mites are the most diverse of all arachnids, and among the oldest of all terrestrial animals. Fossils date mites from the early Devonian, nearly 400 million years ago [1.] Belonging to the class Archnida, the term &amp;quot;mite&amp;quot; refers to the several groups in the subclass Acari, but it is not a clade, and excludes the ticks. Mites and ticks are similarly characterized by their bodies being divided into two parts, named the gnathosoma and idiosoma. The three major lineages of mites are recognized as Opilioacariformes, Acariformes and Parasitiformes [1]. 45,000 species of mites have been described, which is believed to be only small 5% of the number of species estimated to be alive today.&lt;br /&gt;
&lt;br /&gt;
==Characteristics==&lt;br /&gt;
&lt;br /&gt;
The Acari have been defined by &#039;&#039;A Manual of Acarology&#039;&#039; to have the following characteristics [1]:&lt;br /&gt;
&lt;br /&gt;
*Hexapod prelarva (lost in Parasitiformes and many derived Acariformes)&lt;br /&gt;
&lt;br /&gt;
*Hexapod larval stage&lt;br /&gt;
&lt;br /&gt;
*Three octopod nymphal stages (variously abbreviated in derived taxa)&lt;br /&gt;
&lt;br /&gt;
*Gnathosoma delimited by a circumcapitular suture&lt;br /&gt;
&lt;br /&gt;
*Palpcoxal endites fused medially forming a hypostome&lt;br /&gt;
&lt;br /&gt;
*Hypostome with rutella or corniculi (lost in many derived Acariformes)&lt;br /&gt;
&lt;br /&gt;
*Loss of external evidence of opisthosomal segmentation, i.e. without tergites or sternites&lt;br /&gt;
&lt;br /&gt;
*Ingestion of particulate food (lost in many derived taxa)&lt;br /&gt;
&lt;br /&gt;
==Taxonomy==&lt;br /&gt;
&lt;br /&gt;
[[File:diversity of acari.jpg|thumb|left|Diversity of Acari [6]]]&lt;br /&gt;
Acari have been variously ranked as a group made up of one to seven or more distinct orders. The orders comprise approximately half of the described arachnid diversity. Molecular information from ribosomal DNA is used to expose relationships between groups. The 18 S rRNA gene provides information on relationships among phyla and superphyla, while the ITS2, and the 18S ribosomal RNA and 28S ribosomal RNA genes, show relationships at deeper levels [2]. Recent research has suggested that Acari is polyphyletic [3]. &#039;&#039;A Manual of Acarology&#039;&#039; uses a system of six orders, grouped into three superorders to classify Acari [2]:&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
*Superorder Opilioacariformes – a small order of large mites with about 20 known species&lt;br /&gt;
*Superorder Parasitiformes – ticks and a variety of mites&lt;br /&gt;
**Holothyrida - predatory mites from the southern hemisphere&lt;br /&gt;
**Ixodida – hard ticks and soft ticks&lt;br /&gt;
**Mesostigmata – excess of 65 families and 10,000 described species, including bird mites, phytoseiid mites&lt;br /&gt;
***Trigynaspida - large, diverse order&lt;br /&gt;
***Monogynaspida - diverse order of parasitic and predatory mites&lt;br /&gt;
*Superorder Acariformes – contains over 300 families and over 30, 000 described species&lt;br /&gt;
**Trombidiformes – plant parasitic mites (spider mites, peacock mites, gall mites, red-legged earth mites, etc.), snout mites, chiggers, hair follicle mites, velvet mites, water mites, etc.&lt;br /&gt;
***Sphaerolichida - small order of mites containing two families&lt;br /&gt;
***Prostigmata - large order of sucking mites&lt;br /&gt;
**Sarcoptiformes&lt;br /&gt;
***Oribatida – oribatid mites, beetle mites, armored mites (also cryptostigmata)&lt;br /&gt;
***Astigmatina – stored product, fur, feather, dust, and human itch mites, etc.&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
==Anatomy== &lt;br /&gt;
&lt;br /&gt;
Mite size varies from 0.1 mm to 10 mm in length. They are most closely related to spiders than insects. They have the same characteristics of jointed legs and a chitinous exoskeleton. Acari have an open circulating system, ventral nerve cord, alimentary canal and striated muscles and may also possess Malpighian tubules. Acari lack antennae and mandibles [4]. The acarine body is divided into gnathosoma and idiosoma. The gnathosoma is the part of the body of the Acari comprising the mouth and feeding parts, and the idiosoma bears the legs, the genital and anal openings, and an assortment of tactile and sensory structures.&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
[1]&lt;br /&gt;
Walter, David Evans, Gerald Krantz, and Evert Lindquist. 1996. Acari. The Mites. Version 13 December 1996. http://tolweb.org/Acari/2554/1996.12.13 inThe Tree of Life Web Project, http://tolweb.org/&lt;br /&gt;
&lt;br /&gt;
[2]&lt;br /&gt;
Pepato, Almir R, et al. “Phylogenetic Position of the Acariform Mites: Sensitivity to Homology Assessment under Total Evidence.” BMC Evolutionary Biology, BioMed Central, 2 Aug. 2010, bmcevolbiol.biomedcentral.com/articles/10.1186/1471-2148-10-235.&lt;br /&gt;
&lt;br /&gt;
[3]&lt;br /&gt;
Sanggaard, Kristian W.; Bechsgaard, Jesper S.; Fang, Xiaodong (6 May 2014). &amp;quot;Spider genomes provide insight into composition and evolution of venom and silk&amp;quot;. Nature Communications. 5: 3765. Bibcode:2014NatCo...5E3765S. doi:10.1038/ncomms4765. PMC 4273655 Freely accessible. PMID 24801114.&lt;br /&gt;
&lt;br /&gt;
[4]&lt;br /&gt;
Dhooria M.S. (2016) Morphology and Anatomy of Acari. In: Fundamentals of Applied Acarology. Springer, Singapore&lt;br /&gt;
&lt;br /&gt;
[5]&lt;br /&gt;
“Acari.” Acari - Entomologists&#039; Glossary - Amateur Entomologists&#039; Society (AES), www.amentsoc.org/insects/glossary/terms/acari.&lt;br /&gt;
&lt;br /&gt;
[6]&lt;br /&gt;
Wilson, Nixon A. “Acarid.” Encyclopædia Britannica, Encyclopædia Britannica, Inc., 27 Dec. 2017, www.britannica.com/animal/acarid.&lt;/div&gt;</summary>
		<author><name>Elsbethd</name></author>
	</entry>
</feed>