Drilosphere - Revision history

Njhenshu: The LinkTitles extension automatically added links to existing pages (https://github.com/bovender/LinkTitles).

2022-05-06T18:02:08Z

The LinkTitles extension automatically added links to existing pages (<a rel="nofollow" class="external free" href="https://github.com/bovender/LinkTitles">https://github.com/bovender/LinkTitles</a>).

← Older revision		Revision as of 14:02, 6 May 2022
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	(1) Cuddington, Kim, et al. Ecosystem Engineers: Plants to Protists. Academic Press, 2007.		(1) Cuddington, Kim, et al. Ecosystem Engineers: Plants to Protists. Academic Press, 2007.

	(2)Brown, George, et al. Regulation of Soil Organic Matter Dynamics and Microbial Activityin the Drilosphere and the Role of Interactionswith Other Edaphic Functional Domains. European Journal of Soil Biology.		(2)Brown, George, et al. Regulation of Soil [[Organic Matter]] Dynamics and Microbial Activityin the Drilosphere and the Role of Interactionswith Other Edaphic Functional Domains. European Journal of Soil Biology.

	(3) https://www.sas.upenn.edu/~rlenet/Earthworms.html		(3) https://www.sas.upenn.edu/~rlenet/Earthworms.html

Njhenshu: The LinkTitles extension automatically added links to existing pages (https://github.com/bovender/LinkTitles).

2021-04-29T17:04:01Z

← Older revision		Revision as of 13:04, 29 April 2021
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	The drilosphere is defined as the whole soil volume that is under the influence of earthworms, including the earthworm's burrow as well as the body and internal structures of the worm that come in contact with the soil. (2) It generally includes the burrow of the earthworm and the area 2mm away from it, but some effects are known to extend to 4 to 8mm away from it. (4) As ecosystem engineers, earthworms have the ability to change the soil, both physiochemically and biologically (2). The drilosphere has the characteristics of a self-organized system, completely different from the surrounding soil. (1)		The drilosphere is defined as the whole [[soil]] volume that is under the influence of earthworms, including the [[earthworm]]'s burrow as well as the body and internal structures of the worm that come in contact with the soil. (2) It generally includes the burrow of the earthworm and the area 2mm away from it, but some effects are known to extend to 4 to 8mm away from it. (4) As ecosystem engineers, earthworms have the ability to change the soil, both physiochemically and biologically (2). The drilosphere has the characteristics of a self-organized system, completely different from the surrounding soil. (1)

	[[File:Nature worms ecosystem.jpg\|thumb\|The three different ecological groups of earthworms depicted in the types of burrow they dig.(5)]]		[[File:Nature worms ecosystem.jpg\|thumb\|The three different ecological groups of earthworms depicted in the types of burrow they dig.(5)]]
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	(3) https://www.sas.upenn.edu/~rlenet/Earthworms.html		(3) https://www.sas.upenn.edu/~rlenet/Earthworms.html

	(4)Johnson-Maynard, Jodi L., and Daniel G. Strawn. “Linking Physical and Biogeochemical Properties and Processes in the Drilosphere.” Soil Science, vol. 181, no. 3/4, 2016, pp. 126–132.		(4)Johnson-Maynard, Jodi L., and Daniel G. Strawn. “Linking Physical and Biogeochemical [[Properties]] and Processes in the Drilosphere.” Soil Science, vol. 181, no. 3/4, 2016, pp. 126–132.

	(5) https://kollathdesign.com/portfolio/worm-burrow-diagram/		(5) https://kollathdesign.com/portfolio/worm-burrow-diagram/

Jleidner: /* Earthworms and Soil Properties */

2018-05-11T11:44:15Z

Earthworms and Soil Properties

← Older revision		Revision as of 07:44, 11 May 2018
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	=Earthworms and Soil Properties=		=Earthworms and Soil Properties=
	Earthworms have the ability to influence macroporosity, infiltration rates, air permeability, ~~and~~ aggregate stability. (4) One experiment found a positive relationship between earthworm burrow length and and saturated hydraulic conductivity, or the ease with which water can move through pore space. Earthworms are known to increase the formation of [[macroaggregates]]. (4) Another study found that earthworms reduce surface crusting by increasing aggregate stability and infiltration rates. (4) This is caused by the aggregation of organic matter and [[sand]], [[silt]], and [[clay]] particles into structural units through the digestion and secretion of soil by the earthworm~~. (4) Earthworms have been known to improve soil properties such as infiltration, aggregate stability, and water-holding capacity~~. (4) The drilosphere was found to have lower pore diameter and specific pore volume than bulk soil. (4) Water content at field capacity, carbon mineralization rates, and the ratio of carbon mineralization rates to total carbon were greater in the drilosphere than bulk soil. (4)		Earthworms have the ability to influence macroporosity, infiltration rates, air permeability, aggregate stability, and water holding capacity. (4) One experiment found a positive relationship between earthworm burrow length and and saturated hydraulic conductivity, or the ease with which water can move through pore space. Earthworms are known to increase the formation of [[macroaggregates]]. (4) Another study found that earthworms reduce surface crusting by increasing aggregate stability and infiltration rates. (4) This is caused by the aggregation of organic matter and [[sand]], [[silt]], and [[clay]] particles into structural units through the digestion and secretion of soil by the earthworm. (4) The drilosphere was found to have lower pore diameter and specific pore volume than bulk soil. (4) Water content at field capacity, carbon mineralization rates, and the ratio of carbon mineralization rates to total carbon were greater in the drilosphere than bulk soil. (4)

	One study done by Andriuzzi that added 13C and 15N to plant litter around earthworm burrows found that, after 45 days, earthworm activity had increased nutrients in the drilosphere, as well as up to 50-75 mm from the soil. (4)		One study done by Andriuzzi that added 13C and 15N to plant litter around earthworm burrows found that, after 45 days, earthworm activity had increased nutrients in the drilosphere, as well as up to 50-75 mm from the soil. (4)

Jleidner: /* Earthworms and Soil Properties */

2018-05-11T11:43:29Z

Earthworms and Soil Properties

← Older revision		Revision as of 07:43, 11 May 2018
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	=Earthworms and Soil Properties=		=Earthworms and Soil Properties=
	Earthworms have the ability to influence macroporosity, infiltration rates, air permeability, and aggregate stability. (4) One experiment found a positive relationship between earthworm burrow length and and saturated hydraulic conductivity, or the ease with which water can move through pore space. Earthworms are known to increase the formation of [[macroaggregates]]. (4) Another study found that earthworms reduce surface crusting by increasing aggregate stability and infiltration rates. (4) This is caused by the aggregation of organic matter and [[sand]], [[silt]], and [[clay]] particles into structural units. (4) Earthworms have been known to improve soil properties such as infiltration, aggregate stability, and water-holding capacity. (4) The drilosphere was found to have lower pore diameter and specific pore volume than bulk soil. (4) Water content at field capacity, carbon mineralization rates, and the ratio of carbon mineralization rates to total carbon were greater in the drilosphere than bulk soil. (4)		Earthworms have the ability to influence macroporosity, infiltration rates, air permeability, and aggregate stability. (4) One experiment found a positive relationship between earthworm burrow length and and saturated hydraulic conductivity, or the ease with which water can move through pore space. Earthworms are known to increase the formation of [[macroaggregates]]. (4) Another study found that earthworms reduce surface crusting by increasing aggregate stability and infiltration rates. (4) This is caused by the aggregation of organic matter and [[sand]], [[silt]], and [[clay]] particles into structural units through the digestion and secretion of soil by the earthworm. (4) Earthworms have been known to improve soil properties such as infiltration, aggregate stability, and water-holding capacity. (4) The drilosphere was found to have lower pore diameter and specific pore volume than bulk soil. (4) Water content at field capacity, carbon mineralization rates, and the ratio of carbon mineralization rates to total carbon were greater in the drilosphere than bulk soil. (4)

	One study done by Andriuzzi that added 13C and 15N to plant litter around earthworm burrows found that, after 45 days, earthworm activity had increased nutrients in the drilosphere, as well as up to 50-75 mm from the soil. (4)		One study done by Andriuzzi that added 13C and 15N to plant litter around earthworm burrows found that, after 45 days, earthworm activity had increased nutrients in the drilosphere, as well as up to 50-75 mm from the soil. (4)

Jleidner: /* Earthworms and Soil Properties */

2018-05-11T11:42:44Z

Earthworms and Soil Properties

← Older revision		Revision as of 07:42, 11 May 2018
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	=Earthworms and Soil Properties=		=Earthworms and Soil Properties=
	Earthworms have the ability to influence macroporosity, infiltration rates, air permeability, and aggregate stability. (4) One experiment found a positive relationship between earthworm burrow length and and saturated hydraulic conductivity, or the ease with which water can move through pore space. (4) Another study found that earthworms reduce surface crusting by increasing aggregate stability and infiltration rates. (4) This is caused by the aggregation of organic matter and [[sand]], [[silt]], and [[clay]] particles into structural units. (4) ~~Earthworms are known to increase the formation of [[macroaggregates]].~~ Earthworms have been known to improve soil properties such as infiltration, aggregate stability, and water-holding capacity. (4) The drilosphere was found to have lower pore diameter and specific pore volume than bulk soil. (4) Water content at field capacity, carbon mineralization rates, and the ratio of carbon mineralization rates to total carbon were greater in the drilosphere than bulk soil. (4)		Earthworms have the ability to influence macroporosity, infiltration rates, air permeability, and aggregate stability. (4) One experiment found a positive relationship between earthworm burrow length and and saturated hydraulic conductivity, or the ease with which water can move through pore space. Earthworms are known to increase the formation of [[macroaggregates]]. (4) Another study found that earthworms reduce surface crusting by increasing aggregate stability and infiltration rates. (4) This is caused by the aggregation of organic matter and [[sand]], [[silt]], and [[clay]] particles into structural units. (4) Earthworms have been known to improve soil properties such as infiltration, aggregate stability, and water-holding capacity. (4) The drilosphere was found to have lower pore diameter and specific pore volume than bulk soil. (4) Water content at field capacity, carbon mineralization rates, and the ratio of carbon mineralization rates to total carbon were greater in the drilosphere than bulk soil. (4)

	One study done by Andriuzzi that added 13C and 15N to plant litter around earthworm burrows found that, after 45 days, earthworm activity had increased nutrients in the drilosphere, as well as up to 50-75 mm from the soil. (4)		One study done by Andriuzzi that added 13C and 15N to plant litter around earthworm burrows found that, after 45 days, earthworm activity had increased nutrients in the drilosphere, as well as up to 50-75 mm from the soil. (4)

	A study in 1999 done by Tiuov and Scheu found that organic carbon, total nitrogen, pH, basal respiration, microbial biomass, and bacterial volume were significantly higher in the drilosphere than in the surrounding bulk soil. (4)		A study in 1999 done by Tiuov and Scheu found that organic carbon, total nitrogen, pH, basal respiration, microbial biomass, and bacterial volume were significantly higher in the drilosphere than in the surrounding bulk soil. (4)


	=Castings=		=Castings=

Jleidner at 20:17, 10 May 2018

2018-05-10T20:17:28Z

← Older revision		Revision as of 16:17, 10 May 2018
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	The drilosphere is defined as the whole soil volume that is under the influence of earthworms, including the earthworm's burrow as well as the body and internal structures of the worm that come in contact with the soil. (2) As ecosystem engineers, earthworms have the ability to change the soil, both physiochemically and biologically (2). The drilosphere has the characteristics of a self-organized system, completely different from the surrounding soil. (1~~) The drilosphere generally includes the burrow of the earthworm and the area 2mm away from it, but some effects are known to extend to 4 to 8mm away from it. (4~~)		The drilosphere is defined as the whole soil volume that is under the influence of earthworms, including the earthworm's burrow as well as the body and internal structures of the worm that come in contact with the soil. (2) It generally includes the burrow of the earthworm and the area 2mm away from it, but some effects are known to extend to 4 to 8mm away from it. (4) As ecosystem engineers, earthworms have the ability to change the soil, both physiochemically and biologically (2). The drilosphere has the characteristics of a self-organized system, completely different from the surrounding soil. (1)

	[[File:Nature worms ecosystem.jpg\|thumb\|The three different ecological groups of earthworms depicted in the types of burrow they dig.(5)]]		[[File:Nature worms ecosystem.jpg\|thumb\|The three different ecological groups of earthworms depicted in the types of burrow they dig.(5)]]

Jleidner at 20:16, 10 May 2018

2018-05-10T20:16:33Z

← Older revision		Revision as of 16:16, 10 May 2018
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	The drilosphere is defined as the whole soil volume that is under the influence of earthworms, including the earthworm's burrow as well as the body and internal structures of the worm that come in contact with the soil. (2) As ecosystem engineers, earthworms have the ability to change the soil, both physiochemically and biologically (2). The drilosphere has the characteristics of a self-organized system, completely different from the surrounding soil. (1) The drilosphere generally includes the burrow of the earthworm and the area 2mm away from it, but some effects are known to extend to 4 to 8mm away from it. (4)		The drilosphere is defined as the whole soil volume that is under the influence of earthworms, including the earthworm's burrow as well as the body and internal structures of the worm that come in contact with the soil. (2) As ecosystem engineers, earthworms have the ability to change the soil, both physiochemically and biologically (2). The drilosphere has the characteristics of a self-organized system, completely different from the surrounding soil. (1) The drilosphere generally includes the burrow of the earthworm and the area 2mm away from it, but some effects are known to extend to 4 to 8mm away from it. (4)

	[[File:Nature worms ecosystem.jpg\|thumb]]		[[File:Nature worms ecosystem.jpg\|thumb\|The three different ecological groups of earthworms depicted in the types of burrow they dig.(5)]]

	The term drilosphere was first coined in 1975 by M.B. Bouche. (4)		The term drilosphere was first coined in 1975 by M.B. Bouche. (4)
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	(4)Johnson-Maynard, Jodi L., and Daniel G. Strawn. “Linking Physical and Biogeochemical Properties and Processes in the Drilosphere.” Soil Science, vol. 181, no. 3/4, 2016, pp. 126–132.		(4)Johnson-Maynard, Jodi L., and Daniel G. Strawn. “Linking Physical and Biogeochemical Properties and Processes in the Drilosphere.” Soil Science, vol. 181, no. 3/4, 2016, pp. 126–132.

			(5) https://kollathdesign.com/portfolio/worm-burrow-diagram/

Jleidner at 20:15, 10 May 2018

2018-05-10T20:15:11Z

← Older revision		Revision as of 16:15, 10 May 2018
Line 1:		Line 1:
	The drilosphere is defined as the whole soil volume that is under the influence of earthworms, including the earthworm's burrow as well as the body and internal structures of the worm that come in contact with the soil. (2) As ecosystem engineers, earthworms have the ability to change the soil, both physiochemically and biologically (2). The drilosphere has the characteristics of a self-organized system, completely different from the surrounding soil. (1) The drilosphere generally includes the burrow of the earthworm and the area 2mm away from it, but some effects are known to extend to 4 to 8mm away from it. (4)		The drilosphere is defined as the whole soil volume that is under the influence of earthworms, including the earthworm's burrow as well as the body and internal structures of the worm that come in contact with the soil. (2) As ecosystem engineers, earthworms have the ability to change the soil, both physiochemically and biologically (2). The drilosphere has the characteristics of a self-organized system, completely different from the surrounding soil. (1) The drilosphere generally includes the burrow of the earthworm and the area 2mm away from it, but some effects are known to extend to 4 to 8mm away from it. (4)

			[[File:Nature worms ecosystem.jpg\|thumb]]

	The term drilosphere was first coined in 1975 by M.B. Bouche. (4)		The term drilosphere was first coined in 1975 by M.B. Bouche. (4)

Jleidner at 20:11, 10 May 2018

2018-05-10T20:11:14Z

← Older revision		Revision as of 16:11, 10 May 2018
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	The drilosphere is defined as the whole soil volume that is under the influence of earthworms, including the earthworm's burrow as well as the body and internal structures of the worm that come in contact with the soil. (2) As ecosystem engineers~~(1)~~, earthworms have the ability to change the soil, both physiochemically and biologically (2). The drilosphere has the characteristics of a self-organized system, completely different from the surrounding soil. (1~~) Earthworms have been known to improve soil properties such as infiltration, aggregate stability, and water-holding capacity. (4~~) The drilosphere generally includes the burrow of the earthworm and the area 2mm away from it, but some effects are known to extend to 4 to 8mm away from it. (4) The drilosphere was found to have lower pore diameter and specific pore volume than bulk soil. (4) Water content at field capacity, carbon mineralization rates, and the ratio of carbon mineralization rates to total carbon were greater in the drilosphere than bulk soil. (4)		The drilosphere is defined as the whole soil volume that is under the influence of earthworms, including the earthworm's burrow as well as the body and internal structures of the worm that come in contact with the soil. (2) As ecosystem engineers, earthworms have the ability to change the soil, both physiochemically and biologically (2). The drilosphere has the characteristics of a self-organized system, completely different from the surrounding soil. (1) The drilosphere generally includes the burrow of the earthworm and the area 2mm away from it, but some effects are known to extend to 4 to 8mm away from it. (4)


			The term drilosphere was first coined in 1975 by M.B. Bouche. (4)

			=Earthworms and Soil Properties=
			Earthworms have the ability to influence macroporosity, infiltration rates, air permeability, and aggregate stability. (4) One experiment found a positive relationship between earthworm burrow length and and saturated hydraulic conductivity, or the ease with which water can move through pore space. (4) Another study found that earthworms reduce surface crusting by increasing aggregate stability and infiltration rates. (4) This is caused by the aggregation of organic matter and [[sand]], [[silt]], and [[clay]] particles into structural units. (4) Earthworms are known to increase the formation of [[macroaggregates]]. Earthworms have been known to improve soil properties such as infiltration, aggregate stability, and water-holding capacity. (4) The drilosphere was found to have lower pore diameter and specific pore volume than bulk soil. (4) Water content at field capacity, carbon mineralization rates, and the ratio of carbon mineralization rates to total carbon were greater in the drilosphere than bulk soil. (4)

	One study done by Andriuzzi that added 13C and 15N to plant litter around earthworm burrows found that, after 45 days, earthworm activity had increased nutrients in the drilosphere, as well as up to 50-75 mm from the soil. (4)		One study done by Andriuzzi that added 13C and 15N to plant litter around earthworm burrows found that, after 45 days, earthworm activity had increased nutrients in the drilosphere, as well as up to 50-75 mm from the soil. (4)
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	A study in 1999 done by Tiuov and Scheu found that organic carbon, total nitrogen, pH, basal respiration, microbial biomass, and bacterial volume were significantly higher in the drilosphere than in the surrounding bulk soil. (4)		A study in 1999 done by Tiuov and Scheu found that organic carbon, total nitrogen, pH, basal respiration, microbial biomass, and bacterial volume were significantly higher in the drilosphere than in the surrounding bulk soil. (4)


	~~The term drilosphere was first coined in 1975 by M.B. Bouche. (4)~~

	~~=Earthworms and Soil Properties=~~
	Earthworms have the ability to influence macroporosity, infiltration rates, air permeability, and aggregate stability. (4) One experiment found a positive relationship between earthworm burrow length and and saturated hydraulic conductivity, or the ease with which water can move through pore space. (4) Another study found that earthworms reduce surface crusting by increasing aggregate stability and infiltration rates. (4) This is caused by the aggregation of organic matter and [[sand]], [[silt]], and [[clay]] particles into structural units. (4) Earthworms are known to increase the formation of [[macroaggregates]]

	=Castings=		=Castings=

Jleidner: /* Earthworms and Soil Properties */

2018-05-10T20:08:14Z

Earthworms and Soil Properties

← Older revision		Revision as of 16:08, 10 May 2018
Line 9:		Line 9:

	=Earthworms and Soil Properties=		=Earthworms and Soil Properties=
	Earthworms have the ability to influence macroporosity, infiltration rates, air permeability, and aggregate stability. (4) One experiment found a positive relationship between earthworm burrow length and and saturated hydraulic conductivity, of the ease with which water can move through pore space. (4) Another study found that earthworms reduce surface crusting by increasing aggregate stability and infiltration rates. (4) This is caused by the aggregation of organic matter and [[sand]], [[silt]], and [[clay]] particles into structural units. (4) Earthworms are known to increase the formation of [[macroaggregates]]		Earthworms have the ability to influence macroporosity, infiltration rates, air permeability, and aggregate stability. (4) One experiment found a positive relationship between earthworm burrow length and and saturated hydraulic conductivity, or the ease with which water can move through pore space. (4) Another study found that earthworms reduce surface crusting by increasing aggregate stability and infiltration rates. (4) This is caused by the aggregation of organic matter and [[sand]], [[silt]], and [[clay]] particles into structural units. (4) Earthworms are known to increase the formation of [[macroaggregates]]

	=Castings=		=Castings=