Difference between revisions of "Soil Horizons"
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| − | Soil Horizons are the distinct layers of a soil profile. They are divided into these layers (from top to bottom): O Horizon, A Horizon, E Horizon, B Horizon, C Horizon, and | + | Soil Horizons are the distinct layers of a soil profile. They are divided into these layers, referred to as "master horizons" (from top to bottom): O Horizon, A Horizon, E Horizon, B Horizon, C Horizon, and R Horizon. The amount of horizons can vary with different soils; the most well-developed soils have all of these layers, and the least-developed soils might only have an A and a D horizon. (This Page is under construction by Jason Kaczmarczyk) |
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| + | == O Horizon == | ||
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| + | The O Horizon is composed of organic material that has accumulated and been modified (physically and chemically) over time, typically from the remains of plant and animals. (Elements of the Nature and Properties of Soils, Second Edition, page 12. This citation is obviously not going to be here for the final submission; it's just a handy reference while I construct this page.) This horizon is most easily observed in soils that are rarely if ever disturbed and with plenty of foliage and/or organisms nearby to contribute to its development, such as forests. In more barren locations such as grasslands, an O Horizon is usually rarer. Due to its presence being determined by external factors (outside of the original parent material that form soils), it is the only layer not dominated by mineral substances. This layer has three well-accepted subordinate horizons: Oi (slightly decomposed organic matter), Oe (moderately decomposed organic matter), and Oa (highly decomposed organic matter). (Elements pg. 53) Microbial activity is high in this layer, utilizing the abundance of organic matter and decomposing it in ways that allow it to contribute to the soil profile. | ||
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| + | == A Horizon == | ||
| + | The A Horizon is a well-weathered and fertile layer dominated by mineral particles but still rich in organic matter, especially if covered by an O Horizon, which can leach decomposed organic matter into the A Horizon. This is a much thicker layer than the O Horizon, dominated by highly weathered mineral particles (the most highly weathered from the parent material of the soil), and typically darker and coarser than other Soil Horizons. (Elements pg. 53) The A Horizon (and the O Horizon, if present) is considered ''topsoil''. Subterranean life (including microfauna, mesofauna, and macrofauna) tend to be the most abundant in this layer. (Add how plants utilize this layer at a later point.) | ||
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| + | == E Horizon == | ||
| + | The E in "E Horizon" stands for ''eluviation'', another word for leaching. This name is appropriate because in this layer clay, iron, and aluminum oxides leach into the lower layers (mostly the B Horizon). (Elements pg. 54) Like the O Horizon, this layer is not always present, but when it is, it's usually in forested areas and rarely in grasslands. Because of the loss of material through eluviation, it tends to be noticeably lighter than the layers above and below it. | ||
Revision as of 21:59, 5 March 2018
Soil Horizons are the distinct layers of a soil profile. They are divided into these layers, referred to as "master horizons" (from top to bottom): O Horizon, A Horizon, E Horizon, B Horizon, C Horizon, and R Horizon. The amount of horizons can vary with different soils; the most well-developed soils have all of these layers, and the least-developed soils might only have an A and a D horizon. (This Page is under construction by Jason Kaczmarczyk)
O Horizon
The O Horizon is composed of organic material that has accumulated and been modified (physically and chemically) over time, typically from the remains of plant and animals. (Elements of the Nature and Properties of Soils, Second Edition, page 12. This citation is obviously not going to be here for the final submission; it's just a handy reference while I construct this page.) This horizon is most easily observed in soils that are rarely if ever disturbed and with plenty of foliage and/or organisms nearby to contribute to its development, such as forests. In more barren locations such as grasslands, an O Horizon is usually rarer. Due to its presence being determined by external factors (outside of the original parent material that form soils), it is the only layer not dominated by mineral substances. This layer has three well-accepted subordinate horizons: Oi (slightly decomposed organic matter), Oe (moderately decomposed organic matter), and Oa (highly decomposed organic matter). (Elements pg. 53) Microbial activity is high in this layer, utilizing the abundance of organic matter and decomposing it in ways that allow it to contribute to the soil profile.
A Horizon
The A Horizon is a well-weathered and fertile layer dominated by mineral particles but still rich in organic matter, especially if covered by an O Horizon, which can leach decomposed organic matter into the A Horizon. This is a much thicker layer than the O Horizon, dominated by highly weathered mineral particles (the most highly weathered from the parent material of the soil), and typically darker and coarser than other Soil Horizons. (Elements pg. 53) The A Horizon (and the O Horizon, if present) is considered topsoil. Subterranean life (including microfauna, mesofauna, and macrofauna) tend to be the most abundant in this layer. (Add how plants utilize this layer at a later point.)
E Horizon
The E in "E Horizon" stands for eluviation, another word for leaching. This name is appropriate because in this layer clay, iron, and aluminum oxides leach into the lower layers (mostly the B Horizon). (Elements pg. 54) Like the O Horizon, this layer is not always present, but when it is, it's usually in forested areas and rarely in grasslands. Because of the loss of material through eluviation, it tends to be noticeably lighter than the layers above and below it.