Hydric soil: Difference between revisions
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== Overview == |
== Overview == |
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Most [[soil]]s are [[Wikt:aerobic|aerobic]]. ) and there must be sufficient air—especially oxygen—in the soil to support most forms of [[soil life]]. Air normally moves through interconnected [[porosity|pores]] by forces such as changes in [[atmospheric pressure]], the flushing action of rainwater, and by simple [[diffusion]]. |
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In addition to plant [[root]]s, m] need oxygen to survive. This is true of the more well-known soil animals as well, such as [[ants]], [[earthworms]] and [[Mole (animal)|moles]]. But soils can often become saturated with water due to rainfall and flooding. [[Gas diffusion in soil]] slows (some 10,000 times slower) when soil becomes saturated with water because there are no open passageways for air to travel. When oxygen levels become limited, intense competition arises between soil life forms for the remaining oxygen. When this anaerobic environment continues for long periods during the growing season, quite different biological and chemical reactions begin to dominate, compared with aerobic soils. In soils where saturation with water is prolonged and is repeated for many years, unique soil properties usually develop that can be recognized in the field. Soils with these unique properties are called hydric soils, and although they may occupy a relatively small portion of the landscape, they maintain important functions in the environment<ref>Schuyt, K. and Brander, L. 2004. Living Waters: Conserving the Source of Life – The Economic Values of theWorld’sWetlands. Amsterdam, the Netherlands: European Union, and Gland, Switzerland: World Wildlife Fund.</ref>. |
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The plants found in hydric soils often have [[aerenchyma]], internal spaces in stems and rhizomes, that allow atmospheric oxygen to be transported to the rooting zone<ref>Justin, S. H. F. W. and Armstrong, W. 1987. The anatomical characteristics of roots and plant response to soil flooding. New Phytologist 106: 465–95.</ref>. Hence, many [[wetlands]] are dominated by plants with aerenchyma<ref>Keddy, P.A. 2010. Wetland Ecology: Principles and Conservation (2nd edition). Cambridge University Press, Cambridge, UK.</ref>; common examples include cattails, sedges and water-lillies. |
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==References== |
==References== |
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Revision as of 11:39, 10 September 2012
A hydric soil is a soil that formed under conditions of saturation, flooding, or ponding long enough during the growing season to develop anaerobic conditions in the upper part.[1]
This term is part of the legal definition of a wetland included in the United States Food Security Act of 1985 (P.L. 99-198). The US Natural Resources Conservation Service maintains the official list of hydric soils.
Overview
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References
- ^ This definition (Federal Register, July 13, 1994) replaced the older 1991 version and accomplished two things. First, a soil that is artificially drained or protected (ditches, levees, etc.) is a hydric soil if the soil in its undisturbed state meets the definition of a hydric soil. Estimated soil properties for manipulated soils are based on best professional estimates of the properties thought to exist before manipulation. Second, the link between the definition and criteria was removed.
Notes
See also
References
USDA-NRCS Hydric Soils Technical Note 1: Proper use of Hydric Soil Terminology. Url last accessed 2006-04-16
Bibliography
Environmental Laboratory. 1987. Corps of Engineers Wetland Delineation Manual, Technical Report Y-87-1, U.S. Army Engineer Waterways Experiment Station, Vicksburg, Miss. Url (pdf) last accessed 2006-04-16
Soil Conservation Service. 1994. National Food Security Act Manual. Title 180. USDA Soil Conservation Service, Washington, D.C.
Soil Survey Staff. 1999. Soil Taxonomy: A Basic System of Soil Classification for Making and Interpreting Soil Surveys. USDA Natural Resources Conservation Service, Agric. Hdbk. 436, U.S. Government Printing Office, Washington, D.C. 869 pp.
Soil Survey Staff. 1994. National Soil Survey Handbook. USDA Soil Conservation Service, Washington, D.C.