Soil Horizon
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High Quality Content by WIKIPEDIA articles! High Quality Content by WIKIPEDIA articles! A soil horizon is a specific layer in the land area which measures parallel to the soil surface and possesses physical characteristics which differ from the layers above and beneath. Horizon formation is a function of a range of geological, chemical, and biological processes and occurs over long time periods. Soils vary in the degree to which horizons are expressed. Relatively new deposits of soil parent material, such as alluvium, sand dunes, or volcanic ash, may have no horizon formation, or only the distinct layers of deposition. As age increases, horizons generally are more easily observed. The exception occurs in some older soils, with few horizons expressed in deeply weathered soils, such as the oxisols in tropical areas with high annual precipitation.
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GarantieWeitere Informationen
- Allgemeine Informationen
- GTIN 09786131452987
- Genre Geowissenschaften
- Editor Lambert M. Surhone, Mariam T. Tennoe, Susan F. Henssonow
- Anzahl Seiten 68
- Herausgeber Betascript Publishing
- EAN 9786131452987
- Titel Soil Horizon
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