Stagnosol
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High Quality Content by WIKIPEDIA articles! High Quality Content by WIKIPEDIA articles! A stagnosol in the FAO World Reference Base for Soil Resources is a soil with strong mottling of the soil profile due to redox processes caused by stagnating surfacewater. Stagnosols are periodically wet and mottled in the topsoil and subsoil, with or without concretions and/or bleaching. The topsoil can also be completely bleached (albic horizon). A common name in many national classification systems for most Stagnosols is pseudogley. In the USDA soil taxonomy, many of them belong to the Aqualfs, Aquults, Aquents, Aquepts and Aquolls. They are developed in a wide variety of unconsolidated materials like glacial till, and loamy aeolian, alluvial and colluvial deposits and physically weathered siltstone. Stagnosols occur on flat to gently sloping land in cool temperate to subtropical regions with humid to perhumid climate conditions.
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GarantieWeitere Informationen
- Allgemeine Informationen
- GTIN 09786131454325
- Genre Geowissenschaften
- Editor Lambert M. Surhone, Mariam T. Tennoe, Susan F. Henssonow
- Anzahl Seiten 76
- Herausgeber Betascript Publishing
- EAN 9786131454325
- Titel Stagnosol
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