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Encyclopedia > Alfisols

Alfisols are a soil order in USA soil taxonomy. Alfisols form in semiarid to humid areas, typically under a hardwood forest cover. They have a clay and nutrient-enriched subsoil. Because of their productivity and abundance, the Alfisols represent one of the more important soil orders.


Suborders

Aqualfs — wet soils; aquic soil moisture regime
Boralfs — cold climate; frigid or cryic soil temperature regime
Udalfs — humid climate; udic moisture regime
Ustalfs — subhumid climate; ustic moisture regime
Xeralfs — Mediteranaean climate; xeric moisture regime

See also

Pedogenesis
Pedology (soil study)
Soil classification
Soil science
Soil type


External Links

SSSA glossary - alfisols (http://www.soils.org/cgi-bin/gloss_search.cgi?QUERY=Alfisols)
USDA - NRCS - alfisols (http://soils.usda.gov/technical/classification/orders/alfisols.html)
University of Idaho - alfisols (http://soils.ag.uidaho.edu/soilorders/alfisols.htm)
University of Florida - alfisols (http://grunwald.ifas.ufl.edu/Nat_resources/soil_orders/alfisols.htm)




  Results from FactBites:
 
Alfisols (3694 words)
The suborders of Alfisols are distinguished by soil temperature and soil moisture (Figure 1.).
Ustalfs are the Alfisols of subhumid to semiarid regions.
Alfisols with wet soil moisture conditions and redox depletions with a chroma of 2 or less (e.g.
Alfisols - Wikipedia, the free encyclopedia (82 words)
Alfisols are a soil order in USA soil taxonomy.
Alfisols form in semiarid to humid areas, typically under a hardwood forest cover.
Because of their productivity and abundance, the Alfisols represent one of the more important soil orders.
  More results at FactBites »


 
 

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