Information About

Aridisols




Water deficiency is the major defining characteristic of Aridisols. Also required is sufficient age to exhibit sub-soil weathering and development. Imperfect leaching in Aridisols often results in one or more subsurface soil horizons in which suspended or dissolved minerals have been deposited: silicate clays, sodium, calcium carbonate, gypsum or soluble salts. These subsoil horizons can also be cemented by carbonates, gypsum or silica. Accumulation of salts on the surface can result in salinization.

SUBORDERS

: Argid s ( Clay )
:Calcids ( Carbonate )
:Cambidianouses (tropical)
:Cryrids ( Cold )
:Duripids (duripan)
: Gypsid s ( Gypsum )
: Salid s (salts)

REFERENCES

SSSA glossary - [http://www.soils.org/cgi-bin/gloss_search.cgi?QUERY=Aridisols aridisols]

USDA - NRCS - aridisols

University of Idaho - aridisols

University of Florida - aridisols



SEE ALSO

Pedogenesis

Pedology (soil Study)

Soil Classification

Soil Science

Soil Type