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Subject Item
n2:ENVO_00002231
rdf:type
owl:Class
rdfs:label
alisol
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n2:ENVO_00001998
n2:IAO_0000115
Alisols are soils that have a higher clay content in the subsoil than in the topsoil as a result of pedogenetic processes (especially clay migration) leading to an argic subsoil horizon. Alisols have a low base saturation at certain depths and high-activity clays throughout the argic horizon. They lack the albeluvic tonguing as in Albeluvisols. They occur predominantly in humid tropical, humid subtropical and warm temperate regions.
obo:hasOBONamespace
ENVO
obo:id
ENVO:00002231