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1 Suborders  





2 References  














Inceptisol






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From Wikipedia, the free encyclopedia
 


Inceptisol
Inceptisol profile
Used inUSDA soil taxonomy

Inceptisols are a soil order in USDA soil taxonomy. They form quickly through alteration of parent material. They are more developed than Entisols.[1] They have no accumulation of clays, iron oxide, aluminium oxide or organic matter. They have an ochric or umbric horizon and a cambic subsurface horizon.

In the World Reference Base for Soil Resources (WRB), most Inceptisols are CambisolsorUmbrisols. Some may be Nitisols. Many Aquepts belong to Gleysols and Stagnosols.[2]

Suborders[edit]

References[edit]

  1. ^ "Inceptisols". Michigan State University.
  • ^ IUSS Working Group WRB (2015). "World Reference Base for Soil Resources 2014, Update 2015" (PDF). World Soil Resources Reports 106, FAO, Rome.

  • Retrieved from "https://en.wikipedia.org/w/index.php?title=Inceptisol&oldid=1134770872"

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