Entisol

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Entisol
Entisol profile.jpg
Entisol profile showing little or no evidence of pedogenic horizon development
Used inUSDA soil taxonomy

In USDA soil taxonomy, Entisols are defined as soils that do not show any profile development other than an A horizon. An entisol has no diagnostic horizons, and most are basically unaltered from their parent material, which can be unconsolidated sediment or rock. Entisols are the second most abundant soil order (after Inceptisols), occupying about 16% of the global ice-free land area.

In Australia, most Entisols are known as rudosols or tenosols. In the World Reference Base for Soil Resources (WRB), because of the diversity of their properties, suborders of Entisols form individual Reference Soil Groups: Psamments correlate with Arenosols and Fluvents with Fluvisols. Many Orthents belong to Regosols or Leptosols. Most Wassents and aquic subgroups of other suborders belong to the Gleysols.[1]

Causes of delayed or absent development[edit]

Suborders[edit]

  • Aquents – permanently or usually wet soils formed on river banks, tidal mudflats etc. Here, general wetness limits development.
  • Fluvents – alluvial soils where development is prevented by repeated deposition of sediment in periodic floods. Found in valleys and deltas of rivers, especially those with high sediment load.
  • Orthents – shallow or "skeletal soils". Found on recent erosional surfaces or very old landforms completely devoid of weatherable minerals.
  • Psamments – Entisols that are sandy in all layers where development is precluded by the impossibility of weathering the sand. Formed from shifting or glacial sand dunes.
  • Wassents – Entisols that have a positive water potential at the soil surface for more than 21 hours of each day in all years.

Paleopedology[edit]

Most fossil soils before the development of terrestrial vegetation in the Silurian are Entisols, showing no distinct soil horizons. Entisols have been abundant in the paleopedological record ever since then, though, unlike other soil orders (Oxisols, Ultisols, Gelisols for instance) they do not have value as indicators of climate – though orthents might in some cases be indicated of an extremely old landscape with very little soil formation (as in Australia today).

See also[edit]

References[edit]

  • "Entisols". USDA-NRCS. Archived from the original on May 9, 2006. Retrieved 2006-05-14. Cite uses deprecated parameter |deadurl= (help)
  • "Entisols". University of Florida. Archived from the original on September 18, 2004. Retrieved 2006-05-14. Cite uses deprecated parameter |deadurl= (help)
  • "Entisols". University of Idaho. Archived from the original on 2006-09-01. Retrieved 2006-05-14. Cite uses deprecated parameter |dead-url= (help)
  1. ^ IUSS Working Group WRB (2015). "World Reference Base for Soil Resources 2014, Update 2015" (PDF). World Soil Resources Reports 106, FAO, Rome.