Stagnosol

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A Stagnosol in the

mottled in the topsoil and subsoil, with or without concretions and/or bleaching. The topsoil can also be completely bleached (albic horizon). A common name in many national classification systems for most Stagnosols is pseudogley. In the USDA soil taxonomy
, many of them belong to the Aqualfs, Aquults, Aquents, Aquepts and Aquolls.

They are developed in a wide variety of unconsolidated materials like

alluvial and colluvial deposits and physically weathered siltstone. Stagnosols occur on flat to gently sloping land in cool temperate to subtropical regions with humid
to perhumid climate conditions.

The

fertile soils
owing to their moderate degree of leaching.

Stagnosols cover 150–200 million ha worldwide. For the greater part in humid to perhumid temperate regions of

Planosols
. with a light-coloured,
permeable subsoil with significantly more clay than the surface horizon. In the US Soil Classification of 1938 used the name Planosols, whereas its successor, the USDA soil taxonomy
, includes most Planosols in the Great Groups Albaqualfs, Albaquults and Argialbolls.

See also

References

  • IUSS Working Group WRB: World Reference Base for Soil Resources, fourth edition. International Union of Soil Sciences, Vienna 2022. ).

Further reading

External links