Earth:Luvisol

From HandWiki

Template:FOR

Luvisol
ISRIC monolith NL-001.jpg
Luvisol from the Netherlands
Used inWRB, other
WRB codeLV
ProfileAhEBtC
ClimateHumid temperate climate

Luvisols are a group of soils, comprising one of the 32 Reference Soil Groups in the international system of soil classification, the World Reference Base for Soil Resources (WRB).[1] They are widespread, especially in temperate climates, and are generally fertile. Luvisols are widely used for agriculture.[2]

Distribution

Global distribution

Luvisols cover 500–600 million ha of land area, mainly in the temperate zones. They form on a wide variety of mineral parent materials. In Mediterranean regions, the formation of hematite can produce red-coloured Chromic Luvisols.[2]

Description and formation

The main characteristic of Luvisols is an argic horizon, a subsurface zone with higher clay content than the material above it.[1] This typically arises as clay is washed downward by water and accumulates at greater depth. The clay minerals have not been extensively weathered and are therefore of the high-activity, 2:1 type, giving these soils high cation exchange capacities and high base saturation.[1][2] In uneroded landscapes, a lighter, clay-depleted eluvial horizon occurs above the argic horizon.[2]

In other classification systems

The Canadian system of soil classification includes Luvisols. In the USDA Soil Taxonomy, Luvisols are typically classified as Alfisols.[2]

References

  1. 1.0 1.1 1.2 IUSS Working Group WRB (2022). "World Reference Base for Soil Resources, fourth edition". International Union of Soil Sciences, Vienna. https://wrb.isric.org/files/WRB_fourth_edition_2022-12-18.pdf. 
  2. 2.0 2.1 2.2 2.3 2.4 Zech, Wolfgang; Schad, Peter; Hintermeier-Erhard, Gerd (2014) (in German). Böden der Welt (2nd ed.). Berlin: Springer Spektrum. 

Further reading

  • W. Zech, P. Schad, G. Hintermaier-Erhard: Soils of the World. Springer, Berlin 2022, Chapter 4.3.2. ISBN:978-3-540-30460-9

External links