Phaeozem

Source: Wikipedia, the free encyclopedia.
Luvic Phaeozem in Luqmuts, Ethiopia
Distribution of Phaenozem soils as defined by the World Reference Base for Soil Resources classification:
  Dominant (more than 50% of soil cover)
  Codominant (25-50%)
  Associated (5-25%)

A Phaeozem in the

Mollisols) of the USDA soil taxonomy.[1][2]

These soils are found mainly in humid and sub-humid tall-grass

glacial till and typically have organic matter contents of about 5% and a pH
of 5–7.

Intensive agricultural use is widespread and includes wheat, soybean and cotton production and improved pastures for cattle.

See also

References

  • IUSS Working Group WRB: World Reference Base for Soil Resources, fourth edition. International Union of Soil Sciences, Vienna 2022. ).
  1. ^ Delvaux, B.; Brahy, V. "Mineral Soils conditioned by a Wet (Sub)Tropical Climate". FAO. Retrieved 14 June 2014.
  2. ^ "Major Soils of the World. ISRIC Wageningen, The Netherlands, 2001" (PDF). Archived from the original (PDF) on 2016-03-04. Retrieved 2014-06-14.

Further reading

  • W. Zech, P. Schad, G. Hintermaier-Erhard: Soils of the World. Springer, Berlin 2022, Chapter 5.3.1.