Phaeozem
Appearance


Dominant (more than 50% of soil cover)
Codominant (25-50%)
Associated (5-25%)
A Phaeozem in the
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
- Pedogenesis
- Pedology
- Soil classification
References
- IUSS Working Group WRB: World Reference Base for Soil Resources, fourth edition. International Union of Soil Sciences, Vienna 2022. ISBN 979-8-9862451-1-9 ([1]).
- ^ Delvaux, B.; Brahy, V. "Mineral Soils conditioned by a Wet (Sub)Tropical Climate". FAO. Retrieved 14 June 2014.
- ^ "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. ISBN 978-3-540-30460-9
External links
- profile photos (with classification) WRB homepage
- profile photos (with classification) IUSS World of Soils