From Latin acris meaning sour, very acid, indicative of a low base saturation of the cation exchange capacity at pH 7.0.
Definition
Soils having
- 1.
an argic horizon, which has a cation exchange capacity (in 1 M NH 4OAc at pH 7.0) of less than 24 cmol c kg −1 clay in some part, either starting within 100 cm from the soil surface, or within 200 cm from the soil surface if the argic horizon is overlain by loamy sand or coarser textures throughout, and
- 2.
a base saturation of less than 50% (in 1 M NH 4OAc at pH 7.0) in the major part between 25 and 100 cm.
General characteristics
Soils characterized by the presence of a well‐defined B horizon, with a blocky, prismatic, granular or massive structure (depending on water content, amount of Fe sesquioxides, and mineralogy of the fine fraction), which has a markedly increase in clay content (argic horizon) relative to the overlying horizons, and a cation exchange complex in which acidic cations (ionic Al species and, to a lesser extent, H +,...
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Bibliography
FAO, 2001. Lecture notes on the major soils of the world. World Soil Resources Reports, 94. Rome: Food and Agriculture Organization of the United Nations. 334 pp.
IUSS Working Group WRB, 2006. World reference base for soil resources 2006. World Soil Resources Reports No. 103. Rome: FAO.
Pédro, G., 1983. Structuring of some basic pedological processes. Geoderma, 31: 289–299.
Zech, W., and Hintermaier‐Erhard, G., 2007. Soils of the World. Heidelberg, Berlin: Springer‐Verlag, 130 pp.
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Dahlgren, R.A., Macías, F., Arbestain, M.C., Chesworth, W., Robarge, W.P., Macías, F. (2008). Acrisols. In: Chesworth, W. (eds) Encyclopedia of Soil Science. Encyclopedia of Earth Sciences Series. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-3995-9_11
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DOI: https://doi.org/10.1007/978-1-4020-3995-9_11
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