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World’s Soil Resources

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KASTANOZEMS (Ustolls and Xerolls)<br />

Kastanozems are humus-rich soils that were originally covered with early-maturing native grassland<br />

vegetation which produced a characteristic brown topsoil 20-40 cm thick in which the organic matter<br />

content ranges between 2 and 6 percent. Kastanozems have a brown topsoil with a granular or fine blocky<br />

structure. The rest of the profile is lighter in colour and is characterized by the secondary accumulation of<br />

calcite (Figure A 19). Kastanozems are chemically rich soils with a pH slightly above neutral. Near the surface,<br />

soil pH may reach a value of 8.0.<br />

These soils are found in relatively dry climatic zones (annual precipitation 200–400 mm). Kastanozems<br />

are mostly used for irrigated farming and grazing. Kastanozems have relatively high levels of available calcium<br />

ions and other nutrients. Carbonates weakly move down in the soil profile with percolating water to form<br />

layers of secondary carbonates; gypsum is also common in these soils. Kastanozems form in semi-arid regions<br />

under relatively sparse grasses and shrubs.<br />

The total extent of Kastanozems is estimated to be about 465 million ha. Major areas are in the Eurasian<br />

short-grass steppe belt (southern Ukraine, the south of the Russian Federation, Kazakhstan and Mongolia),<br />

in the Great Plains of the United States of America, in Mexico, and in the southwestern pampas and Chaco<br />

regions of Argentina, in Paraguay and southeastern Bolivia (FAO, 2014).<br />

The main obstacle to the agricultural use of these potentially rich soils is drought (Encyclopaedia of <strong>Soil</strong><br />

Science, 2008). Irrigation, which brings the threat of secondary salinization, is nearly always necessary to<br />

obtain high yields. Another serious problem on Kastanozems is overgrazing (Wang and Batkhishig, 2014),<br />

extensive grazing being another important use for these soils. Overgrazing on light-textured soils often<br />

produces deflation, destroying the topsoil.<br />

Status of the <strong>World’s</strong> <strong>Soil</strong> <strong>Resources</strong> | Main Report Annex | <strong>Soil</strong> groups, characteristics,<br />

563<br />

distribution and ecosystem services

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