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- W4236967647 abstract "Publisher SummarySoil is the product of the interactions among the five soil-forming factors: parent material (rock types), climate, vegetation, topography, and time. In the arid regions, the major factors affecting the chemical properties of soils are climate, topography, and time, with vegetation (which is heavily dependent upon climate) and parent material playing secondary roles. When the average annual precipitation in both the hot and the cold arid regions is less than 250 mm, soils generally have neutral to alkaline reactions and a base saturation of 90% or more, contain less than 2% organic matter, have a calcareous horizon within the top 2 m of soil, that is at least slightly saline, and have a clay mineral complex dominated by illite and montmorillonite. When annual precipitation exceeds 250 mm, differences appear that are related to the increased rainfall, variations in rainfall distribution patterns, position on slopes, and the age of soil. The development of certain horizons in arid-region soils is an indication of the nature of the chemical environment in those soils. Subsurface horizons are of particular interest, because they are influenced less than surface soils by transitory climatic events. The principal subsurface horizons representative of arid-region soils are calcic, petrocalcic, gypsic, petrogypsic, salic, and natric." @default.
- W4236967647 created "2022-05-12" @default.
- W4236967647 date "1976-01-01" @default.
- W4236967647 modified "2023-09-27" @default.
- W4236967647 title "Chapter 10 Chemical Properties" @default.
- W4236967647 doi "https://doi.org/10.1016/s0166-2481(08)70103-x" @default.
- W4236967647 hasPublicationYear "1976" @default.
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