Main types of soil degradation in the Kura-Aras Lowland of Azerbaijan

被引:9
作者
Babaev, M. P. [1 ]
Gurbanov, E. A. [1 ]
Ramazanova, F. M. [1 ]
机构
[1] Natl Acad Sci Azerbaijan, Inst Soil Sci & Agr Chem, Baku 1073, Azerbaijan
关键词
irrigation-induced erosion; wind erosion; salinization; slope of the surface; degree of erosion; sierozems (Calcisols); meadow-sierozemic soils (Gleyic Calcisols); light gray-cinnamonic soils (Haplic Kastanozems); EROSION RESISTANCE; IRRIGATED SOILS; RUSSIA;
D O I
10.1134/S106422931504002X
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
The main types of soil degradation in the Kura-Aras Lowland are irrigation-induced erosion, natural water and wind erosion, and salinization. Among 2098.8 thousand ha of agricultural land in the lowland, the areas of lands subjected to erosion and salinization reach 333.6 and 373.4 thousand ha, respectively. The dependence of irrigation-induced erosion on the soil type (sierozems, meadow sierozems, and gray-cinnamonic soils), the inclination of the irrigation furrows, the irrigation water salinity (0.15-0.95 g/L), and the water discharge (0.8-1.4 L/s) was studied. It was found that soil erosion and salinization result in changes in the soil bulk density and porosity and in a decreasing content of humus and nutrients. Certain changes take place in the soil texture. The land areas subjected to rainstorm erosion of strong, moderate, and low degrees are estimated at 57.7, 24.4, and 15.3 thousand ha, respectively. Measures to control soil erosion and salinization are discussed.
引用
收藏
页码:445 / 456
页数:12
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