盐对哈萨克斯坦南部以棉花为基础的灌溉农业土壤有影响

S. Tanirbergenov, E. Saljnikov, B. Suleimenov, A. Saparov, Dragan Čakmak
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引用次数: 1

摘要

对哈萨克斯坦某棉田灌溉土壤的土壤盐分进行了研究,旨在为全区集排水系统的重建和防止土壤退化提供依据。利用2012-2014年的试验数据绘制了土壤盐度(1:10000)的季节性和垂直分布图。2014年春季0 ~ 20 cm层中盐渍土面积由79.5%下降到57.7%;弱盐渍土面积由20.5%增加到34.6%。秋冬两季,强盐渍土面积由25.6%下降至14.1%。非盐碱地面积为7.7%。在温度梯度和地下水位的驱动下,盐类沿土壤剖面运移,在春季由上而下,在秋季和冬季由下而上相反,在垂直方向和季节上均发生变化。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Salt affected soils under cotton-based irrigation agriculture in southern Kazakhstan
Soil salinity of the irrigated soils in a cotton farm of Kazakhstan was studied aimed to provide background for reconstruction of collection-drainage system of whole region and preventing soil deterioration. The experimental data obtained for 2012-2014 were plotted for the development of the map of soil salinity (1:10000) seasonally and vertically. In spring 2014 the area under medium saline soil in 0-20 cm layer decreased from 79.5 to 57.7%; the area of weakly saline soils increased from 20.5 to 34.6%. In autumn and winter periods the area of strongly saline soils decreased from 25.6 to 14.1%. The area of non-saline soils was 7.7%. The changes in the ions amount, both vertically and seasonally, occur with transport of salts along soil profile driven by temperature gradients and the level of ground water, i.e., in spring from up to down, and in autumn and winter, contrary from down to up.
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