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Changes in the Ameliorative Status of Irrigated Soils of Volgograd Oblast in the 21st Century

机译:21世纪伏尔加格勒州灌溉土壤改善地位的变化

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The ameliorative status of irrigated soils was estimated on the basis of reclamation cadaster data for 2001 and 2016 on 17 state irrigation systems in three nature regions of Volgograd oblast: (1) the Khvalyn clayey plain and Volga sand ridge in the Caspian Lowland, (2) the Volga and Ergeni uplands, and (3) the Volga and Don river valleys. Significant changes took place in the ameliorative status of these systems during the studied period: the total irrigation area sharply decreased (-31%), especially under irrigation by the local runoff (44.5%); the groundwater level became lower, and the area with deep (>5 m) groundwater table increased to 77.3%; and the areas of saline and solonetzic soils decreased by 22.9% and 19.3%, respectively. In many cases, the differences in natural conditions determined the ameliorative status of irrigated soils and the intensity of their changes. The changes were the greatest on the initially saline slightly drained soils of the Khvalyn clayey plain and the smallest in the Volga River valley. During the entire period of irrigation, some areas were subjected to secondary salinization and abandoned. Our investigations at the Raigorodsk plot of the Svetloyarsk irrigation system within the Khvalyn clayey plain in 2016 demonstrated that the soils subjected to secondary salinization in the period of maximum irrigation intensity (in 1990) are now at the stage of gradual desalinization.
机译:灌溉土壤的改善地位是根据伏尔加格勒州三个自然地区的17个国家灌溉系统的2001年和2016年的填海机构数据估计:(1)Caspian Lowland的Khvalyn Clayey Plane和Volga Sand Ridge(2 )Volga和Ergeni Uplands,以及(3)伏尔加和唐河谷。在研究期间,这些系统的改进状态发生了重大变化:灌溉面积大幅下降(-31%),特别是当地径流(44.5%)灌溉;地下水位变低,深(> 5米)地下水位的区域增加到77.3%;和盐水和溶菌土壤的区域分别下降了22.9%和19.3%。在许多情况下,自然条件的差异确定了灌溉土壤的改善状态以及其变化的强度。最初盐水的变化是最初的盐水略有排水的龙杨克莱y平原和伏尔加河谷最小的土壤。在整个灌溉期间,一些地区遭受二次盐渍化并被遗弃。我们2016年Khvalyn Clayey Plane的Svetloyarsk灌溉系统Raigorodsk策略的调查表明,在最大灌溉强度(1990年)的次级盐渍化中进行的土壤现在处于逐步脱盐的阶段。

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