自然因素对伏尔加河三角洲初淹土壤盐渍化的影响

M. Valov, A. Barmin, D. Belyaev, Alexander V. Sintsov, Ekaterina V. Lipezina
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引用次数: 0

摘要

土壤退化的常见类型之一是土壤盐渍化,是严重限制粮食安全和领土可持续发展的因素。干旱区土壤的第一次盐渍化需要特别关注,因为干旱气候导致上层根系土壤层盐的活跃积累,并导致大面积土地从经济周转量中撤出。研究了自然因素影响下伏尔加河三角洲上游自然边界土壤中水溶性盐的特征。植物自然保护区“Svinoroiny草甸(Meshkovsky)”被选为研究对象,与伏尔加河三角洲贝尔丘陵景观分布内的新里海沿岸平原相关联。1979年至2020年对该地区进行了水提物离子分析和土壤溶液毒性计算。结果表明,在区域溢水状态下,盐化类型的动力学方向是由水优势上升比下降所决定的。盐渍化的增加在很大程度上取决于春夏洪水的大容量和适当的地下水位上升,区域脱盐是由大气降水量决定的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Natural factors influence on first rarely flooded soil salination of the river Volga delta
Soil degradation is one of the common types of which is soil salination, is a serious limited factor of food security and sustainable territory development. It is necessary to pay a special attention on the first soil salination of arid regions, as arid climate leads to the active salt accumulation in the upper rooting soil horizons and gives rise to withdrawal of large land areas from economic turnover. The purpose of the this work is defining of the watersoluble salts specific features in soils of the river Volga delta upper level natural boundaries under the influence of natural factors. Botanic natural sanctuary “Svinoroiny meadow (Meshkovsky)” was chosen as a research object, associated with the new Caspian coastal plain within distribution of the river Volga delta Baer knoll landscape. Water extract ions analysis and soil solution toxicity calculation on the area were carried out from 1979 till 2020. It was revealed that dynamics direction of salination types are defined by the ascent of water predominanceon over descending on the area in the conditions of the territory exudative water regime. Salination increase to a great extent depends on the great volumes of spring-summer floods and appropriate ground water level rise, area desalination is defined by atmospheric precipitations quantity.
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