Problems of desertification in the eastern zone of the Rostov region

Valentina Kumacheva, Nelly Mazur
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Abstract

The article presents an analysis of the dynamics of soil fertility, trace elements, pH, aridity index and normalized index. Salt lakes in the complex from 30-50 % occupy 68.3 thousand hectares. The humus content in the arable layer is low. There is a decrease in the content of humus (from 2.2% to 1.7%) and phosphorus (from 18.6 mg/kg to 18.2 mg). The content of exchangeable potassium is generally within the optimal range. The processes of loss of humus and nutrients in the soils of the area are a manifestation of the desertification process. The content of sulfur and trace elements (copper, zinc, manganese, cobalt) is low, insufficient for grain crops. The soils of the district are slightly alkaline (pH – 8.1). The aridity index of the Zavetinsky district is 0.41, and the normalized index is 0.59. According to the normalized aridity index – 0.59, the territory of the Zavetinsky district belongs to the moderately arid (NIA =0.5—0.6). Keywords: DESERTIFICATION, SALT LAKES, ARIDITY INDEX, SOIL FERTILITY, TRACE ELEMENTS
罗斯托夫州东部地区的荒漠化问题
文章对土壤肥力、微量元素、pH 值、干旱指数和归一化指数的动态进行了分析。复合盐湖面积从 30-50% 到 68.3 千公顷。耕作层腐殖质含量较低。腐殖质含量(从 2.2% 降至 1.7%)和磷含量(从 18.6 毫克/千克降至 18.2 毫克)均有所下降。可交换钾的含量一般在最佳范围内。该地区土壤中腐殖质和养分的流失过程是荒漠化过程的一种表现。硫和微量元素(铜、锌、锰、钴)含量较低,不足以种植粮食作物。该地区的土壤呈弱碱性(pH 值 - 8.1)。扎韦廷斯基区的干旱指数为 0.41,标准化指数为 0.59。根据归一化干旱指数 - 0.59,扎韦廷斯基区属于中度干旱区(NIA =0.5-0.6)。关键词荒漠化、盐湖、干旱指数、土壤肥力、微量元素
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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