鞑靼斯坦共和国境内的河水硬度变化。

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摘要

衡量河流水质的主要标准之一是综合硬度,综合硬度的大小决定了其在国民经济各部门的适用性。关于鞑靼斯坦共和国河水总体硬度大小的多年资料是分析其时间和空间变化的基础。作为一个整体指标,选择了总硬度的年平均值,其在共和国全境的分布情况清楚地反映在给定的骨架图中。对20世纪和21世纪观测到的河流总硬度的对比分析表明,其值仍然处于中等、中等硬度和硬水的范围内,但这些值在空间上有再分布。由于刚性的形成在很大程度上取决于领土的局部特征,首先取决于盆地地质结构的异质性,因此对其变化的分析与鞑靼斯坦共和国三个大地理区域——前伏尔加、前卡马和扎卡米耶的地质结构相适应。硬度的形成也受人为因素的影响。在鞑靼斯坦共和国境内建立的大型水库影响区内,地下水水位上升,不仅改变了共和国地下水体供应的性质,而且改变了河水的质量。共和国东南部的总体硬度的重新分配与石油企业的活动有关,这些企业对天然水的水/化学成分进行了重大调整。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
River waters hardness variations on the territory of the republic of Tatarstan.
One of the main criteria for river water quality is overall hardness, the value of which determines its suitability for use in various sectors of the national economy.Availability of the many-year information about the magnitude of the overall hardness of the river waters of the Republic of Tatarstan served as the basis for analyzing its changes in time and space. As an integral indicator, the average annual value of the overall hardness is chosen, the distribution of which throughout the territory of the Republic is clearly reflected in the given skeleton maps. A comparative analysis of the total hardness of river waters, observed in the XX and XXI centuries, showed that its value remained within the category of moderate, medium hardness and hard waters, but there was a redistribution of these values in space. Since the formation of rigidity largely depends on local features of the territory and, first of all, on the heterogeneity of the geological structure of the basin, the analysis of its changes was made commensurate with the geological structure of the three large geographical regions of the Republic of Tatarstan − Pre-Volga, Pre-Kama and Zakamye.The formation of hardness is also influenced by the anthropogenic factor. In the zone of influence of large reservoirs, created in the territory of the Republic of Tatarstan, a rise in the level of groundwater is observed, changing not only the nature of the underground supply of water bodies of the Republic, but also the quality of river water. The redistribution of general hardness in the south-east of the republic is connected with the activities of oil enterprises, which make significant adjustments to the hydro/chemical composition of natural waters.
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