人为和自然因素影响下乌克兰地表水和地下水地带性水化学成分的变质作用

M. Romashchenko, S. S. Kolomiyets', A. Sardak
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引用次数: 0

摘要

提出了一种通过定量评价人为因素(排水复垦)或自然因素(气候)对地表水和地下水水化学组成变化的综合功能诊断方法。该方法基于地表和地下水水化学成分的自然纬向和垂向分带,作为土壤圈土工膜性质的体现。定量评价施泰尔河和伊尔平河流域排水填海面积增加对流域影响的阶段是对1947-1989年截流线上各宏观成分含量的时间序列进行线性回归分析,以及填海面积增加的动态和相关性分析。为了增加相关性的紧密性,水化学成分以%-等效形式表示,这最准确地表征了宏观成分的比例,但不依赖于水的总矿化。随着流域面积的增加,烃类和钙等标型离子含量降低,其他宏观组分和矿化含量增加,具有统计学意义。一般来说,随着排水复垦面积的增加,河水的水化学成分也会干旱化。根据О.О分类的河流水化学类型的变化。Alekina。所获得的水化学成分大组分含量的时间趋势参数模型,可以确定两江流域围垦的极限面积,并预测水的水化学类型在干旱化方向上的变化。停止新的围垦系统的建设,降低干旱地的农业利用效率,使河流的水化学成分朝着围垦发展的方向恢复。对Prykarpattia和西布格河流域及其支流的5个复垦系统进行了功能诊断方法的验证,证明了该方法的高效率,为建立自然和人为因素对水资源化学成分和水质影响的参数化模型提供了前景。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Metamorphization of zonal hydrochemical composition of surface and groundwater of Ukraine under the influence of anthropogenic and natural factors
An integrated method of functional diagnostics of basin geosystems through quantitative assessment of anthropogenic (drainage reclamation) or natural factors (climate) on the change of hydrochemical composition of surface and groundwater is presented. The method is based on the natural latitudinal and vertical zonation of the hydrochemical composition of surface and groundwater, as a manifestation of the geomembrane properties of the pedosphere. The stages of the quantitative assessment of the impact of increasing drainage reclamation areas in the Styr and Irpin river basins, were a linear regression analysis of chronological series of the content of each of the macrocomponents of the river water composition in the closing line for 1947-1989, and also the dynamics of increasing reclamation areas and correlation analysis of the obtained dependencies. To increase the closeness of the correlation, the hydrochemical composition was presented in %-equivalent form, which most accurately characterizes the ratio of macrocomponents, but does not depend on the total mineralization of water. A decrease in the content of such typomorphic ions as hydrocarbons and calcium and an increase in the content of other macrocomponents and mineralization were found statistically significantly with increasing drainage areas. In general, with increasing areas of drainage reclamation, there is an aridization of the hydrochemical composition of river water. The change of hydrochemical type of river water according to the classification of О.О. Alekina. The obtained parametric models of time trends of the content of macrocomponents of hydrochemical composition allowed to determine the limiting area of reclamation of the basins of two rivers and to predict changes in the hydrochemical type of water in the direction of its aridization. Stopping the construction of new reclamation systems and reducing the efficiency of agricultural use of drained lands leads to the restoration of the hydrochemical composition of rivers in the direction of their reclamation development. Approbation of the created method of functional diagnostics was carried out on five reclamation systems of Prykarpattia and in the basin of the Western Bug river and its branches proved its high efficiency and perspective for the creation of parametric models of the influence of natural and anthropogenic factors on chemical composition and quality of water resources.
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