衡水浅层地下水水化学特征及利用前景

Zhou Xiaoni, Liushaoyu, Miao Zhuang, Hanbin, Wangzhe, Houxinwei, Song Ling
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引用次数: 0

摘要

本文在阐述衡水地区水文地质背景的基础上,根据样品资料,采用Shoka Lev和SuLin等分类方法对浅层咸水的化学特征进行了说明。通过聚类分析、因子分析、水文地球化学参数和地质解释等方法探讨了其成因机制。结果表明:研究区水化学类型及其成因较为复杂;浅层含盐地下水是陆地盐度影响、海水入侵影响和人为影响三种类型的结果。本文对利用浅层地下水的发展和技术方法进行了展望,并通过样品试验绘制了盐淡水比等高线图。它可以指导农业生产,具有重要的现实意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The Hydro-chemical Feature and Prospect on Utilisation of Shallow Groundwater in Hengshui
On the base of expatiation the background of hydrogeology in Hengshui area, the chemical character of the shallow salt water is explained by the classification methods such as Shoka Lev and SuLin according to the data of samples in the paper. We have discussed the genesis mechanism by using cluster analysis, factor analysis, hydro-geochemical parameters and geologic interpretation. It reaches conclusions that the types of water chemistry and its causes are complex in the research area; the shallow salt groundwater is the results of three types: affection of mainland salinity, seawater intrusion and human affection. The paper a view of the development and technical methods of utilizing shallow groundwater and make the contour map of the ratio between salt and fresh water with the test of samples. It can guide the agricultural production and has important practical significance.
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