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水文地质工作中,地下水的化学分类通常采用舒卡列夫、布罗茨基、阿廖金等分类。另外还有各种图解法,如三角形坐标图解法。它们大多是利用主要阴、阳离子间的对比关系进行划分的。其优点是简便易行,基本上可反映地下水的形成过程,并为广大水文地质工作者所熟悉。但在水文地质普查中,特別是在基岩山区,地下水径流交替强烈,水化学成分差别不大,上述分类尚欠精细。水质评价以及其他一些水文地质问題,如泉水的归属,河谷第四系中的泉水补给
In hydrogeological work, the chemical classification of groundwater is usually based on the classification of Shkar-Lev, Brodsky, Alejgin. In addition there are a variety of graphic method, such as the triangle coordinate graph solution. Most of them are the use of the main anion, the contrast between the classification. Its advantages are simple and easy, basically reflect the formation of groundwater, and familiar to the majority of hydrogeologists. However, in the hydrogeological survey, especially in bedrock mountainous areas, groundwater runoff alternates intensely with little difference in the chemical composition of water, and the above classification is still not meticulous. Water quality assessment and other hydrogeological issues such as the ownership of spring water, spring recharge in Quaternary