| 汤兜地区水文地球化学特征及成因分析 |
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| 引用本文： | 黄奇波,汪玉松,刘秀明.汤兜地区水文地球化学特征及成因分析[J].地下水,2008,30(6):6-8. |
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| 作者姓名： | 黄奇波 汪玉松 刘秀明 |
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| 作者单位： | 1. 中国地质大学(武汉)环境学院,湖北,武汉,430074
2. 江西省煤田地质局二二六地质队,江西,萍乡,337054 |
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| 摘 要： | 根据汤兜地区水样化学成分分析资料，分析了区内水的水化学特征。用比例系数分析法得出汤兜地下热水不是海相沉积水，热水起源于大气降水，地下热水在径流过程中与围岩进行了充分的水文地球化学反应，获得了围岩中的矿物组分，导致其各种离子组分含量增加。用因子分析法得出地下水的化学组分主要由长石、黄铁矿、碳酸盐风化溶解所形成。
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| 关 键 词： | 水化学成分 比例系数法 因子分析 |
Hydro-geochemical Characteristics and Formation Reason of Water in Tangdou Region |
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| HUANG Qi-bo,WANG Yu-song,LIU Xiu-ming.Hydro-geochemical Characteristics and Formation Reason of Water in Tangdou Region[J].Groundwater,2008,30(6):6-8. |
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| Authors: | HUANG Qi-bo WANG Yu-song LIU Xiu-ming |
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| Institution: | HUANG Qi-bo,WANG Yu-song,LIU Xiu-ming (School of Environmental Studies,China University of Geosciences,Wuhan 430074,Hubei) |
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| Abstract: | According to the chemical composition of water in Tang dou region,this paper analyzes the water chemical characteristics.The article found that the underground hot water in Tangdou area is not marine sediments water by the analyzed method of proportionality coefficient.The hot water originated from precipitation.In the course of runoff,the hot groundwater has a full hydro-geochemical reaction with its around rock,got the mineral components of the around rock,which result in various component increasing.Usin... |
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| Keywords: | Chemical composition of water the proportionality coefficient method factor analysis |
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