欢迎访问《高校地质学报》官方网站,今天是
分享到:

J4

• 文章目录 • 上一篇    下一篇

地下水与玄武财反应趋势分析

艾瑶 高明 戴水汉   

  1. [1]华东交通大学土木工程系 [2]南京大学地球科学系
  • 收稿日期:1998-06-20 修回日期:1998-06-20 出版日期:1998-06-20 发布日期:1998-06-20

TENDENCY ANALYSIS OF THE INTERACTION BETWEEN GROUDW ATER AND BASALT

Ai Yao1, Gao Ming2, Dai Shui-han2   

  1. 1. Department of Civil Engineering, East China Jiao Tong University, Nanchang 330013, China; 2. Department of Earth Sciences, Nanjing University, Nanjing, 210093 China
  • Received:1998-06-20 Revised:1998-06-20 Online:1998-06-20 Published:1998-06-20

摘要: 通过建立水化学平衡反应模型,计算地下水组分的各种可能存在形式的浓度和活度,并求得各种矿的饱和指数,再用饱和指数分析水-岩相互作用过程中矿物的溶解与沉淀反应趋势。本文采用该方法对盱眙玄武岩土区水-岩间反应趋势进行了分析。

Abstract: A model of hydrochemical equilibrium reactions is proposed based on the principle of equilibrium of complex actions in the solution, and used to calculate the concentrations and activities of different mineral species in groundwater. The index of mineral saturations related to the groundwater are then determined. So the tendency of dissolution and precipitation of minerals in the hydrorock reactions can be studied. This method was applied to study the basalt in Xuyi county, Jiangsu province and discuss the reactions between groundwater and basalt.