摘要
含偏硅酸矿泉水在我国分布很广,是一种宝贵的矿产资源。本文根据水-岩相互作用过程中热力学平衡原理,研究六合、盱眙玄武岩地区含偏硅酸矿泉水形成的水文地球化学机理及其主要影响因素,从而提出了含偏硅酸矿泉水形成的水文地球化学模式。
The metasilicate mineral wager, widely disrtibuted in China, is a very valuable resource. On the basis of the ptinciple of thermodynamic balance during the process of water-rock interaction mechanism in the formation of metasilicic mineral water and main factors influencing it in basaltic arcas of Liuhe and Xuyi districts. A hydrogeochemical model of the formation of metasilicate mineral water is given in this paper.
出处
《水文地质工程地质》
CAS
CSCD
北大核心
1992年第3期39-41,共3页
Hydrogeology & Engineering Geology
基金
国家自然科学基金
