摘要
利用矿泉水的水文地质、水化学特征、环境同位素水文地质学和国际WATCH水/岩平衡计算机程序等新理论、新方法,可以推算出雪峰矿泉水的形成年龄和补给与迳流条件,计算出水的循环深度,以及主要成分的迁移系数,从而有机地研究矿泉水的水文地球化学机制,探讨矿泉水形成的水文地球化学成因模式。
Through studying the hydrogeological and hydrochemical character, of mineral water and using the new theory of environmental isotope hydrogeology and a new method of the WATCH water/rock balance comput-er program, one may date the water and deduce its recharge and run—off condition. cycle depth and the migration coefficients of important components in water, It is by the new theory and new method that author has studied or-ganically the hydrogeochemical principle of mineral water in Zhijiang and has also discussed the genetic model of the hydrogeochemistry for the formation of the mineral water.
出处
《湖南地质》
1993年第4期257-261,230,共6页
Hunan Geology
关键词
矿泉水
水文学
地球化学
the hydrogeochemical principle
isotopic geology
water/rock balance
cycle depth