摘要
本文描述了在碳酸盐岩分布的水文地质系统内,怎样利用水质相对,绝对含量,运用化学热力学、化学动力学和水动力学的理论及方法,进行半定量或定量的确定研究区某些水文地质信息,具有重要的理论和实际意义。 文章就系统水文地球化学类型分带模型和成因;系绕水化学分带溶蚀特征的定量评价;以及定量评价水文地质条件的化学动力学法等三个方面展开讨论。理论和计算在山东、河北、山西等省区某些水文地层系统中运用时,获得与实际水文地质特点相吻合的效果。
The paper describes a method which makes use of absolute or relative carbonate content of water in combination with the theory of chemical thermodynamics, chemical kinetics and water dynamics to obtain semi-quantitatively or quantitatively useful hydrogeologic informatioan in a carbonate region. Application of the method indicates its theoretical and practical significance.The following are discussed in the paper:1. Hydrochemistry zonation model and cause of its formation.2. Quantitative evaluation of dissolution properties in different zones of a system.3. Chemical kinetics method for determinations of hydrogeologic parameters.Application in Shandong, Hebei and Shanxi provinces shows the method effective. The parameters calculatcd by the method is identical to the actual hydrogeologic conditions.
出处
《水文地质工程地质》
CAS
CSCD
北大核心
1993年第4期35-40,共6页
Hydrogeology & Engineering Geology
基金
自然科学基金和地质行业基金联合资助项目
