摘要
本文通过对多年来积累的水文物探资料的初步分析研究，发现含水层的电性特征与地下水矿化度之间存在着幂函数的变化规律，其相关关系式为Ｍｓ＝３５．９３５３ρｓ－１．１４１６和ＭＪ＝３３．５８９２ρｓ－１．０４９６，这在近年来寻找地下淡水体方面发挥了重要作用，并取得了良好的社会效益和经济效益。
Through the preliminary analysis and study of
hydrological geophysical data through the years, a variation rule of power function was found to
exist between the electric property of the aquifer and the mineralization degree of groundwater,
with the correlation formula of M s=35 9353ρ s -1 1416 and M J=33 5892ρ s -1 0496
. This has played important role in the searching for underground fresh water masses and
obtained good social and economic effects.
出处
《水文地质工程地质》
CAS
CSCD
1998年第6期54-58,共5页
Hydrogeology & Engineering Geology
