Author:
Liang Xiujuan,Tian Hui,Xiao Changlai,Li Mingqian,Sun Ying,Li Yinxi
Abstract
A light stable isotope investigation of the source of natural mineral water in Jingyu County indicates an origin predominantly from atmospheric precipitation. As water-rock interaction occurs in the runoff process, SiO2 in the basaltic aquifer is dissolved, forming a metasilicate-type mineral water. The average residence time of natural mineral water in the stratum is 20 to 56 years.
Cited by
1 articles.
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