E3S Web Conf.
Volume 98, 201916th International Symposium on Water-Rock Interaction (WRI-16) and 13th International Symposium on Applied Isotope Geochemistry (1st IAGC International Conference)
|Number of page(s)||5|
|Section||Geological Evolution of Water-Rock System: Mechanisms, Processes, Factors, Stages. The Session Dedicated to Stepan Shvartsev’s Memory|
|Published online||07 June 2019|
Recharge of natural mineral water Jingyu County, northeastern China
Key Laboratory of Groundwater Resources and Environment, Ministry of Education, Jilin University, No 2519, Jiefang Road, Changchun 130021, PR China ;
2 Changbai Mountain Natural Mineral Water Research Center, Baishan, Jilin, 135200, PR China
* Corresponding author: email@example.com
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.
© The Authors, published by EDP Sciences, 2019
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