摘要
山西寿阳县矿泉水田位于娘子关泉群岩溶水系统西北部补给径流区。受多期构造影响,使该处奥灰岩溶深埋,而其深部地下水交替却较为积极,使补给区游离CO2随大气降水进入岩石裂隙,溶解奥灰岩中的菱锶矿,形成了超深水位岩溶矿泉水田。该处矿泉水具有高锶、低钠特征和优势,且含有锶、锌、钼、偏硅酸等有益于人体健康的元素或组分,有较好的开发前景。
Mineral water field of Shouyang county in Shanxi province located in recharge and watershed area of northwestern Karst water system in spring complex of Niangziguan. Because of multi- stages of structural influence, make the Karst of Ordovician limestone deep buried, but the deep ground water alternated much actively, and make the free CO2 of recharge area enter to fractures of rock along with atmospheric water, and dissolved strontianite of Ordovician limestone, and formed Karst mineral water field at overdeep water level. The mineral water at here has property and superiority of higher strontium and lower sodium, and contains elements or components which benefit to the health of human body, such as strontium? zinc? molybdenum and metasilicic acid etc., so there are better exploitation prospect.
出处
《中国煤田地质》
2002年第3期26-27,共2页
Coal Geology of China
关键词
山西
寿阳县
矿泉水田
深部岩溶
超深水位
利用
开发
mineral water field
Karst in deep
overdeep water level
utilization and exploitation
Shouyang of Shanxi Province