摘要
和村—孙庄盆地锶矿泉水属低钠低矿化度含锶重碳酸钙镁型中性低温矿泉水。通过对盆地构造、岩溶发育、地下水动态等特征的分析与研究认为,奥陶系中统峰峰组二、三段岩溶裂隙含水层为盆地内的主要富锶矿泉水地层,锶元素来源于碳酸盐和岩浆岩,矿泉水中氚浓度(33.86±3.44TU)含量表明,该矿泉水形成年龄为10～20a,具有远源补给、深层循环特征。
The strontium contained mineral water in Hecun-Sunzhuang Basin belongs to low sodium, low degree of mineralization strontium contained calcium and magnesium bicarbonate type neutral low temperature mineral water. After basin structural, karstic development and groundwater regime characteristic analyses figured out the main strontium contained mineral water aquifer is Middle Ordovlcian Fengfeng Formation members Ⅱ and Ⅲ karstic fractured aquifer, the element strontium is come from carbonate and igneous rocks, the tritium concentration in the mineral water （33.86±3.44TU） indicated that the mineral water formed age is 10-20a, and provided with characteristics of long distance recharging and deep circulation.
出处
《中国煤炭地质》
2008年第2期24-26,共3页
Coal Geology of China
关键词
锶矿泉水
赋存特征
岩溶裂隙含水层
峰峰组二、三段
和村-孙庄盆地
strontium contained mineral water
hosting character
karstic fractured aquifer
Fengfeng Formation members Ⅱ and Ⅲ
Hecun-Sunzhuang Basin
