摘要
东亢矿泉水处于临汾断陷盆地边缘山前地带。矿泉水赋存于石炭系、奥陶系及侵入岩体的裂隙中。单井涌水量达71.4m ̄3/h,水位埋深51.09m。矿泉水中锌、锶、偏硅酸分别为0.289mg/L,1.28mg/L,33.28mg/L,属锌锶偏硅酸-重碳酸·硫酸-钠型优质矿泉水,具有良好的开发前景。
Dongkang mineral water is Located at the edge of Linfen faulted basins.It occurs in thefissures of between Carboniferous and Ordovician system and intrusive badies.Single wellyeild is up to 71.4m ̄3/h. Water table is 51.09 m below surface,The mineral water containsSr 1.28 mg/L,Zn 0.289 mg/L and metasilicate 33.28mg/L,which is accordant with the na-tional standard of potable natural mineral water,It is classified as Sr-Zn-bearing metasilicatebicarbonate Na sulphate type of top-quality mineral water,and has bright future of develop-ment.
关键词
锌-锶-偏硅酸
矿泉水
裂隙水
天然矿泉水
饮用
Zn-Sr-H_2SiO_3 natural mineral water,fissure water,Linfen faulted basin