摘要
稷山仁和矿泉水赋存于第四系中更新统中细砂层中,含水层厚17m,富水性很强,单位涌水量可达40.29m ̄3/h·m,水位埋深142m。该矿泉水含锶达2.278mg/L偏硅酸39.0mg/L,锂的含量也高达0.15mg/L以上。矿化度超过1000mg/L,水温达37~38℃。经山西省矿产储量委员会审定为含锶、偏硅酸的重碳酸硫酸钠型饮用及医用矿泉水。
Renhe mineral water occurs in the fine-grained sandstone of Middle Pleistocene of Qua-ternary system. The aquifer is 17 m thick with abundant water contained. Specific yeild is upto 40.29 m ̄3/h· m. Water table is 142 m below surface,This kind of mineral water containsSr 2.278 mg/L, metasilicate 39 mg/L and Li more than 0.15 mg/L. The degree of mineral-ization is more than 1000 mg/L,and the temperature is of 37~38℃, The assessment byShanxi Mineral and Resources Reserve Committee proved that it is Sr-bearing metasilicatesulfate Na bicarbonate type of top-quality mineral water.
关键词
矿泉水
地热异常
稷山县
水质评价
mineral water,geothermal anomally,Renhe of Jishan