摘要
本文阐述了矿泉水形成与赋存条件，指出该矿泉水赋存于第四系中、上更新统中粗砂为主的孔隙中，属松散岩类孔隙水。该矿泉水水化学类型为重碳酸钙·镁型，锶、偏硅酸达到饮用天然矿泉水国家标准（ＧＢ８５３７－８７）的界限指标，属含锶－偏硅酸的重碳酸钙·镁型饮用天然矿泉水。
In this paper,the author explains the conditions of mineral water formation and occur-rence,and points out that the mineral water is mainly occurred in the coarse sands of Upper-Middle-pleistocene Series of Quaternary.It is calcium-magnesium-bicarbonate type,and thecontents of strontium and metasilicate reach the limiting targets of National Standard ofPotable Natural Mineral Water(GB 8537-87),so it belongs to calcium-magnesium-bicarbon-ate drinking natural mineral water with strontium and metasilicate.
关键词
矿泉水
锶
偏硅酸
重碳酸钙
镁
天然矿泉水
mineral water,strontium, metasilicate,calcium-magnesium-bicarbonatetype,Longyao of Hebei
