摘要
为研究长白山地区广泛分布的偏硅酸型矿泉水的补给源,通过氢氧同位素与水化学分析,结合水文地质、地球物理等资料,确定长白山泉水接受来自于西藏羌塘盆地的外源水补给。长白山泉水TDS很低但富含偏硅酸的现象表明,地下水流经的含水层是由硅酸盐等火山岩组成,结合长白山地区火山玄武岩大量的喷发事实,推断地下水导水通道由孔洞玄武岩构成。指出应加强对西藏冰川、河流与湖泊的保护,从而确保长白山优质矿泉水能够持续地开发利用。
In order to study the supply source of widely distributed metasilicate type mineral water in the Changbai Mountain area,based on the information of hydrogeology and geophysics,the water supply of the Changbai Mountain springs from the Qiangtang Basin in Tibet was determined,through the hydrogen and oxygen isotope analysis as well as the water chemical analysis. TDS of the Changbai Mountain spring water is low,but with rich metasilicate,and this phenomenon indicates that the aquifer that water flows through is composed of silicate volcanic rock. Combined with the massive eruption of volcanic basalt in the area of Changbai Mountain,it can be concluded that the groundwater channel is composed of pore basalt. Therefore,the protection of Tibetan glaciers,rivers and lakes should be strengthened to ensure the sustainable development and utilization of high-quality mineral water in the area of Changbai Mountain.
引文
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