黔中地区某饮用天然矿泉水成因动态特征研究

Study on the origin and dynamic characteristics of a drinking natural mineral water in the middle area of Guizhou

贵州省地下水资源丰富,水质优良,以岩溶大泉、地下河的形式出露地表,寻找优质矿泉水资源对于推动贵州省地方绿色经济发展、改善民众生活水平具有重要意义。贵州省矿泉水成因分为红层盆地型、碳酸盐岩层控型以及断裂裂隙型三大类。本文通过资料收集、资料综合研究、动态长观、水质分析等手段,表明凤岗县红沙沟饮用天然矿泉水为含锶型饮用天然矿泉水,成因属于碳酸盐岩层控型兼断裂裂隙型,动态类型属于较稳定型,水质优良,具有很强的开发潜力。对红沙沟矿泉水成因规律进行研究,对于西南岩溶地区找寻优质矿泉水资源具有重要的指导意义。

Guizhou Province is rich in groundwater resources and has excellent water quality.It is exposed to the surface in the form of karst springs and underground rivers.Finding high-quality mineral water resources is of great significance to promoting the development of local green economy in Guizhou Province and improving people’s living standards.The genesis of mineral water in Guizhou Province can be divided into three categories:red bed basin type,carbonate rock layer-controlled type and fault fracture type.By means of data collection,data comprehensive research,dynamic long view,and water quality analysis,this paper shows that the drinking natural mineral water in Hongshagou,Fenggang County,is a strontium-containing drinking natural mineral water,and its genesis belongs to the carbonate rock stratum-controlled type and the fracture fissure type.The dynamic type is relatively stable,with excellent water quality and strong development potential.The research on the genetic law of Hongshagou mineral water has important guiding significance for the search for high-quality mineral water resources in the karst area of southwest China.