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承德市乾隆泉饮用天然矿泉水特征
引用本文:崔石林.承德市乾隆泉饮用天然矿泉水特征[J].华北地质矿产杂志,1995,10(4):463-466.
作者姓名:崔石林
作者单位:河北地质矿产勘查开发局第4地质大队
摘    要:乾隆泉饮用天然矿泉水产于著名的承德避暑山庄之南的崔梨沟。该泉水受NNW向大南沟断裂控制。赋存岩层为上株罗系张家口组、鸡冠山组火山碎屑岩。降水入渗过程中,淋滤了火山凝灰岩中的多种成分,形成了重碳酸钙-钠型、低矿化度矿泉水,水中含偏硅酸49.5mg/L,氟1.0mg/L,锶0.136mg/L,锌0.004mg/L,锂0.001mg/L,对人类具有很高的医疗保健价值。

关 键 词:饮用  天然矿泉水  火山凝灰岩  上侏罗世

Qianlong Spring Natural Mineral Water of Cuiligou in Chengde,Hebei
Authors:Cui Shilin
Abstract:Qianlong Spring potable natural mineral water is located at Cuiligou.The spring is con-trolled by NNW Danangou fault,and occurs in the volcanic clastic rocks of Zhangjiakou For-mation and Jiguanshan Formation of Upper Jurrassic.It belongs to bicarbonate of Calcium,low Na,low mineralization mineral water,and is formed through the filtration of the volcanictuffs by the precipitation inflow. The mineral water contains metasilicate 49.6 mg/L,F1.0mg/L,Sr 0.136 mg/L,Zn 0.004 mg/L,Li 0.001 mg/L,and is of high value of medical andhealth care.
Keywords:potable natural mineral water  Upper Jurassic  volcanic tuffs  Chengde City
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