摘要
常德市区及其以北约70km2范围里矿泉水资源极其丰富.从地形地貌、地质构造、水文地质、地球化学条件几方面出发,对戴家岗矿泉水水源地的形成条件、特别是对矿泉水中偏硅酸形成的地球化学条件及循环深度进行了分析,对开展本区域或相似类型矿泉水水源地勘查评价工作具有积极的借鉴意义.
Mineral spring water resource in Changde city and 70 kilometers north of downtown was repoted. According to the topography, geological structure, hydrogeological and geochemical conditions of the starting areas, Daijiagang formation conditions of mineral water sources, especially for the formation of metasilicate mineral water conditions and circulation depth of geochemical were analysised, which was positive to the conduct of the regional or similar types of mineral exploration and evaluation of water sources.
出处
《湖南文理学院学报(自然科学版)》
CAS
2009年第3期85-87,90,共4页
Journal of Hunan University of Arts and Science(Science and Technology)
关键词
常德市
矿泉水
水文地质
地球化学
形成条件
Changde city
mineral spring water
hydrogeol- ogy
geochemistry
forming condition