关中地区地下热水的分类

基金项目:

中国地质调查局地质调查(鄂尔多斯盆地地下水勘查)项目(编号:121201013302)

详细信息

Classification of thermal water in Guanzhong Area, Shaanxi Province

School of Environment Science and Engineering, Chang'an University, Xi'an 710054, China

摘要: 环境同位素研究结果表明,研究区地热水为大气降水成因。根据降水补给的年代及混合程度可将地下热水分为主要由现代大气降水补给的混合型地下热水;由现代大气降水和古代降水补给的混合型地下热水;主要由古代大气降水补给的深部循环型地下热水。
- 地下热水 /
- 环境同位素 /
- 大气降水 /
- 关中地区
Abstract: The meteoric origin of geothermal water in study area is evidenced by its environmental isotope composition.The geothermal water can be classified into three categories based on the time when replenishment take place and mixing extent with normal groundwater which are:geothermal water mixing with normal groundwater recharged mainly by the modern meteoric water;geothermal water mixing with normal groundwater water recharged by both ancient and modern meteoric water;deep-runoff geothermal water recharged mainly by ancient meteoric water.
- geothermal water /
- environmental isotope /
- precipitation /
- Guanzhong Area