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根据惰性气体含量计算深层地下水的形成温度
Determination of deep groundwater paleotemperatures by the calculation of dissolved noble gases amount
【摘要】 惰性气体在地下水中的溶解量主要取决于水温和气体分压.而且溶解度在常见的水温范围内是水温的单调函数.因此,当深层地下水系统处于封闭状态,系统中不存在蜕变成因的惰性气体源时,可将溶解的惰性气体作为指示地下水形成温度的天然示踪剂.
【Abstract】 The concentration of the noble gases dissolved in groundwater depends mainly on the water temperature and the partial pressure of the gases and is , in normal temperatur range , the monotonous function of the water temperature. Therefore, the dissolved noblegases can be used as natural tracing elements to estimate the groundwater pal-eotemperature, if the deep flow system is a confined one and meanwhile there is no radiogenic or metamorphic noble gases in it.
- 【文献出处】 淮南矿业学院学报 , 编辑部邮箱 ,1995年02期
- 【分类号】P641
- 【被引频次】1
- 【下载频次】33