| 根据惰性气体含量计算深层地下水的形成温度 |
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| 引用本文： | 成春奇,徐龙.根据惰性气体含量计算深层地下水的形成温度[J].安徽理工大学学报(自然科学版),1995(2). |
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| 作者姓名： | 成春奇 徐龙 |
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| 作者单位： | 淮南矿业学院资源与环境工程系 |
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| 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.
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| 关 键 词： | 零族无素 地下水 水温 |
Determination of deep groundwater paleotemperatures by the calculation of dissolved noble gases amount |
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| Cheng Chunqi Xu Long.Determination of deep groundwater paleotemperatures by the calculation of dissolved noble gases amount[J].Journal of Anhui University of Science and Technology:Natural Science,1995(2). |
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| Authors: | Cheng Chunqi Xu Long |
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| Institution: | Dept. of Resources and Environment Engineering |
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| 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. |
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| Keywords: | group 0 elements ground water water temperature |
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