The Possible Use of Tritium' for Estimating Groundwater Storage

The Possible Use of Tritium' for Estimating Groundwater Storage
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DOI:
10.3402/tellusa.v10i4.9265
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发表时间:
1958-11
期刊:
Tellus A
影响因子:
--
通讯作者:
E. Eriksson
E. Eriksson
中科院分区:
其他
文献类型:
--
作者:
E. Eriksson

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鉴于Begemann&Libby(1957)最近的一项工作,对他们关于地下水体内快速混合的假设进行了检验。研究发现,不存在可以实现这种混合的可能过程。然而,他们的观察结果可以很容易地从一个简单的地下水流动模型中得到解释,假设没有混合。文中还讨论了利用氚等示踪剂估算地下水储量的可能方法。DOI:10.1111/j.2153-3490.1958.tb02035.x
In view of a recent work by Begemann & Libby (1957) their postulate on rapid mixing inside a groundwater body is examined. It is found that there are no possible processes which can accomplish such a mixing. Their observations can, however, be readily explained from a simple model of groundwater flow, assuming no mixing. Possible methods of using tracers like tritium for estimating groundwater storage are also discussed. DOI: 10.1111/j.2153-3490.1958.tb02035.x