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A New Method For The Determination Of Geophysical Parameters By Radon Concentration Measurements In Bore-hole

机译:钻孔中Rad浓度测定地球物理参数的新方法

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We propose a new method to measure the ~(222)Rn concentration in a closed bore-hole and to use the results for estimation of the diffusion parameter and the average radium content of the surrounding geological formations. In a closed bore-hole, only several meters from the surface, the radon concentration is rather constant (in the ±15% range) under different meteorological conditions. The inflow of radon gas, after removing the radon from the bore-hole by dry nitrogen, shows characteristic time-dependence, which is determined by the diffusion parameter for radon in the surrounding environment. The experimental data were well described by a straightforward model calculation. From the results estimate can be given for the diffusion parameter and for the average radium content of the surrounding geological formation.
机译:我们提出了一种新方法来测量封闭井眼中〜(222)Rn的浓度,并将结果用于估算扩散参数和周围地质构造的平均镭含量。在距离地面仅几米的封闭钻孔中,under在不同气象条件下的浓度相当恒定(在±15%范围内)。在用干燥氮气将the从钻孔中除去后,of气的流入显示出特征性的时间依赖性,这取决于周围环境中ra的扩散参数。通过简单的模型计算可以很好地描述实验数据。从结果可以估计出扩散参数和周围地质构造的平均镭含量。

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