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Fractional Current Flow in the Subsurface Using Electrical Resistivity Method: A Laboratory Approach

机译:使用电阻率法在地下流动的分数流动:实验室方法

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The authors describe electrical resistivity method using a laboratory experiment, which was conducted in order to calculate the percentage of current that penetrated each layer of soil arranged in a container using Schlumberger array. Four soil samples arranged in three dif ferent set-ups were used. The apparent resistivity obtained was interpreted using curve matching tech niques and WinResist iteration yielding types A curve, H curve and A curve, respectively. The interpreted data gave the resistivity of each layer and its thicknesses. The thicknesses obtained from the interpretation were at variance with the actual thicknesses arranged in the container. A multiplier was obtained which serves as a constant in other to obtain the actual thickness. The effective penetration depth of current was determined through the calculated thickness of each layer and the known electrode spacing (AB). The percentage of cur rent that penetrates the layers was found to depend on the electrode spacing as well as the thickness of that layer. Thus, a layer with relatively small thickness has a small percentage of current passing through it com pared to a thicker layer.
机译:作者描述了使用实验室实验的电阻率法,以便计算使用Schlumberger阵列排列在容器中的每层土壤的电流百分比。使用了三种在三个不同的设置中排列的四种土壤样品。使用曲线匹配技术Niques和WinResist迭代的曲线分别释放曲线,H曲线和曲线的曲线迭代所获得的表观电阻率。解释的数据给出了每层的电阻率及其厚度。从解释中获得的厚度与布置在容器中的实际厚度方差。获得乘法器,其用作常数以获得实际厚度。通过计算每个层的厚度和已知电极间距(AB)来确定电流的有效渗透深度。发现了穿透层的CUR租金的百分比,以取决于电极间距以及该层的厚度。因此,具有相对较小的厚度的层具有小的电流百分比,其通过其与较厚的层进行混合。

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