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首页> 外文期刊>Journal of Applied Geophysics >The effect of a variable pore radius on formation resistivity factor
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The effect of a variable pore radius on formation resistivity factor

机译:可变孔隙半径对地层电阻率因子的影响

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Formation resistivity factor F was introduced as the ratio of the resistivity of a rock fully saturated with conductive water to the resistivity of the conductive water based on results of laboratory measurements. It was also found that the formation factor is a function of the type and character of a formation and is related to porosity by a relationship including an exponent m. For model calculations of the formation factor, capillary channel models describing a straight tube with a constant circular cross-sectional area are frequently used. However, the pore channel radius is not constant in natural rocks.
机译:根据实验室测量的结果,引入地层电阻率因子F作为完全被导电水饱和的岩石的电阻率与导电水的电阻率之比。还发现地层因子是地层类型和特征的函数,并且通过包括指数m的关系与孔隙率相关。对于形成因子的模型计算,经常使用描述具有恒定圆形横截面面积的直管的毛细管通道模型。然而,天然岩石中的孔隙通道半径不是恒定的。

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