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Interfacial, pore geometry and saturation effect on complex resistivity of shaly sandstone: dispersion and laboratory investigation

机译:页岩砂岩的界面,孔隙几何形状和饱和度对复电阻率的影响:分散和实验室研究

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The electrical evaluation of reservoir rock needs to deem several factors that really describe a subsurface condition. As confining pressure can cause either pore space of the rock to collapse or rock properties to change, a detailed identification towards the extent of the pressure and water saturation effect on electrical properties is needed. This work is mainly focused on the investigations of electrical properties on shaly sandstones, encompassing the effects of pore geometries, confining pressure, and partial water saturation on electrical properties. Here, the frequency of electrical measurement is between 1 Hz and 0.2 MHz. It is indicated that an interfacial and geometry change due to pressure is easily recognized by imaginary resistivity in low water saturation, reflecting that confining pressure will affect only small defect to pore geometry. Meanwhile in high water saturation, bulk volume conductivity is more dominant, thus making interfacial contribution negligible. From petrographic analysis of this work it is found that only pore radius distribution has a good relationship with electrical dispersion. The relaxation time and its distribution are estimated by simultaneous inversion of real and imaginary resistivity. The Cole-Cole model inversion is applied to obtain these parameters. For this purpose, the integration of Lavenberg-Marquardt and Singular Value decomposition (SVD) are used in order to avoid singularity problems. The obtainment of decreasing of relaxation time with the increasing of confining pressure reflects the reduction of the internal surface area.
机译:储层岩石的电学评估需要考虑几个真正描述地下条件的因素。由于围压会导致岩石的孔隙空间塌陷或岩石性质发生变化,因此需要详细确定压力和水饱和度对电性质的影响程度。这项工作主要集中于研究泥质砂岩的电学性质,包括孔隙几何形状,围压和部分含水饱和度对电学性质的影响。在此,电气测量的频率在1 Hz至0.2 MHz之间。结果表明,在低水饱和度下,假想的电阻率很容易识别出由于压力引起的界面和几何形状的变化,这反映了围压仅会影响孔隙几何形状的微小缺陷。同时,在高含水饱和度下,体积电导率更为占优势,因此界面贡献可忽略不计。从这项工作的岩石学分析发现,只有孔半径分布与电扩散具有良好的关系。弛豫时间及其分布是通过同时反演实,虚电阻率来估算的。应用Cole-Cole模型反演获得这些参数。为此,使用Lavenberg-Marquardt和奇异值分解(SVD)的积分以避免奇异性问题。随着围压的增加,弛豫时间的减少反映了内表面积的减少。

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