基于电导率张量的各向异性介质含水饱和度研究

Rong Geng, Yujue Gao, Xu Liu, Zhitao Zhang
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引用次数: 2

摘要

地层电性各向异性是指测量地层视电阻率时,地层视电阻率随测量方向的变化。由于录井仪测得的电导率张量与岩心分析测得的分量重合,在储层评价中往往忽略了其他张量分量。电导率张量标度表示实验室岩心的电各向异性。电导率张量测量仪很难在一次实验中完全得到电导率张量的九个分量。根据阿奇公式测井仪测得的电阻率计算含水饱和度。常用的方法是根据标量Archie公式分别建立电导率张量各主轴分量与含水饱和度的关系,从而推导含水饱和度张量表达式。本文在文献研究成果的基础上,利用电导率张量测量仪对方形铁芯进行测量,测量了铁芯电导率张量的9个分量,并讨论了可应用于实验室的阿奇张量表达式。阿奇公式的未知系数由实验室数据确定。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Study of water saturation in electrically anisotropic media based on conductivity tensor
The formation electrical anisotropy means that the formation apparent resistivity changes with the direction of measurement when the formation apparent resistivity is measured. Because the electrical conductivity tensor measured by the well logging instrument coincides with the component measured in the core analysis, other tensor components are often ignored in formation evaluation. The electrical anisotropy of the laboratory core is indicated by the conductivity tensor scale. It is difficult to obtain the nine components of the conductivity tensor completely in one experiment with the conductivity tensor measuring instrument. The water saturation can be calculated according to the resistivity measured by the Archie formula logging instrument. The common method is to establish the relation of the main axis components of the conductivity tensor on water saturation respectively according to the scalar Archie formula, so as to derive the tensor expression of water saturation. In this paper, based on the literature research results, the conductivity tensor measuring instrument is used to measure the square core, and the 9 components of the conductivity tensor of the core are measured, and the expression of Archie tensor which can be applied to the laboratory is discussed. The unknown coefficients of Archie formula are determined by laboratory data.
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