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根据HB方程并考虑多种导电影响因素,得到了泥质砂岩的含水饱和度理论公式。该理论公式与已有公式相比,较全面地考虑了诸如泥质导电、岩石骨架导电、地层束缚水导电等因素对岩石整体导电性的贡献,为进一步研究泥质砂岩含水饱和度奠定了基础。
According to HB equation and considering a variety of conductive factors, the theoretical formula of water saturation of shaly sands is obtained. Compared with the existing formulas, the theoretical formula more comprehensively considers the contributions to the overall conductivity of rocks such as mud conductivity, conductivity of rock skeleton, conductivity of formation bound water and the like, which lays a foundation for further studying the water saturation of shaly sands .