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Conductivity of Double-Porosity Carbonate Formations Saturated with Water – Oil Mixtures

机译:水-油混合物饱和的双孔隙碳酸盐岩层的电导率

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The determination of water saturation from resistivity logs is an important problem in formation evaluation required for the correct assessment of oil-resources. In carbonate formations this problem is especially complicated because of the complex structure of pore space composed of the small-scale matrix porosity and large-scale secondary pores of different shapes. In this paper we introduce a new approach for calculating the conductivity of carbonate formations with different wettability types. This approach is based on the double porosity model and computing the conductivity of pore saturating fluid treated as a mixture of conductive water and non-conductive oil (gas) inclusions. The non-conductive component is represented by spheroids embedded in the water (host). The variation of inclusion shapes allows us to model the dependence of conductivity on the formation wettability. The calculations have shown that the effective conductivity of the double porosity formations significantly depends on the type of the secondary pores, rock wettability, and water saturation of the matrix and secondary pore-systems. This result indicates that the assessment of the water saturation in carbonate formations, using traditional approaches without considering the secondary-porosity and wettability types, may lead to erroneous oil reserve estimation.
机译:从电阻率测井确定水饱和度是正确评估石油资源所需的地层评估中的重要问题。在碳酸盐岩地层中,这个问题特别复杂,因为孔隙空间的结构复杂,由小规模的基质孔隙度和不同形状的大规模次生孔隙组成。在本文中,我们介绍了一种用于计算具有不同润湿性类型的碳酸盐岩层电导率的新方法。该方法基于双重孔隙率模型,并计算被视为导电水和非导电油(气)夹杂物的混合物的孔隙饱和流体的电导率。非导电成分由嵌入水(主体)中的球状体表示。夹杂物形状的变化使我们能够对电导率对地层润湿性的依赖性进行建模。计算表明,双重孔隙地层的有效电导率在很大程度上取决于次生孔隙的类型,岩石的润湿性以及基质和次生孔隙系统的水饱和度。该结果表明,在不考虑次生孔隙度和润湿性类型的情况下,使用传统方法评估碳酸盐岩地层中的水饱和度可能会导致错误的储油量估算。

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