首页> 外文期刊>Petrophysics: The SPWLA Journal of Formation Evaluation and Reservoir Description >Simulation of the Electrical Resistivity of Dual-Porosity Carbonate Formations Saturated with Fluid Mixtures
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Simulation of the Electrical Resistivity of Dual-Porosity Carbonate Formations Saturated with Fluid Mixtures

机译:混合流体饱和的双孔碳酸盐岩地层电阻率的模拟

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For carbonate formations characterized by a complex pore structure, traditional methods for estimating water saturation from resistivity logs can lead to significant errors. In this paper we present the results of simulations of the effective electrical conductivity of dual-porosity carbonate formations saturated with fluid mixtures. For the calculations we have applied the Effective Medium Approximation method. Carbonate rocks are represented is media composed of (1) a matrix with solid grains and small-scale primary pores, and (2) large-scale secondary pores embedded in this matrix. In this model, all components are approximated by tri-axial ellipsoids. We consider different distributions of water and non-conductive fluid in the primary and secondary pores. The matrix pore system has been represented by a mixture of pores that are completely saturated either with water or with non-conductive fluids, by pores approximated by layered ellipsoids where the outer layer is water (water-wet formations), and by a combination of these two models. Water distribution in the secondary pore system has been modeled by layered ellipsoids where water occupies the outer layer. We have obtained dependences of the effective electrical resistivity as a function of saturation of the primary and secondary pores for different secondary-pore concentrations and types. The calculations have shown that the application of Archie's expression for a single-pore system results in under- or over-estimation of the water saturation in dual-porosity carbonates. Depending on the secondary-pore shapes and concentrations, the relative errors in the determination of water saturation can reach 25-30 percent for formations with a matrix porosity of 0.08-0.10 and a secondary porosity of 0.01-0.02. Based on the simulations performed, we propose an approach for determining water saturation in dual-porosity water-wet carbonate formations. The approach includes (1) the estimation of the type and concentration of the secondary pores using joint inversion of micro-electrical and acoustic data, and (2) the assessment of water saturation by adjusting the model parameters so that the calculated resistivity agrees with that measured by laterologs. The feasibility of evaluating water saturation using this approach is demonstrated with experimental data.
机译:对于以复杂孔隙结构为特征的碳酸盐岩地层,传统的根据电阻率测井估算水饱和度的方法可能会导致重大误差。在本文中,我们介绍了用流体混合物饱和的双孔隙碳酸盐岩地层有效电导率的模拟结果。对于计算,我们采用了有效介质近似法。碳酸盐岩是由(1)具有固体颗粒和小尺度初级孔隙的基质和(2)埋在该基质中的大规模次级孔隙组成的介质。在此模型中,所有分量均由三轴椭球近似。我们考虑了水和非导电流体在主要和次要孔隙中的不同分布。基质孔隙系统的特征是,混合物被水或非导电性流体完全饱和,被层状椭球体(其中外层是水)近似的孔隙(水湿地层)和这两个模型。次要孔隙系统中的水分布已通过分层椭圆形进行建模,其中水占据了外层。对于不同的次级孔浓度和类型,我们已经获得了有效电阻率与初级孔和次级孔饱和度的函数关系。计算结果表明,将Archie表达式用于单孔系统会导致双孔隙度碳酸盐中水饱和度的估计过低或过高。根据次生孔的形状和浓度,对于基质孔隙度为0.08-0.10和次生孔隙度为0.01-0.02的地层,水饱和度测定中的相对误差可达到25-30%。基于执行的模拟,我们提出了一种确定双孔隙水湿碳酸盐岩地层中水饱和度的方法。该方法包括(1)使用微电声数据的联合反演来估算次生孔隙的类型和浓度,以及(2)通过调整模型参数以使计算出的电阻率与通过事后测验来衡量。实验数据证明了使用这种方法评估水饱和度的可行性。

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