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Determination of Primary and Secondary Porosity in Carbonate Formations Using Acoustic Data

机译:利用声波数据确定碳酸盐岩地层中的一次和二次孔隙度

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A technique for quantitative estimation of crack or vugporosity using acoustic well-log data is proposed. Theestimation is based on a double-porosity rock model thatconsists of a solid matrix with primary porosity and inclusionswhich represent the secondary pore system. We applied themethod of effective medium approximation (EMA) tocalculate P- and S-wave velocities in the double-porosityformations. This method allows modeling multicomponentsystems composed by grains of different mineral components,primary pores and secondary inclusions. All these componentsare approximated by spheroids with different aspect ratios.The technique includes two steps. At the first step the matrixP- and S-wave velocities as functions of the primary porosityare calculated. For this procedure two groups of parametersare required: 1 - solid-skeleton elastic moduli that are definedby laboratory measurements or calculated using formationmineralogical composition; 2 - aspect ratios for grains andprimary pores. We determined these aspect ratios by theinversion of the published regression equations for P- and Swavevelocities to the microstructure parameters.At the second step, using the obtained previously matrixparameters, the value and aspect ratio of secondary pores aredetermined by the joint inversion of P- and S-velocities(minimizing the difference between the experimental data andvelocities predicted for the double-porosity model). Theobtained aspect ratio indicates the type of secondary-poresystem (cracks or vugs).Examples of secondary-porosity determination using acousticcore and well log data are presented.
机译:定量评估裂缝或孔洞的技术 提出了使用声波测井数据的孔隙度。这 估计是基于双孔隙岩石模型, 由具有主要孔隙率和夹杂物的固体基质组成 代表次生孔隙系统。我们应用了 有效介质近似(EMA)的方法 计算双孔隙中的P波和S波速度 编队。该方法允许对多组分进行建模 由不同矿物成分的谷物组成的系统, 主要毛孔和次要夹杂物。所有这些组成部分 由具有不同长宽比的球体近似。 该技术包括两个步骤。第一步,矩阵 P波和S波速度与主要孔隙度的关系 被计算。对于此过程,两组参数 需要:1-定义的实体骨架弹性模量 通过实验室测量或使用地层计算 矿物组成; 2-纵横比 初级毛孔。我们通过 已发布的P波和Swave回归方程的反演 速度对微结构参数的影响。 第二步,使用获得的先前矩阵 参数,次生孔隙的值和长宽比为 由P速度和S速度的联合反演确定 (最大程度地减少了实验数据与 双孔隙率模型预测的速度)。这 获得的长宽比表示次级孔的类型 系统(裂缝或洞洞)。 使用声学确定次生孔隙度的示例 介绍了岩心和测井数据。

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