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Accurate Jacobian Matrix Using the Exact Zoeppritz Equations and Effects on the Inversion of Reservoir Properties in Porous Media

机译:使用精确的Zoeppritz方程和对多孔介质中储层性能反转的效果准确的Jacobian矩阵

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The analysis of amplitude variation with offset (AVO) plays a significant role in fluid detection and lithology discrimination in hydrocarbon reservoirs. The Zoeppritz equations are part of the basic theory of AVO analysis which describes the relationship between seismic reflection and transmission coefficients and elastic rock properties (e.g., P- and S-wave velocities and density). Currently, most AVO inversion methods are based on approximations of the exact Zoeppritz equations, which not only limit the accuracy of AVO inversion, but also restrict its application to wide-angle seismic reflection data. In addition, the most difficult part of linear AVO inversion obtaining an accurate Jacobian matrix (partial derivatives of reflection coefficients with respect to inverted parameters). Based on our previous study on the accurate gradient calculation of seismic reflection coefficients for the inversion of rock properties, we further combine the exact Zoeppritz equations with Biot-Gassmann equations to compute the gradients of seismic reflection coefficients with solid density and reservoir properties (e.g., porosity, water/gas/oil saturations) in porous media. In this paper, the partial derivative expressions of the Zoeppritz matrix elements with respect to solid density and reservoir properties are simplified to simple algebraic equations, which are readily calculated. By comparing reflection coefficients and partial derivative curves with those obtained by classic Shuey and Aki-Richards approximations, we show that our proposed method can be used to accurately obtain reservoir properties in AVO inversion.
机译:用偏移(AVO)对振幅变化的分析在流体检测和碳氢化合物储层中的岩性辨别中起着重要作用。 ZOEPPRITZ方程是AVO分析基本理论的一部分,其描述了地震反射和透射系数与弹性岩石性质(例如,P-和S波速度和密度)之间的关系。目前,大多数AVO反转方法基于精确Zoeppritz方程的近似,这不仅限制了AVO反转的准确性,还限制了其在广角地震反射数据的应用。另外,线性AVO反转的最困难的部分获得精确的雅各比矩阵(反射系数的部分导数相对于反相参数)。基于我们先前关于岩石性能反演的地震反射系数的准确梯度计算的研究,我们进一步将精确的Zoeppritz方程与Biot-Gassmann方程组合,以计算具有固体密度和储存器的地震反射系数的梯度(例如,多孔介质中的孔隙度,水/气/油饱和度)。在本文中,简化了Zoeppritz矩阵元件的Zoeppritz矩阵元件的局部导数表达到简单的代数方程,其简单地计算。通过将反射系数和部分衍生曲线与通过经典的Shuey和Aki-Richards近似获得的反射系数和部分导数曲线进行比较,我们表明我们的提出方法可用于精确地在AVO反转中获得储层性质。

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