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Time-lapse joint AVO inversion using generalized linear method based on exact Zoeppritz equations

机译:基于精确ZOEPPRITZ方程的广义线性方法的时间流逝联合AVO反演

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The conventional method of time-lapse AVO (Amplitude Versus Offset) inversion is mainly based on the approximate expression of Zoeppritz equations. Though the approximate expression is concise and convenient to use, it has certain limitations. For example, its application condition is that the difference of elastic parameters between the upper medium and lower medium is little and the incident angle is small. In addition, the inversion of density is not stable. Therefore, we develop the method of time-lapse joint AVO inversion based on exact Zoeppritz equations. In this method, we apply exact Zoeppritz equations to calculate the reflection coefficient of PP wave. And in the construction of objective function for inversion, we use Taylor series expansion to linearize the inversion problem. Through the joint AVO inversion of seismic data in baseline survey and monitor survey, we can obtain the P-wave velocity, S-wave velocity, density in baseline survey and their time-lapse changes simultaneously. We can also estimate the oil saturation change according to inversion results. Compared with the time-lapse difference inversion, the joint inversion doesn't need certain assumptions and can estimate more parameters simultaneously. It has a better applicability. Meanwhile, by using the generalized linear method, the inversion is easily implemented and its calculation cost is small. We use the theoretical model to generate synthetic seismic records to test and analyze the influence of random noise. The results can prove the availability and anti-noise interference ability of our method. We also apply the inversion to actual field data and prove the feasibility of our method in actual situation. (C) 2018 Elsevier B.V. All rights reserved.
机译:传统的延期AVO(振幅与偏移)反转方法主要基于Zoeppritz方程的近似表达。虽然近似表达式简洁而方便使用,但它具有一定的限制。例如,其应用条件是上介质和下介质之间的弹性参数的差异几乎没有,入射角小。此外,密度的反转不稳定。因此,我们基于精确的Zoeppritz方程式开发时间流逝联合AVO反转的方法。在该方法中,我们应用精确的Zoeppritz方程来计算PP波的反射系数。并且在建造反演的客观函数时,我们使用泰勒序列扩张来线性化反演问题。通过基线调查和监测调查中的地震数据的联合AVO反转,我们可以获得P波速度,S波速度,基线调查密度及其延时同时变化。我们还可以根据反演结果估算油饱和度变化。与时间流逝差反转相比,联合反演不需要某些假设,并且可以同时估计更多参数。它具有更好的适用性。同时,通过使用广义的线性方法,容易实现反演,其计算成本很小。我们使用理论模型来产生合成地震记录来测试和分析随机噪声的影响。结果可以证明我们方法的可用性和抗噪声干扰能力。我们还将反转应用于实际现场数据,并证明了我们在实际情况下的方法的可行性。 (c)2018 Elsevier B.v.保留所有权利。

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