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Numerical Estimation of Seismic Wave Attenuation in Fractured Porous Fluid-Saturated Media

机译:裂隙多孔流体饱和介质中地震波衰减的数值估计

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Study of wave-induced fluid flow (WIFF) became actual in geophysics last years, because attenuation caused by this effect can serve as indicator of fractured highly-permeable reservoirs. In our work we model two-scale fractured domains with small scale fractures forming percolating clusters. Statistical geometry analysis and numerical wave propagation simulations using finite-difference approximation of Biot's dynamic equations were done to estimate seismic attenuation and investigate the dependence of attenuation due to WIFF on percolation length. Theoretical predictions of at tenuation due to scattering are also provided. Obtained estimations demonstrate sufficient correlation between fracture connectivity and attenuation of waves propagating in considered fractured media.
机译:近年来,对波诱导流体流(WIFF)的研究在地球物理学中已成为现实,因为这种作用引起的衰减可以作为裂缝性高渗透储层的指示。在我们的工作中,我们对两级裂缝域进行建模,小范围裂缝形成渗流团簇。使用Biot动力学方程的有限差分近似进行统计几何分析和数值波传播模拟,以估算地震衰减并研究WIFF引起的衰减对渗流长度的依赖性。还提供了由于散射引起的衰减时的理论预测。所获得的估计值表明,裂缝连通性与在考虑的裂缝介质中传播的波的衰减之间具有足够的相关性。

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