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Seismic wave attenuation and dispersion induced by fluid flow within various cracks and a small amount of bubbly fluid

机译:各种裂缝内流体流动诱导的地震波衰减和分散和少量的泡沫流体

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Hydrocarbon reservoirs usually contain pores and various cracks, which may contain a small amount of bubble fluid. In this study, based on the wave theory of basic porous medium, the influence of various factors on fluid pressure are investigated, and then the stress-strain relationship and Lagrangea??s equations with a dissipation function is utilized to derive the elastic wave equation of porous medium containing various cracks and a small amount of bubbly fluid initially. This elastic wave equation describes the influence of squirt flow induced by various cracks on seismic wave attenuation and dispersion, and the influence of the bubble linear vibration on seismic wave attenuation and dispersion effectively. Then, the seismic wave attenuation and dispersion of a given model is estimated and the matching of rock physics parameters are obtained in different frequency bands. The numerical results illustrate that the proposed approach is compatible with previous theory to explain the mechanics of the seismic wave attenuation and dispersion induced by fluid flow and can better describe the propagation of elastic waves in actual rock medium especially for the mechanics of the seismic wave attenuation and dispersion induced by fluid flow within various cracks and a small amount of bubble fluid.
机译:碳氢化合物储层通常含有孔和各种裂缝,其可含有少量的气泡流体。在本研究中,基于基本多孔介质的波理论,研究了各种因素对流体压力的影响,然后利用具有耗散函数的应力 - 应变关系和拉格朗斯的等式来导出弹性波方程最初含有各种裂缝和少量气泡流体的多孔介质。这种弹性波方程描述了各种裂缝引起的抗冲流对地震波衰减和分散的影响,以及泡沫线性振动有效地震波衰减和分散的影响。然后,估计给定模型的地震波衰减和分散,并在不同频带中获得岩石物理参数的匹配。数值结果说明了所提出的方法与先前的理论兼容,以解释流体流动诱导的地震波衰减和分散的机制,并且可以更好地描述在实际岩体介质中的弹性波的传播,特别是对于地震波衰减的力学。通过流体流动在各种裂缝内和少量气泡流体诱导的分散。

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