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首页> 外文期刊>Journal of Petroleum Science & Engineering >Frequency-dependent attenuation of compressional wave and seismic effects in porous reservoirs saturated with multi-phase fluids
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Frequency-dependent attenuation of compressional wave and seismic effects in porous reservoirs saturated with multi-phase fluids

机译:多相流体饱和的多孔储层中压缩波的频率相关衰减和地震效应

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Varying fluid types and saturations in porous media cause attenuation of compressional seismic waves and thus contribute to frequency-dependent reflections. We analyze the frequency-dependent attenuation and the corresponding seismic reflection behavior by taking into account the effects of the multi-phase fluid on the wave-induced fluid flow in porous reservoir. Fluid viscosity, the property that largely controls pore-fluid mobility, is proportional to the relaxation time, which in turn influences the frequency-dependent velocities. Here, we describe the variation of effective viscosity varies with saturation for a sandstone reservoir saturated for different multi-phase fluid mixtures using the Refutas equation. Then we explore the frequency-dependent velocity and inverse quality factors under different fluid saturation cases by employing equivalent-medium theory of Chapman's model. Next, we present a frequency-dependent phase-shift wavefield extrapolation method to simulate frequency-dependent seismic wavefield on 4-layer models. Comparative analyses indicate that the frequency-dependent attenuation and the seismic behaviors are functions of fluid viscosity associated with hydrocarbon saturations. Hydrocarbon saturations in fluid mixture strongly affect attenuation and characteristic frequencies. The frequency-dependent attenuation within the seismic frequency range can be increased due to the presence of hydrocarbons in multi-phase fluids. Synthetic seismic records indicate that the frequency-dependent attenuation of compressional wave and seismic reflection signatures are significantly dependent on hydrocarbon saturation, in terms of amplitude, waveform and traveltime of the reflection located at the base of the saturated reservoir and the underlying shale layer. (C) 2016 Elsevier B.V. All rights reserved.
机译:多孔介质中流体类型和饱和度的变化会导致压缩地震波的衰减,从而导致频率相关的反射。通过考虑多相流体对多孔储层中波浪诱导的流体流动的影响,我们分析了频率相关的衰减和相应的地震反射行为。流体粘度是很大程度上控制孔隙流体流动性的特性,它与松弛时间成正比,而松弛时间又会影响频率相关的速度。在这里,我们使用Refutas方程描述了对于不同多相流体混合物饱和的砂岩储层,有效粘度随饱和度的变化。然后,利用查普曼模型的等效介质理论,研究了在不同流体饱和情况下频率相关的速度和品质因数的逆问题。接下来,我们提出一种基于频率的相移波场外推法,以在4层模型上模拟基于频率的地震波场。比较分析表明,随频率变化的衰减和地震行为是与烃饱和度相关的流体粘度的函数。流体混合物中的烃饱和度强烈影响衰减和特征频率。由于多相流体中存在碳氢化合物,因此可以增加地震频率范围内与频率有关的衰减。综合地震记录表明,压缩波和地震反射信号的频率相关衰减在很大程度上取决于油气饱和度,就饱和油藏底部和下层页岩层反射的振幅,波形和传播时间而言。 (C)2016 Elsevier B.V.保留所有权利。

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