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首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >Propagation of Biot slow waves in heterogeneous pipe networks: Effect of the pipe radius distribution on the effective wave velocity and attenuation
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Propagation of Biot slow waves in heterogeneous pipe networks: Effect of the pipe radius distribution on the effective wave velocity and attenuation

机译:比奥慢波在异质管网中的传播:管半径分布对有效波速和衰减的影响

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摘要

This paper extends a previous study of the harmonic (or AC) flow of a compressible fluid through a single, elastic, thick-wall pipe. The model previously developed is used to investigate propagation of pore-scale Biot slow waves through heterogeneous one-, two- and three-dimensional networks of pipes. A novel method is applied to the results of the network simulations to numerically determine the dispersion equation of the upscaled Biot slow waves and investigate its dependence on pore-scale heterogeneity. As a function of frequency, the phase velocity of the macroscale Biot slow waves displays an S-shaped curve, increasing from zero at low frequencies (i.e., nonpropagative regime) to C_x at high frequencies (i.e., propagative regime with С_x lower than the sound velocity in the fluid). The transition between these two regimes is marked by the inflection point at the frequency x_B (whereis inversely proportional to the length scale A characteristic of fluid flow and permeability). The high-frequency phase velocity С depends on the dimensionality of the network considered and decreases with increasing heterogeneity. The wave attenuation (as measured by the inverse quality factor) also presents an S-shaped curve, decreasing from 2 (i.e., critical damping) to zero, with the same inflection point at This behavior is approximately independent on the pore radius distribution, provided that x_B (or the corresponding fluid flow length scale A) is held constant. A mechanism based on wave scattering and interferences of forward and backward traveling (pore-scale) Riot slow waves is proposed to explain the observations.
机译:本文扩展了先前对可压缩流体通过单个弹性厚壁管的谐波(或AC)流的研究。先前开发的模型用于研究孔尺度毕特慢波通过异质一维,二维和三维管网的传播。一种新的方法应用于网络模拟的结果,以数值方式确定放大的毕特慢波的弥散方程,并研究其对孔隙尺度非均质性的依赖性。作为频率的函数,大尺度毕奥特慢波的相速度显示出一条S形曲线,从低频处的零(即非传播状态)增加到高频处的C_x(即С_x低于声音的传播状态)流体中的速度)。这两个状态之间的过渡由频率x_B处的拐点标记(其中,它与流体流动和渗透率的特征长度标A成反比)。高频相速度С取决于所考虑网络的维数,并且随着异质性的增加而降低。在相同的拐点处,波衰减(通过逆品质因数测量)也呈现出一条S形曲线,从2(即临界阻尼)减小到零,这种行为大致与孔半径分布无关,只要x_B(或相应的流体流动长度标度A)保持恒定。提出了一种基于波散射和前进和后退(孔径)Riot慢波干扰的机制来解释这些现象。

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