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首页> 外文期刊>Pure and Applied Geophysics >Oscillating Flow of a Compressible Fluid through Deformable Pipes and Pipe Networks: Wave Propagation Phenomena
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Oscillating Flow of a Compressible Fluid through Deformable Pipes and Pipe Networks: Wave Propagation Phenomena

机译:可变形流体通过可变形管和管网的振荡流动:波传播现象

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摘要

Similarly to blood pulse propagation in the artery system, oscillating flow can propagate as a wave in fluid-saturated pipes, networks of pipes or, by extension, in porous media, if the fluid is compressible and/or the pipes are elastically deformable. First, propagation of flow waves generated in a semi-infinite pipe by harmonic pressure oscillations at the pipe entrance is analyzed. The dispersion equation is derived, allowing determination of the phase velocity and quality factor as functions of frequency. Wave reflections at the end of a finite-length pipe and ensuing interferences between forward and backward traveling waves are then examined. Because of fluid storage in the pipe, the amplitude of the AC volumetric fluxes entering and exiting the pipe at its upstream and downstream ends are not equal. Thus, two different, upstream and downstream, frequencydependent, AC hydraulic conductivities are introduced. Superposed on the classic viscous-inertial flow transition (controlled by the value of the pipe radius), these complex-valued parameters show another transition between an interference-free regime at low frequencies and a strong interference regime above a critical frequency that roughly scales as the pipe length. Because of attenuation, the flow wave interferences tend to gradually weaken with increasing frequencies. Finally, the single pipe model is used to investigate fluid flow waves through pipe networks with results very similar to those described above. The flow waves analyzed here are akin to the Biot’s slow P waves and their propagation properties could affect seismic soundings in some geological settings.
机译:与脉搏在动脉系统中的传播相似,如果流体是可压缩的和/或管道是可弹性变形的,则振荡流可以在流体饱和的管道,管道网络中或作为扩展在多孔介质中以波的形式传播。首先,分析了在管道入口处由谐波压力振荡在半无限管道中产生的流波的传播。导出了色散方程,可以确定相速度和品质因数作为频率的函数。然后检查有限长管道末端的波反射以及随之产生的前进和后退行波之间的干扰。由于管道中存储的流体,进入和离开管道的上游和下游端的交流体积通量的振幅不相等。因此,引入了两种不同的,取决于频率的上游和下游的交流水力传导率。这些复杂值参数叠加在经典的粘滞-惯性流过渡(由管道半径的值控制)上,显示出低频的无干扰状态和临界频率以上的强干扰状态之间的另一种过渡,大致按比例缩放管道长度。由于衰减,流波干扰会随着频率的增加而逐渐减弱。最后,单管模型用于研究流经管网的流体波,其结果与上述结果非常相似。此处分析的流波类似于毕奥的慢速P波,它们的传播特性可能会影响某些地质环境中的地震测深。

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