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Scattering of a longitudinal wave by a circular crack in a fluid-saturated porous medium

机译:饱和流体在多孔介质中圆形裂纹对纵波的散射

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Physical properties of many natural and man-made materials can be modelled using the concept of poroelasticity. Some porous materials, in addition to the network of pores, contain larger inhomogeneities such as inclusions, cavities, fractures or cracks. A common method of detecting such inhomogeneities is based on the use of elastic wave scattering. We consider interaction of a normally incident time-harmonic; longitudinal plane wave with a circular crack imbedded in a porous medium governed by Biot's equations of dynamic poroelasticity. The problem is formulated in cylindrical co-ordinates as a system of dual integral equations for the Hankel transform of the wave field, which is then reduced to a single Fredholm integral equation of the second kind. It is found that the scattering that takes place is predominantly due to wave induced fluid flow between the pores and the crack. The scattering magnitude depends on the size of the crack relative to the slow wave wavelength and has it's maximum value when they are of the same order. (C) 2007 Elsevier Ltd. All rights reserved.
机译:可以使用多孔弹性的概念来模拟许多天然和人造材料的物理特性。除孔网络之外,某些多孔材料还包含较大的不均匀性,例如夹杂物,空洞,裂缝或裂缝。检测这种不均匀性的常用方法是基于弹性波散射的使用。我们考虑了正常入射时间谐波的相互作用。带有圆形裂纹的纵向平面波嵌入在由Biot动力学孔隙弹性方程控制的多孔介质中。该问题在圆柱坐标系中表示为对波场进行汉克尔变换的对偶积分方程组,然后将其简化为第二种单个Fredholm积分方程。发现发生的散射主要是由于波引起的孔隙和裂缝之间的流体流动。散射量取决于裂缝相对于慢波波长的大小,并且当它们处于相同数量级时具有最大值。 (C)2007 Elsevier Ltd.保留所有权利。

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