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Wave propagation in layered dry, saturated and unsaturated poroelastic media

机译:波在干燥,饱和和不饱和层状多孔弹性介质中的传播

摘要

An exact stiffness formalism is presented to study harmonic and transient wave propagation in multilayered dry, saturated and unsaturated isotropic poroelastic media. Smeulders' extension of Blot's poroelastic theory is used to incorporate-unsaturated porous media with a small gas fraction. A-wide range of problems in geophysical and civil engineering can be treated, ranging from amplification of plane harmonic waves, dispersion and attenuation of surface waves to transient wave propagation due to a forced excitation. The effect of full or partial saturation on wave propagation in a poroelastic layered halfspace is demonstrated in a numerical example, in which the layering is caused by a moving ground water table. (C) 1998 Elsevier Science. All rights reserved.
机译:提出了一种精确的刚度形式,以研究谐波和瞬态波在干,饱和和不饱和各向同性多孔弹性多层介质中的传播。 Smeulders对Blot多孔弹性理论的扩展用于掺入气体含量较小的不饱和多孔介质。可以解决地球物理和土木工程中的各种问题,从平面谐波的放大,表面波的色散和衰减到由于强制激励而引起的瞬态波传播。在数值示例中说明了完全饱和或部分饱和对波在多孔弹性分层半空间中传播的影响,其中分层是由地下水位移动引起的。 (C)1998 Elsevier科学。版权所有。

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