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Journal ArticleDOI

Study of wave motions in fluid‐saturated porous rocks

C. H. Yew, +1 more
- 01 Jul 1976 - 
- Vol. 60, Iss: 1, pp 2-8
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TLDR
In this paper, Biot's theory was employed in the study of wave motions in fluid-saturated porous rocks and the equations were solved using a Laplace transformation, and it was shown that the measured waves are in fact the fast waves.
Abstract
In this investigation, Biot’s theory was employed in the study of wave motions in fluid‐saturated porous rocks. Consistent with the described experimental arrangement, Biot’s equations were solved using a Laplace transformation. The theory predicts two dilatational waves: a slightly dispersed fast wave propagating ahead of a heavily dispersed and attenuated slow wave. By comparing these results with experimental results, it becomes evident that the measured waves are in fact the fast waves.Subject Classification: [43]20.15, [43]20.40.

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Reflection and refraction at an imperfectly bonded interface between poroelastic solid and cracked elastic solid

J. S Nandal, +1 more
TL;DR: In this paper, the energy shares of reflected and refracted waves at the plane interface between water-saturated sandstone and basalt are computed and analyzed for different values of crack parameters as well as loose bonding parameters.
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On Axially Symmetric Vibrations of Fluid Filled Poroelastic Spherical Shells

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An experimental study of shock-induced wave propagation in dry, water-saturated, and partially saturated porous media

TL;DR: A submitted manuscript is the version of the article upon submission and before peer-review as mentioned in this paper, while a published version is the final layout of the paper including the volume, issue and page numbers.
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