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Wave propagation through elastically-anisotropic fluid-saturated porous rocks
School of Mathematics, University of Bath.
Luleå tekniska universitet.
1989 (English)In: Journal of applied mechanics, ISSN 0021-8936, E-ISSN 1528-9036, Vol. 56, no 4, p. 744-750Article in journal (Refereed) Published
Abstract [en]

An elastically-anisotropic sedimentary rock is modeled by a simple cubic packing of identical, contacting spherical particles. The connected pore space is filled with an inviscid, compressible fluid. A set of averaged equations is derived to relate the constitutive and dynamic coupling coefficients, and hence also the effective wave speeds in any given direction explicitly to the microstructural properties of the rock considered. Simple, explicit results are obtained when the propagation of either a purely longitudinal or a purely transverse wave is considered.

Place, publisher, year, edition, pages
1989. Vol. 56, no 4, p. 744-750
National Category
Other Civil Engineering
Research subject
Mining and Rock Engineering
Identifiers
URN: urn:nbn:se:ltu:diva-5019Local ID: 30a805a0-ffdf-11dc-8441-000ea68e967bOAI: oai:DiVA.org:ltu-5019DiVA, id: diva2:977893
Note
Godkänd; 1989; 20080401 (cira)Available from: 2016-09-29 Created: 2016-09-29 Last updated: 2017-11-21Bibliographically approved

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