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

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 inhomogeneit...

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Main Authors: Galvin, R., Gurevich, Boris
Format: Journal Article
Published: Elsevier 2007
Subjects:
Online Access:http://hdl.handle.net/20.500.11937/46119
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author Galvin, R.
Gurevich, Boris
author_facet Galvin, R.
Gurevich, Boris
author_sort Galvin, R.
building Curtin Institutional Repository
collection Online Access
description 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 inducedfluid 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.
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spelling curtin-20.500.11937-461192019-02-19T05:35:18Z Scattering of a longitudinal wave by a circular crack in a fluid-saturated porous medium Galvin, R. Gurevich, Boris Biot theory slow wave poroelasticity fractured medium 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 inducedfluid 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. 2007 Journal Article http://hdl.handle.net/20.500.11937/46119 10.1016/j.ijsolstr.2007.04.011 Elsevier fulltext
spellingShingle Biot theory
slow wave
poroelasticity
fractured medium
Galvin, R.
Gurevich, Boris
Scattering of a longitudinal wave by a circular crack in a fluid-saturated porous medium
title Scattering of a longitudinal wave by a circular crack in a fluid-saturated porous medium
title_full Scattering of a longitudinal wave by a circular crack in a fluid-saturated porous medium
title_fullStr Scattering of a longitudinal wave by a circular crack in a fluid-saturated porous medium
title_full_unstemmed Scattering of a longitudinal wave by a circular crack in a fluid-saturated porous medium
title_short Scattering of a longitudinal wave by a circular crack in a fluid-saturated porous medium
title_sort scattering of a longitudinal wave by a circular crack in a fluid-saturated porous medium
topic Biot theory
slow wave
poroelasticity
fractured medium
url http://hdl.handle.net/20.500.11937/46119