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Analytical boundary integral solutions for cracks and thin fluid-filled layers in a 3D poroelastic solid in time and wavenumber domain

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dc.contributor.author Heimisson, Elías R.
dc.date.accessioned 2024-09-06T01:06:40Z
dc.date.available 2024-09-06T01:06:40Z
dc.date.issued 2024-05
dc.identifier.citation Heimisson , E R 2024 , ' Analytical boundary integral solutions for cracks and thin fluid-filled layers in a 3D poroelastic solid in time and wavenumber domain ' , Journal of the Mechanics and Physics of Solids , vol. 186 , 105591 . https://doi.org/10.1016/j.jmps.2024.105591
dc.identifier.issn 0022-5096
dc.identifier.other 227484164
dc.identifier.other d50b0a52-0c40-4c86-ac59-1a69791ac5d3
dc.identifier.other 85186267281
dc.identifier.uri https://hdl.handle.net/20.500.11815/4979
dc.description Publisher Copyright: © 2024 The Author
dc.description.abstract The spectral boundary integral (SBI) method has been widely employed in the study of fractures and friction within elastic and elastodynamic media, given its natural applicability to thin or infinitesimal interfaces. Many such interfaces and layers are also prevalent in porous, fluid-filled media. In this work, we introduce analytical SBI equations for cracks and thin layers in a 3D medium, with a particular focus on fluid presence within these interfaces or layers. We present three distinct solutions, each based on different assumptions: arbitrary pressure boundary conditions, arbitrary flux boundary conditions, or a bi-linear pressure profile within the layer. The bi-linear pressure solution models the flux through a thin, potentially pressurized, leaky layer. We highlight conditions under which the bi-linear SBI equations simplify to either the arbitrary flux or arbitrary pressure SBI equations, contingent on a specific non-dimensional parameter. We then delve into the in-plane pressure effects arising from a shear crack in a poroelastic solid. While such pressurization has been suggested to influence frictional strength in various ways and only occurs in mode II sliding, our findings indicate that a significant portion of the crack face is affected in 3D scenarios. Additionally, we investigate non-dimensional timescales governing the potential migration of this pressurization beyond the crack tip, which could induce strength alterations beyond the initially ruptured area.
dc.format.extent 1195460
dc.format.extent
dc.language.iso en
dc.relation.ispartofseries Journal of the Mechanics and Physics of Solids; 186()
dc.rights info:eu-repo/semantics/openAccess
dc.subject Boundary integrals
dc.subject Fracture
dc.subject Friction
dc.subject Geological material
dc.subject Porous material
dc.subject Condensed Matter Physics
dc.subject Mechanics of Materials
dc.subject Mechanical Engineering
dc.title Analytical boundary integral solutions for cracks and thin fluid-filled layers in a 3D poroelastic solid in time and wavenumber domain
dc.type /dk/atira/pure/researchoutput/researchoutputtypes/contributiontojournal/article
dc.description.version Peer reviewed
dc.identifier.doi 10.1016/j.jmps.2024.105591
dc.relation.url http://www.scopus.com/inward/record.url?scp=85186267281&partnerID=8YFLogxK
dc.contributor.school Engineering and Natural Sciences


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