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dc.contributor.authorNavarro Gámir, Vicente
dc.contributor.authorMorena Borja, Gema de la
dc.contributor.authorGonzález Arteaga, Jesús
dc.contributor.authorYustres Real, Ángel
dc.contributor.authorAsensio Sánchez, Laura
dc.date.accessioned2021-12-26T11:57:11Z
dc.date.available2021-12-26T11:57:11Z
dc.date.issued2018-09
dc.identifier.issn23523808
dc.identifier.urihttp://hdl.handle.net/20.500.12251/2303
dc.description.abstractThe volumetric deformability of the microstructure of compacted active clays is linked to the water mass exchange with the macrostructural void space. Given that this exchange is determined by the difference in the chemical potential of water in these two structural levels, this work proposes to define a microstructural effective stress (understood as the magnitude controlling microstructural strains) from this difference in chemical potentials, identifying the microstructural effective stress with the thermodynamic swelling pressure. To assess the scope of this definition, an inspection exercise has been conducted, examining the important functional dependence on the microstructural void ratio for different loads, water content and environmental salinity conditions. For the compacted active clays analysed, the thermodynamic swelling pressure is a robust and consistent definition of the microstructural effective stress. © 2017 Elsevier Ltdes
dc.language.isoenges
dc.publisherElsevier Ltdes
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 Internacional*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/*
dc.titleA microstructural effective stress definition for compacted active clayses
dc.typearticlees
dc.identifier.doi10.1016/j.gete.2017.11.003
dc.identifier.urlhttps://doi.org/10.1016/j.gete.2017.11.003es
dc.journal.titleGeomechanics for Energy and the Environmentes
dc.page.initial47es
dc.page.final53es
dc.rights.accessRightsopenAccesses
dc.volume.number15es
dc.item.number103356es


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