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dc.contributor.authorEbrahimi, Davoud
dc.contributor.authorWhittle, Andrew J.
dc.contributor.authorPellenq, Roland Jm
dc.contributor.authorWhittle, Andrew
dc.date.accessioned2016-07-15T21:57:45Z
dc.date.available2017-04-11T21:29:35Z
dc.date.issued2016-06
dc.identifier.issn1434-5021
dc.identifier.issn1434-7636
dc.identifier.urihttp://hdl.handle.net/1721.1/103633
dc.description.abstractThis paper proposes a novel methodology for understanding the meso-scale aggregation of clay platelets in water. We use Molecular Dynamics simulations using the CLAYFF force fields to represent the interactions between two layers of Wyoming montmorillonite (Na-smectite) in bulk water. The analyses are used to establish the potential of mean force at different spacings between the layers for edge-to-edge and face-to-face interactions. This is accomplished by finding the change in free energy as a function of the separation distance between the platelets using thermodynamic perturbation theory with a simple overlap sampling method. These nanoscale results are then used to calibrate the Gay–Berne (GB) potential that represents each platelet as a single-site ellipsoidal body. A coarse-graining upscaling approach then uses the GB potentials and molecular dynamics to represent the meso-scale aggregation of clay platelets (at submicron length scale). Results from meso-scale simulations obtain the equilibrium/jamming configurations for mono-disperse clay platelets. The results show aggregation for a range of clay platelets dimensions and pressures with mean stack size ranging from 3 to 8 platelets. The particle assemblies become more ordered and exhibit more pronounced elastic anisotropy at higher confining pressures. The results are in good agreement with previously measured nano-indentation moduli over a wide range of clay packing densities.en_US
dc.publisherSpringer Berlin Heidelbergen_US
dc.relation.isversionofhttp://dx.doi.org/10.1007/s10035-016-0655-8en_US
dc.rightsCreative Commons Attribution-Noncommercial-Share Alikeen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-sa/4.0/en_US
dc.sourceSpringer Berlin Heidelbergen_US
dc.titleMesoscale simulation of clay aggregate formation and mechanical propertiesen_US
dc.typeArticleen_US
dc.identifier.citationEbrahimi, Davoud, Roland J.-M. Pellenq, and Andrew J. Whittle. “Mesoscale Simulation of Clay Aggregate Formation and Mechanical Properties.” Granular Matter 18.3 (2016): n. pag.en_US
dc.contributor.departmentMassachusetts Institute of Technology. Department of Civil and Environmental Engineeringen_US
dc.contributor.mitauthorEbrahimi, Davouden_US
dc.contributor.mitauthorPellenq, Roland Jmen_US
dc.contributor.mitauthorWhittle, Andrewen_US
dc.relation.journalGranular Matteren_US
dc.eprint.versionAuthor's final manuscripten_US
dc.type.urihttp://purl.org/eprint/type/JournalArticleen_US
eprint.statushttp://purl.org/eprint/status/PeerRevieweden_US
dc.date.updated2016-06-30T12:07:23Z
dc.language.rfc3066en
dc.rights.holderSpringer-Verlag Berlin Heidelberg
dspace.orderedauthorsEbrahimi, Davoud; Pellenq, Roland J.-M.; Whittle, Andrew J.en_US
dspace.embargo.termsNen
dc.identifier.orcidhttps://orcid.org/0000-0001-5358-4140
dc.identifier.orcidhttps://orcid.org/0000-0001-5559-4190
dc.identifier.orcidhttps://orcid.org/0000-0001-9898-7023
mit.licenseOPEN_ACCESS_POLICYen_US


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