Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/95096
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dc.contributorDepartment of Civil and Environmental Engineeringen_US
dc.creatorWei, PCen_US
dc.creatorZhang, LLen_US
dc.creatorZheng, YYen_US
dc.creatorDiao, QFen_US
dc.creatorZhuang, DYen_US
dc.creatorYin, ZYen_US
dc.date.accessioned2022-09-14T08:20:02Z-
dc.date.available2022-09-14T08:20:02Z-
dc.identifier.issn0169-1317en_US
dc.identifier.urihttp://hdl.handle.net/10397/95096-
dc.language.isoenen_US
dc.publisherElsevier BVen_US
dc.rights© 2021 Elsevier B.V. All rights reserved.en_US
dc.rights© 2021. This manuscript version is made available under the CC-BY-NC-ND 4.0 license http://creativecommons.org/licenses/by-nc-nd/4.0/.en_US
dc.rightsThe following publication Wei, P.-C., et al. (2021). "Nanoscale friction characteristics of hydrated montmorillonites using molecular dynamics." Applied Clay Science 210: 106155 is available at https://dx.doi.org/10.1016/j.clay.2021.106155.en_US
dc.subjectHydrated montmorilloniteen_US
dc.subjectMolecular Dynamicsen_US
dc.subjectNanoscale frictionen_US
dc.subjectNormal loaden_US
dc.subjectSliding velocityen_US
dc.titleNanoscale friction characteristics of hydrated montmorillonites using molecular dynamicsen_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.volume210en_US
dc.identifier.doi10.1016/j.clay.2021.106155en_US
dcterms.abstractThe interparticle friction behavior of saturated clay controls its mechanical properties, but remains unclear at nanoscale. As one of major clay minerals, the hydrated montmorillonite (MMT) is selected to investigate the nanoscale friction characteristics using Molecular Dynamics simulation method. Two portions of MMT representing two particles with a water film in the middle are created to simulate an undrained system. A virtual spring is applied on the upper MMT portion to provide the sliding with a constant velocity relative to the bottom portion. The effects of normal load and sliding velocity on the frictional behavior are then investigated. The friction coefficients of hydrated MMT at different cases were measured and compared with other experimental and simulation results for the validation. The evolution of normal load with the number of hydrogen bonds for hydrated MMT was finally analyzed. All simulation results indicated that the friction load fluctuated periodically with a cycle of about 9.10 Å at sliding velocity inferior 0.001 Å•fs−1, which was nearly equal to montmorillonite's lattice constant along the sliding direction; the fluctuation amplitude of the friction load increased with the decreasing sliding velocity; the relationship between the average friction load and the logarithm of sliding velocity followed a power function; the friction coefficient and the cohesion were found to increase approximately linearly with sliding velocity.en_US
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationApplied clay science, 1 Sept. 2021, v. 210, 106155en_US
dcterms.isPartOfApplied clay scienceen_US
dcterms.issued2021-09-01-
dc.identifier.scopus2-s2.0-85107157989-
dc.identifier.eissn1872-9053en_US
dc.identifier.artn106155en_US
dc.description.validate202209 bcfcen_US
dc.description.oaAccepted Manuscripten_US
dc.identifier.FolderNumberCEE-0181-
dc.description.fundingSourceRGCen_US
dc.description.fundingSourceOthersen_US
dc.description.fundingTextNatural Science Foundation of GuangDong Basic and Applied Basic Research Foundation; NSFCen_US
dc.description.pubStatusPublisheden_US
dc.identifier.OPUS52566846-
dc.description.oaCategoryGreen (AAM)en_US
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