Please use this identifier to cite or link to this item: https://hdl.handle.net/11499/47656
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dc.contributor.authorSonmezer Y.B.-
dc.contributor.authorKayabalı K.-
dc.contributor.authorBeyaz T.-
dc.contributor.authorFener M.-
dc.date.accessioned2023-01-09T21:29:30Z-
dc.date.available2023-01-09T21:29:30Z-
dc.date.issued2022-
dc.identifier.issn2005-307X-
dc.identifier.urihttps://doi.org/10.12989/gae.2022.31.2.167-
dc.identifier.urihttps://hdl.handle.net/11499/47656-
dc.description.abstractSoil liquefaction has been one of the most important concerns in geotechnical earthquake engineering in recent years, due to its damages to structures and its destructive effects. The cyclic liquefaction of silty sands, in particular, remains of great interest for both research and application. Although many factors are known that affect the liquefaction resistance of sands, the effect of fine grain content is perhaps one of the most studied and still controversial. In this study, 48 deformation-controlled cyclic simple shear tests were performed on BS and CS silt samples mixed with 5%, 15% and 30% by weight of Krk085, Krk042 and Krk025 sands in constant–volume conditions to determine the liquefaction potential of silty sands. The tests were carried out at 30% and 50% relative density and under 100 kPa effective stress. The results revealed that the liquefaction potential of silty sand increases with increasing average particle size ratio (D50sand / d50silt) of the mixture for a fixed silt content. Furthermore, for identical base sand, the liquefaction potentials of coarse grained sands increase with increasing silt content, while the respective potentials of fine grained sands generally decrease. However, this situation may vary depending on the silt grain structure and is affected by the nature of the fine grains. In addition, the variation of the void ratio interval was shown to provide a good intuition in determining the liquefaction potentials of silty sands, while the intergranular void ratio alone does not constitute a criterion for determining the liquefaction potentials of silty sands. © 2022 Techno-Press, Ltd.en_US
dc.language.isoenen_US
dc.publisherTechno-Pressen_US
dc.relation.ispartofGeomechanics and Engineeringen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectcyclic simple shearen_US
dc.subjectfines contenten_US
dc.subjectliquefactionen_US
dc.subjectsanden_US
dc.subjectsilten_US
dc.subjectEarthquake engineeringen_US
dc.subjectGeophysicsen_US
dc.subjectGrain size and shapeen_US
dc.subjectParticle sizeen_US
dc.subjectSilten_US
dc.subjectSoil liquefactionen_US
dc.subjectTexturesen_US
dc.subjectCyclic simple shearen_US
dc.subjectFiner grainsen_US
dc.subjectFines contenten_US
dc.subjectGeotechnicalen_US
dc.subjectGrainsizeen_US
dc.subjectLiquefaction potentialsen_US
dc.subjectSilt contentsen_US
dc.subjectSilty sandsen_US
dc.subjectSize ratioen_US
dc.subjectVoids ratioen_US
dc.subjectSanden_US
dc.titleInfluence of grain size ratio and silt content on the liquefaction potentials of silty sandsen_US
dc.typeArticleen_US
dc.identifier.volume31en_US
dc.identifier.issue2en_US
dc.identifier.startpage167en_US
dc.identifier.endpage181en_US
dc.identifier.doi10.12989/gae.2022.31.2.167-
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.authorscopusid56507422900-
dc.authorscopusid55898708900-
dc.authorscopusid12753032900-
dc.authorscopusid14522411400-
dc.identifier.scopus2-s2.0-85140210108en_US
dc.identifier.wosWOS:000880087700004en_US
dc.identifier.scopusqualityQ2-
item.languageiso639-1en-
item.fulltextNo Fulltext-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.cerifentitytypePublications-
item.openairetypeArticle-
item.grantfulltextnone-
crisitem.author.dept10.08. Geological Engineering-
Appears in Collections:Mühendislik Fakültesi Koleksiyonu
Scopus İndeksli Yayınlar Koleksiyonu / Scopus Indexed Publications Collection
WoS İndeksli Yayınlar Koleksiyonu / WoS Indexed Publications Collection
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