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Pair distribution function analysis of nanostructural deformation of calcium silicate hydrate under compressive stress

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dc.contributor.authorBae, Sungchul-
dc.contributor.authorJee, Hyeonseok-
dc.contributor.authorKanematsu, Manabu-
dc.contributor.authorShiro, Ayumi-
dc.contributor.authorMachida, Akihiko-
dc.contributor.authorWatanuki, Tetsu-
dc.contributor.authorShobu, Takahisa-
dc.contributor.authorSuzuki, Hiroshi-
dc.date.accessioned2022-07-12T17:16:31Z-
dc.date.available2022-07-12T17:16:31Z-
dc.date.issued2018-01-
dc.identifier.issn0002-7820-
dc.identifier.issn1551-2916-
dc.identifier.urihttps://scholarworks.bwise.kr/hanyang/handle/2021.sw.hanyang/150732-
dc.description.abstractDespite enormous interest in calcium silicate hydrate (C-S-H), its detailed atomic structure and intrinsic deformation under an external load are lacking. This study demonstrates the nanostructural deformation process of C-S-H in tricalcium silicate (C3S) paste as a function of applied stress by interpreting atomic pair distribution function (PDF) based on insitu X-ray scattering. Three different strains in C3S paste under compression were compared using a strain gauge, Bragg peak shift, and the real space PDF. PDF refinement revealed that the C-S-H phase mostly contributed to PDF from 0 to 20 angstrom whereas crystalline phases dominated that beyond 20 angstrom. The short-range atomic strains exhibited two regions for C-S-H: I) plastic deformation (0-10 MPa) and II) linear elastic deformation (>10 MPa), whereas the long-range deformation beyond 20 angstrom was similar to that of Ca(OH)(2). Below 10 MPa, the short-range strain was caused by the densification of C-S-H induced by the removal of interlayer or gel-pore water. The strain is likely to be recovered when the removed water returns to C-S-H.-
dc.format.extent11-
dc.language영어-
dc.language.isoENG-
dc.publisherAmerican Ceramic Society-
dc.titlePair distribution function analysis of nanostructural deformation of calcium silicate hydrate under compressive stress-
dc.typeArticle-
dc.publisher.location미국-
dc.identifier.doi10.1111/jace.15185-
dc.identifier.scopusid2-s2.0-85028766311-
dc.identifier.wosid000414367400044-
dc.identifier.bibliographicCitationJournal of the American Ceramic Society, v.101, no.1, pp 408 - 418-
dc.citation.titleJournal of the American Ceramic Society-
dc.citation.volume101-
dc.citation.number1-
dc.citation.startPage408-
dc.citation.endPage418-
dc.type.docTypeArticle-
dc.description.isOpenAccessN-
dc.description.journalRegisteredClasssci-
dc.description.journalRegisteredClassscie-
dc.description.journalRegisteredClassscopus-
dc.relation.journalResearchAreaMaterials Science-
dc.relation.journalWebOfScienceCategoryMaterials Science, Ceramics-
dc.subject.keywordPlusC-S-H-
dc.subject.keywordPlusPORTLAND-CEMENT-
dc.subject.keywordPlusDIFFRACTION-
dc.subject.keywordPlusPASTE-
dc.subject.keywordPlusTEMPERATURE-
dc.subject.keywordPlusPRESSURE-
dc.subject.keywordPlusPHASE-
dc.subject.keywordPlusMODEL-
dc.subject.keywordAuthorcalcium silicate hydrate-
dc.subject.keywordAuthordeformation-
dc.subject.keywordAuthorportland cement-
dc.subject.keywordAuthorX-ray methods-
dc.identifier.urlhttps://ceramics.onlinelibrary.wiley.com/doi/10.1111/jace.15185-
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