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dc.contributor.authorDupuis, Romain
dc.contributor.authorPellenq, Roland
dc.date.accessioned2021-03-02T15:00:12Z
dc.date.available2021-03-02T15:00:12Z
dc.date.issued2019-04
dc.identifier.urihttps://hdl.handle.net/1721.1/130029
dc.description.abstractAlkali-silica-reaction (ASR) is a significant cause of premature concrete deterioration. Although it has received much research attention, an essential question still remains—how does a soft gel, as is formed by this reaction, induce the critical level of stress to exceed the strength of, and crack the concrete matrix? One possibility is that the ASR gel increases in viscosity as it imbibes calcium with age and a concomitant expansion causes the concrete failure. Another is that the gel’s rate of flow into the porous microstructure is slower than the rate at which it forms, which builds up stresses that cannot be relieved. To better understand ASR mechanisms and to eventually test these hypotheses, we sought a basic understanding at the atomic scale.en_US
dc.relation.ispartofseriesMIT CSHub Research Brief; Volume 2019, Issue 3en_US
dc.subjectPoromechanicsen_US
dc.subjectCementen_US
dc.subjectAlkali-silica Reactionen_US
dc.titleResearch Brief: Simulating the Formation of ASR Gelsen_US


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