dc.creatorMilanesi, Carlos Alberto
dc.creatorMarfil, Silvina Andrea
dc.creatorBatic, Oscar R.
dc.creatorMaiza, Pedro
dc.date1996-10
dc.date.accessioned2022-10-16T23:00:10Z
dc.date.available2022-10-16T23:00:10Z
dc.identifierhttps://digital.cic.gba.gob.ar/handle/11746/10234
dc.identifierRecurso online
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/4413066
dc.descriptionThree dolomitic rocks from Argentina were studied under different test conditions (ASTM C 586, ASTM C 227, CSA A23.2-14A, powdered rock samples immersed in strong alkali Solutions). X-ray diffraction (XRD), optical microscopy (OM) and scanning electrón microscopy (SEM) analyses of the various reaction producís detected under these conditions are presented. Results are compared with the alkali expansivity of the dolomitic rocks and are also used to discuss the scope and applicability of the different reaction mechanisms proposed in the literature. It has been concluded ffom this research that the mechanism originally proposed by Hadley is adequate to explain the reaction mechanisms that opérate in concrete structures under natural Service conditions.
dc.formatapplication/pdf
dc.formatp. 1579-1591
dc.languageInglés
dc.relationdoi:10.1016/0008-8846(96)00140-8
dc.rightshttp://creativecommons.org/licenses/by-nc-sa/4.0/
dc.subjectIngeniería de los Materiales
dc.subjectdolomitic rocks
dc.subjectalkali expansivity
dc.subjectreaction mechanisms
dc.titleThe alkali-carbonate reaction and its reaction products an experience with argentinean dolomite rocks


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