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Thermal treatment of kaolin: The effect of mineralogy on the pozzolanic activity

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dc.contributor.author Kakali, G en
dc.contributor.author Perraki, T en
dc.contributor.author Tsivilis, S en
dc.contributor.author Badogiannis, E en
dc.date.accessioned 2014-03-01T01:17:16Z
dc.date.available 2014-03-01T01:17:16Z
dc.date.issued 2001 en
dc.identifier.issn 0169-1317 en
dc.identifier.uri https://dspace.lib.ntua.gr/xmlui/handle/123456789/14427
dc.subject Calcination en
dc.subject Kaolin en
dc.subject Metakaolinite en
dc.subject Mineralogy en
dc.subject Pozzolanic activity en
dc.subject.classification Mineralogy en
dc.subject.other Differential thermal analysis en
dc.subject.other Heat treatment en
dc.subject.other Infrared spectroscopy en
dc.subject.other Mineralogy en
dc.subject.other Thermoanalysis en
dc.subject.other X ray diffraction analysis en
dc.subject.other Pozzolanic activity en
dc.subject.other Kaolin en
dc.subject.other cement en
dc.subject.other kaolin en
dc.subject.other mineralogy en
dc.subject.other thermal alteration en
dc.title Thermal treatment of kaolin: The effect of mineralogy on the pozzolanic activity en
heal.type journalArticle en
heal.identifier.primary 10.1016/S0169-1317(01)00040-0 en
heal.identifier.secondary http://dx.doi.org/10.1016/S0169-1317(01)00040-0 en
heal.language English en
heal.publicationDate 2001 en
heal.abstract This paper reports an investigation on the effect of mineralogy on the pozzolanic activity of fired kaolin. Representative samples of Greek kaolin (Milos Island) and a commercial kaolin of high purity are studied. The samples are tested by X-ray diffraction (XRD), Differential Thermal Analysis (DTA) and Infrared (IR) Spectroscopy in order to determine their mineralogical composition and structural differences. Calcination of samples is carried out at 650 degreesC for 3 h. The decomposition of kaolinite and alunite is recorded using methods of thermal analysis. The resultant products are identified by XRD. The reactivity of the thermally treated samples is evaluated based on Chapelle test. It is concluded that the pozzolanic activity of metakaolinite is strongly related to the crystallinity of the original kaolinite. Well-ordered kaolinite is transformed into less reactive metakaolinite. (C) 2001 Elsevier Science B.V. All rights reserved. en
heal.publisher ELSEVIER SCIENCE BV en
heal.journalName Applied Clay Science en
dc.identifier.doi 10.1016/S0169-1317(01)00040-0 en
dc.identifier.isi ISI:000171063400007 en
dc.identifier.volume 20 en
dc.identifier.issue 1-2 en
dc.identifier.spage 73 en
dc.identifier.epage 80 en


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