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dc.contributor.authorMohd Sobri, Idris
dc.contributor.authorKhairul Nizar, Ismail
dc.contributor.authorShamsul Baharin, Jamaludin
dc.contributor.authorChe Mohd Ruzaidi, Ghazali
dc.contributor.authorKamarudin, Hussin
dc.date.accessioned2008-09-12T08:18:51Z
dc.date.available2008-09-12T08:18:51Z
dc.date.issued2007
dc.identifier.citationAmerican Journal of Applied Sciences, vol. 4 (8), 2007, pages 543-546.en_US
dc.identifier.issn1546-9239
dc.identifier.urihttp://dspace.unimap.edu.my/123456789/2192
dc.identifier.urihttp://scipub.org/scipub/index.php
dc.descriptionLink to publisher's homepage at http://scipub.org/scipub/index.phpen_US
dc.description.abstractTemperature is an important parameter for transformation of minerals in clinker during cement productions. It influences the formation of alite from belite during calcinations and clinkering processes. The result of microstructure shows that the formation of belite minerals started at temperature nearly 1200°C which is at calcinations zone temperature, followed by formation of ß-belite at higher temperature (around 1300°C), then formation of ß-belite and finally, with the suitable conditions it will form alite minerals. The differences between minerals are identified physically using scanning electron microscope (SEM).en_US
dc.language.isoenen_US
dc.publisherScience Publicationsen_US
dc.subjectClinkeren_US
dc.subjectMicrostructureen_US
dc.subjectScanning electron microscopesen_US
dc.subjectBuilding materials -- Testingen_US
dc.subjectPortland cementen_US
dc.subjectPhase transformationsen_US
dc.titleComparative Characterization of Clinker’s Microstructure at Different Temperature Zone during Cement Productionen_US
dc.typeArticleen_US


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