Please use this identifier to cite or link to this item: http://dspace.unimap.edu.my:80/xmlui/handle/123456789/2192
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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
Appears in Collections:School of Environmental Engineering (Articles)
Kamarudin Hussin, Brig. Jen. Datuk Prof. Dr.
Khairul Nizar Ismail, Associate Professor Dr.
Mohd Sobri Idris, Associate Professor Ts. Dr.

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