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dc.contributor.authorKhairul Nizar, Ismail
dc.contributor.authorKamarudin, Hussin
dc.contributor.authorMohd Sobri, Idris
dc.date.accessioned2009-08-21T03:57:14Z
dc.date.available2009-08-21T03:57:14Z
dc.date.issued2007
dc.identifier.citationJournal of Nuclear and Related Technologies, vol.4 (1-2), 2007, pages 47-51.en_US
dc.identifier.issn1823-0180
dc.identifier.urihttp://dspace.unimap.edu.my/123456789/6991
dc.descriptionLink to publisher's homepage at http://www.nuklearmalaysia.org/en_US
dc.description.abstractFly ash is the finely divided mineral residue resulting from the combustion of coal in electric generating plants. Fly ash consists of inorganic, incombustible matter present in the coal that has been fused during combustion into a glossy, amorphous structure. Fly ash particles are generally spherical in shape and range in size from 2 μm to 10 μm. They consist mostly of silicon dioxide(SiO2), aluminium oxide (Al2O3) and iron oxide (Fe2O3). Fly ash like soil contains trace concentrations of the following heavy metals: nickel, vanadium, cadmium, barium, chromium, copper,molybdenum, zinc and lead. The chemical compositions of the sample have been examined and the flyash are of ASTM C618 Class F.en_US
dc.language.isoenen_US
dc.publisherMalaysian Nuclear Societyen_US
dc.subjectFly ashen_US
dc.subjectScanning electron microscope (SEM)en_US
dc.subjectXRFen_US
dc.subjectXRDen_US
dc.subjectChemical propertiesen_US
dc.subjectIron oxide (Fe2O3)en_US
dc.subjectSilicon dioxide (SiO2)en_US
dc.titleChemical & Mineralogical Properties of Fly Ashen_US
dc.typeArticleen_US


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