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dc.contributor.advisorPetrik, Leslie
dc.contributor.advisorFatoba, Olanrewaju
dc.contributor.authorCornelius, Mero-Lee Ursula
dc.date.accessioned2016-09-22T09:13:18Z
dc.date.available2016-09-22T09:13:18Z
dc.date.issued2015
dc.identifier.urihttp://hdl.handle.net/11394/5232
dc.description>Magister Scientiae - MScen_US
dc.description.abstractCoal is the main source of electricity in South Africa, the combustion of which produces a large amount of waste (coal fly ash) annually. The large-scale generation of coal fly ash places major strain on landfills and the material is toxic in nature. The high silicon and aluminium content in fly ash makes it a suitable starting material for zeolite synthesis. Utilisation of fly ash as a starting material for zeolite synthesis alleviates an environmental burden by converting a waste product to an industrially applicable material. In this study, hierarchical zeolite X was synthesised from coal fly ash via the fusion method. The clear fused fly ash (FFA) extract (with molar composition 0.12 Al·14.6 Na·1.00 Si·163 H₂O) served as the synthesis solution for hydrothermal treatment. The influence of synthesis parameters (such as Si/Al ratio, aluminium source, hydrothermal temperature and stirring) on hierarchical zeolite X formation was studied to determine the cause behind the formation of this material. Synthesised zeolites and starting materials (Arnot coal fly ash and fused fly ash) were characterised by various analytical techniques such as XRD and SEM-EDS to determine the phase purity, morphology and elemental composition (framework Si/Al ratio) of these materials. The synthesis of hierarchical zeolite X under hydrothermal conditions was found to be highly sensitive to the aluminium content of the synthesis solution. The hierarchical morphology of zeolite X was formed preferentially in relatively aluminium-deficient (i.e. high Si/Al ratio) synthesis environments under stirred hydrothermal conditions of 90 °C for 16 hours. In the case of sodium aluminate addition, octahedral shaped zeolite X crystals were formed in relatively low Si/Al ratio synthesis environments, which was attributed to the presence of excess sodium cation content in the synthesis solution. Selected hierarchical zeolites (D2 and E2) were characterised further to gain more insight into the properties of this material. HR-TEM and FTIR revealed that hierarchical zeolite D2 and E2 exhibited the typical structural features of zeolite X. Zeolite D2 and E2 contained both micropores and mesopores and had a high BET surface area of 338-362 m²/g. These zeolites also exhibited appreciable solid acidity (0.81-1.12 mmol H/g zeolite). These properties make hierarchical zeolite X a favourable material for application in catalysis or adsorption. Overall, the formation of zeolite X with hierarchical morphology was proposed to be linked to the presence of zeolite P1 structural units in the framework of the zeolite.en_US
dc.description.sponsorshipNational Research Foundationen_US
dc.language.isoenen_US
dc.publisherUniversity of the Western Capeen_US
dc.subjectCoal fly ashen_US
dc.subjectZeolite synthesisen_US
dc.subjectZeolitesen_US
dc.subjectHierarchical zeolite Xen_US
dc.subjectFly ashen_US
dc.titleThe role of aluminium content in the control of the morphology of fly ash based hierarchical zeolite Xen_US
dc.rights.holderUniversity of the Western Capeen_US


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