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dc.contributor.authorO'Connor, Gregory Michael
dc.contributor.supervisorJacques Eksteenen_US
dc.date.accessioned2019-06-19T03:46:27Z
dc.date.available2019-06-19T03:46:27Z
dc.date.issued2018en_US
dc.identifier.urihttp://hdl.handle.net/20.500.11937/75786
dc.description.abstract

The slow leach rate of copper from chalcopyrite in acid solutions has often been attributed to the formation of a poorly soluble “passive” layer on the surface. For this study, it has been shown that no such passive layer exists in alkaline glycine solutions. Surface analyses have shown these species exist, but are not passivating. The leach rate is instead determined by the electronic structure of chalcopyrite.

en_US
dc.publisherCurtin Universityen_US
dc.titleFundamentals of Chalcopyrite Dissolution in Alkaline Glycine Solutionsen_US
dc.typeThesisen_US
dcterms.educationLevelPhDen_US
curtin.departmentWASM: Minerals, Energy and Chemical Engineeringen_US
curtin.accessStatusOpen accessen_US
curtin.facultyScience and Engineeringen_US


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