Quantifying morphology of nickel crystals.

dc.contributor.authorLewis, A
dc.contributor.authorRoberts, M
dc.date.accessioned2016-08-02T13:43:33Z
dc.date.available2016-08-02T13:43:33Z
dc.date.issued2001
dc.date.updated2016-08-02T08:48:52Z
dc.description.abstractParticle morphology is a term that is used to describe the overall external shape and appearance of particulate solids. From the physical point of view, a precipitated solid is characterized primarily by the size and morphology of the particles (Sohnel and Garside, 1992). If the morphology of the crystal structures is to be related to the processing conditions, then the morphologies need to be quantified in some way. This can be achieved by using surface area measurements as well as fractal dimensions. The key idea is that rugged and indeterminate systems can be described by using a fractional number that describes the ruggedness of the system (Kaye, 1989). In other words, when the complexity of a structure, such as an agglomerate, increases with increasing magnification, it is useful to employ fractal dimensions to describe the structure. Fractal geometry proposes that, instead of attempting to measure the length of an irregular boundary, the rate at which the length of the boundary approaches infinity with increasing resolution should be calculated. Cross-sectional profiles of rugged particles can thus be quantified using the fractal dimension, and a measurement of the ruggedness of the morphology obtained. One of the additional uses of measuring the fractal dimension is that the measured value can be related to the physical properties and formation characteristics of the particle (Kaye and Trottier, 1995).The morphology of nickel crystals was quantified with fractal dimension calculations of particle cross-sections. Particle crosssections were obtained by mounting the particles in resin and polishing back. These were then photographed using Scanning Electron Microscopy and the resulting profiles analysed using the structured walk technique.en_ZA
dc.identifier.apacitationLewis, A., & Roberts, M. (2001). Quantifying morphology of nickel crystals. <i>The Journal of The South African Institute of Mining and Metallurgy</i>, http://hdl.handle.net/11427/21100en_ZA
dc.identifier.chicagocitationLewis, A, and M Roberts "Quantifying morphology of nickel crystals." <i>The Journal of The South African Institute of Mining and Metallurgy</i> (2001) http://hdl.handle.net/11427/21100en_ZA
dc.identifier.citationLewis, A. E., & Roberts, M. (2001). Quantifying morphology of nickel crystals. Journal of the South African Institute of Mining and Metallurgy(South Africa), 101(8), 421-426.en_ZA
dc.identifier.issn0038-223Xen_ZA
dc.identifier.ris TY - Journal Article AU - Lewis, A AU - Roberts, M AB - Particle morphology is a term that is used to describe the overall external shape and appearance of particulate solids. From the physical point of view, a precipitated solid is characterized primarily by the size and morphology of the particles (Sohnel and Garside, 1992). If the morphology of the crystal structures is to be related to the processing conditions, then the morphologies need to be quantified in some way. This can be achieved by using surface area measurements as well as fractal dimensions. The key idea is that rugged and indeterminate systems can be described by using a fractional number that describes the ruggedness of the system (Kaye, 1989). In other words, when the complexity of a structure, such as an agglomerate, increases with increasing magnification, it is useful to employ fractal dimensions to describe the structure. Fractal geometry proposes that, instead of attempting to measure the length of an irregular boundary, the rate at which the length of the boundary approaches infinity with increasing resolution should be calculated. Cross-sectional profiles of rugged particles can thus be quantified using the fractal dimension, and a measurement of the ruggedness of the morphology obtained. One of the additional uses of measuring the fractal dimension is that the measured value can be related to the physical properties and formation characteristics of the particle (Kaye and Trottier, 1995).The morphology of nickel crystals was quantified with fractal dimension calculations of particle cross-sections. Particle crosssections were obtained by mounting the particles in resin and polishing back. These were then photographed using Scanning Electron Microscopy and the resulting profiles analysed using the structured walk technique. DA - 2001 DB - OpenUCT DP - University of Cape Town J1 - The Journal of The South African Institute of Mining and Metallurgy LK - https://open.uct.ac.za PB - University of Cape Town PY - 2001 SM - 0038-223X T1 - Quantifying morphology of nickel crystals TI - Quantifying morphology of nickel crystals UR - http://hdl.handle.net/11427/21100 ER - en_ZA
dc.identifier.urihttp://hdl.handle.net/11427/21100
dc.identifier.vancouvercitationLewis A, Roberts M. Quantifying morphology of nickel crystals. The Journal of The South African Institute of Mining and Metallurgy. 2001; http://hdl.handle.net/11427/21100.en_ZA
dc.languageengen_ZA
dc.publisherThe Southern African Institute of Mining and Metallurgyen_ZA
dc.publisher.institutionUniversity of Cape Town
dc.rightsCreative Commons Attribution 4.0 International (CC BY 4.0)*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/en_ZA
dc.sourceThe Journal of The South African Institute of Mining and Metallurgyen_ZA
dc.source.urihttp://www.scielo.org.za/revistas/jsaimm/iaboutj.htm
dc.titleQuantifying morphology of nickel crystals.en_ZA
dc.typeJournal Articleen_ZA
uct.type.filetypeText
uct.type.filetypeImage
uct.type.publicationResearchen_ZA
uct.type.resourceArticleen_ZA
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