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Please use this identifier to cite or link to this item: http://hdl.handle.net/11375/18524
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dc.contributor.advisorNicholson, P. S.-
dc.contributor.authorLenz, John-
dc.date.accessioned2015-11-04T19:05:30Z-
dc.date.available2015-11-04T19:05:30Z-
dc.date.issued1975-02-
dc.identifier.urihttp://hdl.handle.net/11375/18524-
dc.description.abstract<P> This thesis is concerned with the investigation of the diffusion controlled reaction between MgO and β-quartz in the temperature range 1200 - 1450 °C in wet and dry atmospheres. The reactions were studied by placing known faces of quartz crystals in direct contact with Mg0 powder, heat treating them, and then investigating the cross sections. The product layer was investigated by both reflected light and thin section metallography, electron - microprobe and X- ray diffraction. Using Wagner's and Schmalzried's ideas on solid state reactions, a theoretical model for the diffusion controlled formation of silicates was developed. With this model, a mechanism for the diffusion controlled formation of forsterite from MgO and β-quartz was advanced. </P>en_US
dc.language.isoenen_US
dc.subjectdiffusionen_US
dc.subjectMgoen_US
dc.subjectΒ-Quartzen_US
dc.subjectcontrolled reactionen_US
dc.subjectheat treatingen_US
dc.subjectformation of silicatesen_US
dc.titleThe Diffusion Controlled Reaction Between MgO and Β-Quartzen_US
dc.contributor.departmentMaterials Scienceen_US
dc.description.degreetypeThesisen_US
dc.description.degreeMaster of Science (MSc)en_US
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