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dc.contributor.authorSemmens, Barrie
dc.contributor.otherSchool of Geography, Earth and Environmental Sciencesen_US
dc.date.accessioned2013-09-16T11:41:00Z
dc.date.available2013-09-16T11:41:00Z
dc.date.issued1965
dc.identifierNOT AVAILABLEen_US
dc.identifier.urihttp://hdl.handle.net/10026.1/1753
dc.description.abstract

The disruption of the aluminosilicate crystal lattice by aqueous fluoride solutions has been studied. The effect of reaction time, fluoride concentration, pH, and temperature on the reaction have been investigated. The stoichiometric exchange of hydroxyls by fluoride ions in kaolinite and muscovite at pH 7 and below was extremely doubtful. Disruption of the aluminosilicate crystal lattice was thought to be the predominant reaction over the acid pH range.

dc.language.isoenen_US
dc.publisherUniversity of Plymouthen_US
dc.titleDISRUPTION OF THE ALUMINOSILICATE LATTICE BY ACID FLUORIDE SOLUTIONSen_US
dc.typeThesis
plymouth.versionFull versionen_US
dc.identifier.doihttp://dx.doi.org/10.24382/4718
dc.identifier.doihttp://dx.doi.org/10.24382/4718


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