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dc.contributor.authorO'Brien, Kelsey, Elizabeth
dc.date.accessioned2013-08-23T13:26:58Z
dc.date.available2013-08-23T13:26:58Z
dc.date.issued2013-08-23
dc.identifier.urihttp://hdl.handle.net/10222/35468
dc.description.abstractThe relative contributions of bedrock geology, radiometric uranium, till permeability and surficial geology were assessed as predictors of radon in indoor air in the Halifax Regional Municipality (HRM), NS, Canada. Bedrock geology and radiometric uranium were statistically significant predictors (14.4%) of indoor radon, based on available indoor radon data. Permeability was not among the predictors, which was surprising given its importance in past studies. In a follow up field analogue study done in laboratory columns, the permeability and diffusivity, as gas transport mechanisms, were found, as suspected, to be important drivers on the concentrations of radon-222 detected. Given the variable thickness of till in the HRM (< 0.5 m to > 3 m), these experiments highlighted the significance of till thickness, composition, and permeability in predicting the radioactive radon-222 potential.en_US
dc.language.isoenen_US
dc.subjectradon gasen_US
dc.subjectpermeabilityen_US
dc.subjectdiffusivityen_US
dc.subjectsoil columnen_US
dc.subjecttillen_US
dc.subjectindoor radon potential mappingen_US
dc.titleRADON-222 POTENTIAL IN TILLS OF HALIFAX, NOVA SCOTIAen_US
dc.date.defence2013-08-14
dc.contributor.departmentDepartment of Earth Sciencesen_US
dc.contributor.degreeMaster of Scienceen_US
dc.contributor.external-examinerIan Spooneren_US
dc.contributor.graduate-coordinatorNick Culshawen_US
dc.contributor.thesis-readerAnne Marie Ryanen_US
dc.contributor.thesis-readerRebecca Jamiesonen_US
dc.contributor.thesis-supervisorDave Risk, Daniel Rainhamen_US
dc.contributor.ethics-approvalNot Applicableen_US
dc.contributor.manuscriptsYesen_US
dc.contributor.copyright-releaseNot Applicableen_US
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