Source, attenuation, and potential mobility of arsenic at New Britannia Mine, Snow Lake, MB

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dc.contributor.authorSimpson, Stephanie J.en_US
dc.date.accessioned2012-06-12T20:13:45Z
dc.date.available2012-06-12T20:13:45Z
dc.date.issued2007en_US
dc.degree.disciplineGeological Sciencesen_US
dc.degree.levelMaster of Science (M.Sc.)en_US
dc.description.abstractConcentrations of arsenic, averaging 17 ppm, are present in groundwater below a tailings disposal area, down gradient from an arsenopyrite residue stockpile (ARS) containing pore water concentrations of 100 ppm arsenic at New Britannia Mine (NBM), Snow Lake, Manitoba. Hydrogeological modeling illustrates arsenic contaminated groundwater will continue to percolate through the base of the ARS and into the local aquifer so long as there is a source concentration. Geochemical distribution of arsenic in surface and pore water (< 8.7 and 9.0 ppm), solids (< 17800 ppm), and plants (< 13600 ppm) along a flow path from the mine to Snow Lake are above Canadian guidelines. Safe levels of arsenic were measured in Snow Lake. Mineralogical investigations of solids by SEM, EMPA, and u-XRD show arsenic bound to secondary hydrous ferric oxides. Both dissolved and solid phase arsenic are mobile. Arsenic reducing bacteria thrive, thereby enhancing the conversion of arsenic to its more mobile and toxic form. Future monitoring and remediation recommendations for NBM are provided.en_US
dc.format.extent21124671 bytesen_US
dc.identifier(Sirsi) a1845151en_US
dc.identifier.urihttp://hdl.handle.net/1993/8027
dc.language.isoengen_US
dc.rightsopen accessen_US
dc.titleSource, attenuation, and potential mobility of arsenic at New Britannia Mine, Snow Lake, MBen_US
dc.typemaster thesisen_US
local.subject.manitobayesen_US
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