Groundwater surface water interactions in a wetland rich, low relief Boreal environment

dc.contributor.authorTattrie, Kevin
dc.contributor.supervisorGibson, John J.
dc.date.accessioned2011-08-04T17:38:36Z
dc.date.available2011-08-04T17:38:36Z
dc.date.copyright2011en_US
dc.date.issued2011-08-04
dc.degree.departmentDepartment of Geography
dc.degree.levelMaster of Science M.Sc.en_US
dc.description.abstractThis study investigates surface water and groundwater interactions in a wetland/peatland region surrounding Fort McMurray, Alberta. This work measured local meteorology, water table variation, and isotope and geochemistry concentrations over a two year period. Results from vertical water budget calculations showed episodic runoff events ranging between 0 and 38 mm/yr. Groundwater evaluations showed limited groundwater gradients with mean hydraulic conductivities of 1.01*10-5 cms-1 (NE7) and 1.78 * 10-5 cms-1 (SM8). Overall, groundwater flux estimates were variable and heterogeneous across the catchments areas. Isotopic composition showed mixing between winter precipitation, groundwater and surface water, with groundwater representing the average input signature. This study showed that runoff events were largely associated with spring freshet and significant summer storm events.en_US
dc.description.scholarlevelGraduateen_US
dc.identifier.urihttp://hdl.handle.net/1828/3439
dc.languageEnglisheng
dc.language.isoenen_US
dc.rights.tempAvailable to the World Wide Weben_US
dc.subjectwetlandsen_US
dc.subjectgroundwateren_US
dc.subjectsurface wateren_US
dc.subjecthydrologyen_US
dc.subjectisotopesen_US
dc.subjectBorealen_US
dc.subjectFort McMurrayen_US
dc.titleGroundwater surface water interactions in a wetland rich, low relief Boreal environmenten_US
dc.typeThesisen_US

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