Assessment of soil water movement and the relative importance of shallow subsurface flow in a near-level Prairie watershed

dc.contributor.authorRoss, Cody
dc.contributor.examiningcommitteeLobb, David (Soil Sciences) Casson, Nora (University of Winnipeg)en_US
dc.contributor.supervisorAli, Genevieve (Geological Sciences)en_US
dc.date.accessioned2017-01-20T15:02:23Z
dc.date.available2017-01-20T15:02:23Z
dc.date.issued2016
dc.degree.disciplineGeological Sciencesen_US
dc.degree.levelMaster of Science (M.Sc.)en_US
dc.description.abstractNear-level Prairie landscapes have received limited attention in hydrological research. For this thesis, hydrometric measurements and four tracing experiments were completed at three “riparian-to-stream” sites in the Catfish Creek Watershed (southeastern Manitoba) to enhance Prairie hydrology understanding. First, hydrologic state variables were examined to infer vertical and lateral water movement. Second, tracer data were analyzed to evaluate the relative importance of surface versus subsurface water movement. Results show that hydrologic state variables can be useful for inferring riparian-to-stream water movement. Tracer data also revealed that subsurface water movement can contribute significantly to streamflow during snowmelt- and rainfall-triggered events in the study watershed. This thesis demonstrated that subsurface flow is a significant runoff generation mechanism in Prairie landscapes, thus challenging surface water-focused conceptualizations and management strategies that are traditionally used. The findings summarized in this thesis will be critical to improve the performance of hydrological models when applied to the Prairies.en_US
dc.description.noteFebruary 2017en_US
dc.identifier.urihttp://hdl.handle.net/1993/32058
dc.language.isoengen_US
dc.rightsopen accessen_US
dc.subjectHydrology, runoff generation, hydrograph separation, stable water isotopes, fluorescent dye tracers, antecedent moisture conditions, tracer breakthrough curves, subsurface flowen_US
dc.titleAssessment of soil water movement and the relative importance of shallow subsurface flow in a near-level Prairie watersheden_US
dc.typemaster thesisen_US
local.subject.manitobayesen_US
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