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dc.contributor.author Cox, Rosemary Ann en_US
dc.date.accessioned 2012-05-10T21:14:05Z
dc.date.available 2012-05-10T21:14:05Z
dc.date.issued 1969 en_US
dc.identifier ocm72760729 en_US
dc.identifier.uri http://hdl.handle.net/1993/5598
dc.description.abstract A preliminary investigation was made into two aspects of the inter-relationships between groundwater discharge and streamflow in the Wilson Creek Watershed. The first aspect was to evaluate the relationships between the major dissolved ions in the stream (varying both with time and distance from the source) and the groundwater. The second was to attempt a baseflow separation of a peak-flow hydrograph using characterising groundwater ions. Sulphate was used as the characterising ion because of the evidence of its being representative of the groundwater. The stream water was found to be from local and not deep groundwater reservoirs, because of the downward hydraulic gradient in the piezometers, and their chemical characteristics. Consistent results utilising the relationships between the sulphate content and streamflow in calculating the groundwater discharge in a flood peak indicate that this method of baseflow separation is likely to be representative. This assumes a limited dilution of the groundwater component. en_US
dc.format.extent xii, 135 leaves : en_US
dc.language en en_US
dc.rights en_US
dc.title An investigation into the streamflow and groundwater hydrology of Wilson Creek, a small Manitoba watershed en_US
dc.degree.discipline Civil Engineering en_US


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