HR: 11:55h
AN: H42B-07 INVITED     [Abstracts]
TI: Hydrogeophysics in an Alpine Watershed: Lake O'Hara, Canadian Rocky Mountains
AU: * Bentley, L R
EM: lbentley@ucalgary.ca
AF: University of Calgary, Department of Geology & Geophysics University of Calgary, Calgary, AB T2N 1N4, Canada
AU: Hayashi, M
EM: hayashi@ucalgary.ca
AF: University of Calgary, Department of Geology & Geophysics University of Calgary, Calgary, AB T2N 1N4, Canada
AU: Roy, J
EM: Jim.Roy@ec.gc.ca
AF: National Hydrology Research Institute, Canada Centre for Inland Waters 867 Lakeshore Rd, Burlington, ON L7R 4A6, Canada
AB: Alpine watersheds are the headwaters of major rivers in western Canada and many other regions in the world. Consequently, understanding the storage, flow paths and timing of the release of water is an important aspect of water resources management. Recent studies have shown that groundwater stored in moraines, talus slopes and alpine meadows are important water reservoirs in the Canadian Rocky Mountains. A research program in the Lake O'Hara Research Basin, Yoho National Park is characterizing the hydrologic cycle within this alpine watershed. Bedrock topography, preferential flow paths and the internal structure of the subsurface play a fundamental role in determining the volume and timing of groundwater discharge. Geophysical methods are needed to help delineate the subsurface, because drilling is not an option. A preliminary survey using electrical resistivity imaging (ERI) was conducted in the summer of 2006. ERI profiles were run across a small wetland in an alpine meadow and over the nose of a glacial moraine. Much of the surfaces consisted of dry rock rubble and boulders, so contact resistance was at times as high as several hundred thousand ohms. To establish electrical contact, we drove spikes into sponges saturated with salt water that were forced into boulder contacts. Another enhanced contact strategy was to smear medical contact jell over boulder surfaces and connect an electrode to aluminum foil plastered onto the jell. The survey was conducted with an 800 V transmitter, a Wenner array and an electrode spacing of 2 to 5 m. Due to the resistive environment, currents as small as 1 mA produced measured potentials in the volt range. Due to the contact difficulties, some electrode locations were offset one or more meters from the preferred array location and this offset may cause some distortion in the inverted images. The data produced inversions with resistivity values ranging from 500 ohm-m to 100,000 ohm-m. The lowest resistivity values correspond to wetlands and the saturated outflow at the toe of the moraine. The highest resistivity values correspond to dry bolder fields at the surface of the moraine. Bedrock appears to be in the 10,000 to 40,0000 ohm-m range. Although interpretation ambiguities exist in some portion of the images, the wetland is seen to be on the order of 2 m deep and overlies bedrock. In the moraine, discrete zones of groundwater flow have been identified. These results are consistent with water chemistry results that indicate that groundwater discharging from the toe of the moraine comes from more than one source.
DE: 1835 Hydrogeophysics
DE: 1859 Rocks: physical properties
DE: 1895 Instruments and techniques: monitoring
SC: Hydrology [H]
MN: 2007 Joint Assembly