Overview:
Recharge and discharge fluxes are critical parameters
for understanding, modeling and protecting groundwater systems from
overexploitation and contamination. Local-scale
sites are characterized by integrating tools from hydrogeology (slug
and pumping tests), structural geology (fracture mapping), and geochemistry
(stable isotopes and radioisotopes). Regional flow modeling is constrained
by local-scale data, remote sensing, regional geochemistry and water
well data.
Additional Information:
-Groundwater recharge in bedrock aquifers: rapid, localized and
limited. Oral presentation at GSA 2007 Annual Meeting, Denver, October
28-31, 2007. [abstract]
-Identifying watershed-scale barriers to groundwater flow in the
Canadian Shield. Oral presentation at 8th Joint CGS/IAH-CNC Groundwater
Conference, Ottawa, October 21-24, 2007.[abstract]
-Insignificant groundwater discharge in a fractured rock watershed.
Oral presentation at 2007 NGWA/U.S. EPA Fractured Rock Conference,
Portland, Maine, September 24-27, 2007.[abstract]
-Lineaments as
groundwater barriers in a fractured rock aquifer. Oral presentation
at GSA Annual conference, October 2006, Philadelphia. [abstract]
[presentation]
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Tom Gleeson
PhD (2005- ) website |