An Approach to Understand Water Quality Trends in Groundwater in the Columbia Plateau, Washington, Oregon and Idahi

Friday, September 9, 2016: 9:55 a.m.
Terrence Conlon , Oregon Water Science Center, U.S. Geological Survey, Portland, OR

Groundwater of the Columbia Plateau basaltic aquifer in Washington, Oregon, and Idaho was sampled as part of an assessment of water-quality in principal aquifers of the United States conducted the U.S. Geological Survey National Water-Quality Assessment Project. The Columbia Plateau principal aquifer consists of the basaltic rocks of the Columbia River Basalt Group. Water from approximately 60 wells in Oregon, Washington, and Idaho was collected and analyzed using nationally consistent protocols for a suite of constituents including major ion chemistry, nutrients, radiochemistry, volatile organic compounds, pesticides, pharmaceuticals, trace elements, stable isotopes of water, and age-tracers. The groundwater quality information will be used to understand water quality for comparison with past and future conditions, evaluate horizontal and vertical variation in water quality, and assess the source, age, and sustainability of groundwater supplies.

Terrence Conlon, Oregon Water Science Center, U.S. Geological Survey, Portland, OR
Terrence Conlon has more than 25 years of experience with the USGS conducting water resource studies in Wisconsin and Oregon. His focus is on understanding groundwater hydrology, including the interactions of groundwater and surface waters, in areas experiencing competing water demands. He has experience using geophysics, process-based models, and a wide range of data to improve the understanding of groundwater conditions and the effects of changes to land use, climate, and water use on water resources. In his current role as a supervisory hydrologist, he oversees a wide range of studies in groundwater and surface-water availability.