Quantitative Dye-Tracing of Karst Ground-Water Flowby James Smoot, US Geological Survey, United States,
Donald Mull, US Geological Survey, United States,
Timothy Liebermann, US Geological Survey, United States,
Abstract: Analysis of the results of repeat quantitative dye traces between a sinkhole and a spring used for public water supply were used to describe predictive relations between discharge, mean travel time, apparent ground-water flow velocity and solute transport characteristics. Normalized peak concentration, mean travel time, and standard deviation of travel times were used to produce a dimensionless, composite type curve that was used to produce a dimensionless, composite type curve that was used to simulate solute transport characteristics for selected discharges. Using this curve and previously developed statistical relations, a water manager can estimate the arrival time, peak concentration, and persistence of a soluble contaminant at a supply spring or well based on discharge and the quantity of spilled contaminant.
Subject Headings: Groundwater flow | Travel time | Water discharge | Water supply systems | Water flow | Fluid flow | Curvature
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