Excerpt from Infiltration and Permeability of Weathered Crystalline Rocks, Georgia Nuclear Laboratory, Dawson County, Georgia<br/><br/>The ground-water velocity in the area, based on chloride and nitrate tracer tests, ranged from about feet per day to as much as 25 feet per day. Ground water velocities determined from the permeability and porosity of the material, and the hydraulic gradients in'the area, ranged from about foot to 3 feet per day.
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