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Status of the Central Hays County Groundwater Evaluation. Brian A. Smith, Ph.D., P.G. Brian B. Hunt, P.G. Barton Springs/Edwards Aquifer Conservation District. Presentation to Hays County Commissioners Court April 7, 2015. Trinity Aquifer(s). TWDB 2009. Theis Equation.
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Status of the Central Hays CountyGroundwater Evaluation Brian A. Smith, Ph.D., P.G. Brian B. Hunt, P.G. Barton Springs/Edwards Aquifer Conservation District Presentation to Hays County Commissioners Court April 7, 2015
Theis Equation • A method for evaluating non-equilibrium, radial flow to a pumping well
Driscoll’s Comments on Theis Assumptions • These assumptions appear to limit severely the use of the two equations. In reality, however they do not. For example, uniform hydraulic conductivity is rarely found in a real aquifer, but the average hydraulic conductivity as determined from pumping tests has proven to be reliable for predicting well performance. Fletcher Driscoll, Groundwater and Wells, 1986