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Rapid computation of directional wellbore drawdown in a confined aquifer via Poisson resummation
Institution:1. Texas Water Resources Institute, Texas A&M University, 1500 Research Parkway A110, College Station, TX 77843-2260, USA;2. Department of Geology and Geophysics, Texas A&M University, College Station, TX 77843-2260, USA;1. Department of Civil and Environmental Engineering, Universitat Politècnica de Catalunya (UPC), Jordi Girona 1-3, 08034 Barcelona, Spain;2. Institute of Environmental Assessment and Water Research (IDAEA), CSIC, Jordi Girona 18, 08034 Barcelona, Spain;3. Associated Unit: Hydrogeology Group (UPC-CSIC), Spain;1. Department of Earth Sciences, Uppsala University, Box 337, SE-751 05 Uppsala, Sweden;2. Department of Information Technology, Uppsala University, Box 337, SE-751 05 Uppsala, Sweden;3. Department of Mathematical Sciences, Chalmers University of Technology and University of Gothenburg, SE-412 96  Göteborg, Sweden
Abstract:We have derived a rapidly computed analytical solution for drawdown caused by a partially or fully penetrating directional wellbore (vertical, horizontal, or slant) via Green's function method. The mathematical model assumes an anisotropic, homogeneous, confined, box-shaped aquifer. Any dimension of the box can have one of six possible boundary conditions: 1) both sides no-flux; 2) one side no-flux – one side constant-head; 3) both sides constant-head; 4) one side no-flux; 5) one side constant-head; 6) free boundary conditions. The solution has been optimized for rapid computation via Poisson Resummation, derivation of convergence rates, and numerical optimization of integration techniques. Upon application of the Poisson Resummation method, we were able to derive two sets of solutions with inverse convergence rates, namely an early-time rapidly convergent series (solution-A) and a late-time rapidly convergent series (solution-B). From this work we were able to link Green's function method (solution-B) back to image well theory (solution-A). We then derived an equation defining when the convergence rate between solution-A and solution-B is the same, which we termed the switch time. Utilizing the more rapidly convergent solution at the appropriate time, we obtained rapid convergence at all times. We have also shown that one may simplify each of the three infinite series for the three-dimensional solution to 11 terms and still maintain a maximum relative error of less than 10?14.
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