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- W1134667424 abstract "When pumping from a single well in a real (heterogeneous) aquifer, the steady state drawdown at the well is proportional to the pumping rate through a value called the equivalent transmissivity, T eq , which, in short, is the value that best suits Thiem's formula. Equivalent transmissivity is not a local value, but some representative value of a certain area surrounding the well. By means of numerical simulations we study the validity of a recent analytical formula (Sanchez-Vila et al., 1999) that provides a value for T eq which is given as a weighted average of the fluctuations in log T throughout the domain. The formula is found to work acceptably well for mildly heterogeneous T fields." @default.
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- W1134667424 date "2000-01-01" @default.
- W1134667424 modified "2023-10-17" @default.
- W1134667424 title "Upscaling transmissivity under radially convergent flow" @default.
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