Abstract
Most field methods used to estimate transmissivity values rely on the analysis of radial flow towards a single point (pump tests). Using a perturbation approach, we present an analytical solution to the problem of equivalent transmissivity (T eq ) under radially convergent steady-state flow conditions produced by constant pumping from a well of radius r w . In this context T eq is defined as the value that best fits Thiem’s equation, and would be the transmissivity assigned to the well location in a pump test. Using a Green’s function technique, we derive an expression for T eq , up to second-order in the expansion, which is given as a weighted average of the fluctuations in log-T throughout the domain. Previous work (Desbarats, 1992) hypothesized, based on empirical evidence, that the weighting function for log-T eq could be written as a function of the log-T fluctuations normalized by the square of their distance from the well. We find that this is indeed the case, although our second-order terms differ from that of Desbarats. We conclude with a highly heterogeneous example that illustrates the relative ranges over which the empirical formula and our second order expansion are accurate.
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© 1997 Springer Science+Business Media Dordrecht
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Sánchez-Vila, X., Axness, C.L., Carrera, J. (1997). Equivalent Transmissivities in Heterogeneous Porous Media under Radially Convergent Flow. In: Soares, A., Gómez-Hernandez, J., Froidevaux, R. (eds) geoENV I — Geostatistics for Environmental Applications. Quantitative Geology and Geostatistics, vol 9. Springer, Dordrecht. https://doi.org/10.1007/978-94-017-1675-8_1
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DOI: https://doi.org/10.1007/978-94-017-1675-8_1
Publisher Name: Springer, Dordrecht
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