Abstract
The tracer test is one of the few experimental tools capable of estimating transport parameters at the local scale. Models used to estimate transport parameters (such as dispersivity) generally assume a homogeneous conductivity field. However, the distribution of the solute plume in heterogeneous media is primarily determined by the statistical nature of the hydraulic conductivity at the scale of the plume. We numerically simulate 2D transport of particles introduced into a steady injection well with prescribed head boundary conditions at the wellbore and at an exterior circle. We compute the travel time distribution of particles introduced into the well to points along a control circle of a given radius within a single transmissivity realization. In particular, we look at the effect of high, low, or average local wellbore transmissivity (as compared to the mean transmissivity of the domain) on the travel time distribution of each realization. We conclude that the difference between the logtransmissivity at the wellbore and the domain average logtransmissivity is likely to play an important role in the interpretation of dispersivity from conventional tracer tests.
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© 2004 Kluwer Academic Publishers
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Axness, C.L., Gómez-Hernández, J.J., Carrera, J. (2004). 2D Particle Tracking Under Radial Flow in Heterogeneous Media Conditioned at the Well. In: Sanchez-Vila, X., Carrera, J., Gómez-Hernández, J.J. (eds) geoENV IV — Geostatistics for Environmental Applications. Quantitative Geology and Geostatistics, vol 13. Springer, Dordrecht. https://doi.org/10.1007/1-4020-2115-1_16
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DOI: https://doi.org/10.1007/1-4020-2115-1_16
Publisher Name: Springer, Dordrecht
Print ISBN: 978-1-4020-2007-0
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