The transport of contaminants in the subsurface is controlled by the heterogeneity of the hydraulic conductivity field. In order to emphasize some basic properties of transport phenomena in alluvial aquifers, a set of numerical experiments has been conducted on three blocks of sediments representing typical features of subsurface aquifer bodies.
Solute transport in geological porous media : estimation of dispersion coefficients / F. Baratelli, L. Cattaneo, M. Giudici, C. Vassena. - In: PROCEDIA: SOCIAL & BEHAVIORAL SCIENCES. - ISSN 1877-0428. - 2:6(2010), pp. 7605-7606. ((Intervento presentato al 6. convegno Sensitivity Analysis of Model Output tenutosi a Milano nel 2010 [10.1016/j.sbspro.2010.05.139].
Solute transport in geological porous media : estimation of dispersion coefficients
F. BaratelliPrimo
;M. GiudiciPenultimo
;C. VassenaUltimo
2010
Abstract
The transport of contaminants in the subsurface is controlled by the heterogeneity of the hydraulic conductivity field. In order to emphasize some basic properties of transport phenomena in alluvial aquifers, a set of numerical experiments has been conducted on three blocks of sediments representing typical features of subsurface aquifer bodies.
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