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. Baratelli
Primo
;
M. Giudici
Penultimo
;
C. Vassena
Ultimo
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.
contaminant transport; ground water; hydrology; model calibration; porous media
Settore GEO/12 - Oceanografia e Fisica dell'Atmosfera
2010
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/2434/147097
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