The DS method is applied to a regional aquifer which consists of two confined aquifers separated by a semipermeable layer. We use the results of a previously calibrated forward model of this real aquifer system as data for the DS method and we reconstruct the spatial distribution of the aquifers transmissivity and the leakage coefficient.
Identification of hydrodynamic parameters for a regional multilayered aquifer with the DS method / B. Ortuani, M. Giudici, F. Savi - In: Modelling of transport processes in soils at various scales in time and space / [a cura di] J. Feyen, K. Wiyo. - Wageningen : Wageningen Pers, 1999. - ISBN 9074134769. - pp. 467-475 (( convegno Modelling of transport processes in soils at various scales in time and space tenutosi a Leuven nel 1999.
Identification of hydrodynamic parameters for a regional multilayered aquifer with the DS method
B. OrtuaniPrimo
;M. GiudiciSecondo
;
1999
Abstract
The DS method is applied to a regional aquifer which consists of two confined aquifers separated by a semipermeable layer. We use the results of a previously calibrated forward model of this real aquifer system as data for the DS method and we reconstruct the spatial distribution of the aquifers transmissivity and the leakage coefficient.
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