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DatoValore
TitleUSING INVERSE MODELLING TO REDUCE UNCERTAINTY ON THE RECHARGE TO AQUIFERS. THE CASE OF PETRIGNANO D'ASSISI (ITALY)
AbstractIn this paper we propose to reduce the uncertainty on the recharge of a porous regional aquifer, integrating its estimation with the results of the numerical simulation of different flow situations (both in stationary and transient conditions) using several sets of piezometric head data as targets for inverse problems. The methodology has been applied to the case study of Petrignano d'Assisi (Umbria, Italy).
SourceXXXV IAH CONGRESS - GROUNDWATER AND ECOSYSTEMS,, INTERNATIONAL ASSOCIATION OF HYDROGEOLOGISTS, LISBONA, september 2007
Year2007
TypeContributo in atti di convegno
AuthorsROMANO E., PREZIOSI E.
Text89505 2007 USING INVERSE MODELLING TO REDUCE UNCERTAINTY ON THE RECHARGE TO AQUIFERS. THE CASE OF PETRIGNANO D ASSISI ITALY ROMANO E., PREZIOSI E. Consiglio Nazionale delle Ricerche Istituto di Ricerca sulle Acque In this paper we propose to reduce the uncertainty on the recharge of a porous regional aquifer, integrating its estimation with the results of the numerical simulation of different flow situations both in stationary and transient conditions using several sets of piezometric head data as targets for inverse problems. The methodology has been applied to the case study of Petrignano d Assisi Umbria, Italy . XXXV IAH COngress Groundwater and Ecosystems Lisbon 2007 978 989 95297 3 1 XXXV IAH CONGRESS GROUNDWATER AND ECOSYSTEMS,, INTERNATIONAL ASSOCIATION OF HYDROGEOLOGISTS LISBONA september 2007 Internazionale Contributo 2007 IAH Conference Lisbon Romano and Preziosi Using inverse modelling to reduce uncertianty on the recharge to aquifers. The case of Petrignano d Assisi Italy 2007_IAH_Conference_Lisbon_Romano_and_Preziosi_Using_inverse_modelling_to_reduce_uncertianty_on_the_recharge_to_aquifers_The_case_of_Petrignano_d_Assisi_Italy_.pdf Contributo in atti di convegno emanuele.romano ROMANO EMANUELE elisabetta.preziosi PREZIOSI ELISABETTA TA.P02.009.002 Effetti dei cambiamenti climatici sulla componente terrestre del ciclo idrologico