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UID:pretalx-flowpath-2025-7DKC9X@talks.staging.osgeo.org
DTSTART;TZID=CET:20250611T145000
DTEND;TZID=CET:20250611T150000
DESCRIPTION:In the AMARONE project\, funded by the Cohesion and Development
  Fund (FSC 2014-2023)\, a regional-scale numerical model was developed to 
 comprehensively assess the hydrogeological water balance in the High and M
 iddle Venetian plains. The partnership between the Department of Geoscienc
 es of the University of Padova and the Eastern Alps River Basin District A
 uthority aimed to develop a valuable tool for water management to support 
 public authorities\, in accordance with the European Community’s Water F
 ramework Directive (WFD) that promotes sustainable water use and its long-
 term protection. 	\nThe implemented numerical model extends from the Minci
 o River to the Tagliamento River\, covering an area of about 6100 km2 cros
 sed by a dense network of alpine rivers\, spring rivers and artificial cha
 nnels. This area is characterized by the transition from the unconfined aq
 uifer system on gravelly materials of the high plain to the multiaquifer s
 ystem of the low plain\, primarily composed of gravelly-sandy confined aqu
 ifers separated by silty-clayey aquitards. The transition between these hy
 drogeological provinces is marked by a plain spring belt and the groundwat
 er exploitation in the region is a crucial factor for both social and econ
 omic reasons\, as evidenced by the abundant extraction through pumping wel
 ls estimated at 2351.4 M m3/year\, primarily used for drinking\, domestic\
 , irrigation and industrial purposes.	 \nThis complex situation was simula
 ted using a three-dimensional finite-difference numerical model based on t
 he MODFLOW-NWT code\, implementing and calibrating a steady-state simulati
 on to represent the average behavior of the system in the period 2010-2022
 \, based on the results of the previously developed monodimensional water 
 balance. This approach allowed the integration of hydrogeological data int
 o the balance\, such as hydraulic heads and hydraulic conductivity\, resul
 ting in a numerical model useful for performing balances on the water bodi
 es of the Veneto region.
DTSTAMP:20260428T165433Z
LOCATION:Room R3
SUMMARY:Hydrogeological water balance in the high and middle venetian plain
  defined through a regional-scale numerical model (NE\, Italy) - Davide Ca
 ppellari
URL:https://talks.staging.osgeo.org/flowpath-2025/talk/7DKC9X/
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