EGU24-17047, updated on 11 Mar 2024
https://doi.org/10.5194/egusphere-egu24-17047
EGU General Assembly 2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

Evaluation and modelling of the impact of drought on groundwater reserves in Wallonia in the context of climate change

Julien Hutzemakers1, Philippe Orban1, Guillaume Vandelois2, Alain Dassargues1, Pascal Goderniaux2, and Serge Brouyère1
Julien Hutzemakers et al.
  • 1ULiège, Geological engineering, ArGenCo, Belgium (j.hutzemakers@uliege.be)
  • 2Université de Mons, Faculté Polytechnique, Géologie Fondamentale et Appliquée

Climate change has started to impact water resources in many regions and countries. Extreme events 
have become more frequent, with, in particular, severe winter or summer droughts that may affect 
groundwater reservoirs which are essential for drinking water. The exceptionally arid winters of 2016 
and 2017 in Wallonia (Belgium) opened discussions on the necessity to develop tools and indicators 
that allow quantifying such impacts and modelling the responses of aquifer systems to such events.


In this context, the objective here is to describe the methodology that has been developed in
Wallonia (Belgium). The approach relies on numerical groundwater flow models used to obtain 
trends in piezometric levels and groundwater balances using different specific drought scenarios.
Modelling results are used to compute spatial maps of maximal piezometric drawdowns and 
recovery times by comparing baseline and drought scenarios. Adopting a flow budget perspective, 
groundwater flow modelling results are also used to quantify indicators reflecting relative shifts in 
water transfers between aquifer recharge, rivers, adjacent aquifers and exploited groundwater water 
resources. 


The approach is illustrated using different strategic regional aquifers of Wallonia modelled using 
various numerical groundwater flow models able to compute groundwater budgets and simulate 
both the partially saturated and fully saturated zones of aquifers and the interactions with surface 
water courses. To assess the resilience of the groundwater bodies, three different scenarios were 
simulated: the first entailed a series of years with typical recharge levels, the second involved three 
consecutive years with the same recharge as in 2016-2017, followed by years with standard recharge 
rates, and the third replicated the second scenario but follows the three arid years with an 
exceptionally wet year.


Collectively these methodologies yield a better comprehension of drought impacts at a regional scale
both in terms of spatial variability and large-scale water transfers.

How to cite: Hutzemakers, J., Orban, P., Vandelois, G., Dassargues, A., Goderniaux, P., and Brouyère, S.: Evaluation and modelling of the impact of drought on groundwater reserves in Wallonia in the context of climate change, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-17047, https://doi.org/10.5194/egusphere-egu24-17047, 2024.