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What will become of our groundwater reserves as a result of climate change?
While many of the potential consequences of climate change have already been studied, little research has been carried out up until now on groundwater sources. Civil engineer and geologist, Pascal Goderniaux, published a methodology to estimate the impact of climate change on groundwater reserves in the Journal of Hydrology. The application he proposes concerns the Hesbaye region or the Geer basin (1). The proposed methodology can be applied anywhere in the world. ![]() The Geer basin, to which the young researcher from Liège applied his methodology within the framework of his doctoral thesis, covers approximately 465 km2. The source of this tributary of the Meuse is close to Waremme and joins the Meuse just after the Dutch border, beyond Kanne. The region’s groundwater is stored in the thick layers of chalk formations dating from the Cretaceous period, in the pores and fractures of the rock. These chalk formations lie on a relatively impermeable layer of clay. Above the chalk formations, a thick layer of silt acts as a buffer and filter. ![]()
(1) Goderniaux, P ., Brouyere, S., Fowler, H.J., Blekinsop, S., Therrie,n, R., Orban, P., Dassargues, A., Large scale surface-subsurface hydrological model to assess climate change impacts on groundwater reserves, Journal of Hydrology (2009), doi: 10.1016/j.jhydrol.2009.04.017 |
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