Piece 3 - Recharge
How does water enter the aquifer?
How does water enter the aquifer?
Recharge is one of the most difficult components of the groundwater budget to quantify in semi-arid crystalline aquifers.
The double water table fluctuation method
A two-step method combining groundwater budgets and water-table fluctuations: the dry season is used to estimate specific yield, while the wet-season water-table rise is then converted into natural groundwater recharge.
Recharge cannot be represented as a uniform flux: it depends on climate, land use, soil properties, topography and preferential infiltration pathways.
Jean-Christophe Maréchal, Pierre Perrochet, Yvan Caballero
Hydrogeology Journal, vol. 31, 2023 Nov, pp. 1991--1995
Mapping Economic Feasibility of Managed Aquifer Recharge
Jean-Christophe Maréchal, Madjid Bouzit, Jean-Daniel Rinaudo, Fanny Moiroux, Jean-François Desprats, Yvan Caballero
Water, vol. 12, 2020
Laurent Ruiz, Murari R.R. Varma, M. S.Mohan Kumar, M. Sekhar, Jean-Christophe Maréchal, Marc Descloitres, Jean Riotte, Sat Kumar, C. Kumar, Jean Jacques Braun
Journal of Hydrology, vol. 380, 2010 Jan, pp. 460--472
Indirect and direct recharges in a tropical forested watershed: Mule Hole, India
Jean-Christophe Maréchal, Murari R R Varma, Jean Riotte, Jean-Michel Vouillamoz, M S Mohan Kumar, Laurent Ruiz, Muddu Sekhar, Jean-Jacques Braun
Journal of Hydrology, vol. 364, 2009 Jan, pp. 272--284
Jean-Christophe Maréchal, Benoit Dewandel, Shakeel Ahmed, Laurent Galeazzi, Faizal K Zaidi
Journal of Hydrology, vol. 329, 2006 Sep, pp. 281--293