Estimation of rainfall inputs and direct recharge to the deep unsaturated zone of southern Niger using the chloride profile method
References (27)
- et al.
Energy and woodland budgets of an area of patterned woodland in the Sahel
Agric. For. Meteorol.
(1993) - et al.
Estimating the spatial variability of groundwater recharge in the Sahel using chloride
J. Hydrol.
(1994) Filter-paper method for routine measurement of field water potential
J. Hydrol.
(1981)- et al.
Crust formation on sandy soils in the Sahel. I. Rainfall and infiltration
Soil Tillage Res.
(1984) A review of some of the physical, chemical and isotopic techniques available for estimating groundwater recharge
- et al.
The use of environmental chloride and tritium to estimate total recharge toan unconfined aquifer
Aust. J. Soil Res.
(1978) Contribution à l'édaphologie de la brousse tigrée de l'ouest Nigerien
La bordure orientale du plateau de Say. Etude géologique préliminaire
- et al.
Estimating Palaeorecharge from unsaturated zone profiles
Water Resour. Res.
(1992) - et al.
Spatiocarte des états de surface
(1992)
Groundwater recharge in Senegal
A geochemical and isotopic approach to recharge evaluation in semi-arid zones - past and present
Solute profile techniques for recharge estimation in semi-arid and arid terrain
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Groundwater recharge through internally drained basins in a semiarid climate, Western Australia
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2022, Journal of HydrologyCitation Excerpt :In these regions deep ‘fossil’ groundwaters recharged prior to the Holocene dominate aquifer stores (Sturchio et al., 2004; Guendouz et al., 2006; Abotalib et al., 2016; Jasechko et al., 2017). Groundwater recharge volumes are often biased towards the rainy season as elevated rainfall is required to overcome high rates of evapotranspiration (Bromley et al., 1997; Demlie et al., 2007; Walraevens et al., 2009; Mechal et al., 2015), and greater monthly and daily precipitation intensity leads to a more efficient conversion of rainfall to recharge (Jasechko and Taylor 2015; Owor et al. 2009; Taylor and Howard 1996). Groundwater level observations in the Makutapora wellfield, Tanzania, suggest that recharge is dependent upon months with the most extreme (>95th percentile) rainfall (Taylor et al., 2013b) often enhanced by the El Nino Southern Oscillation and the Indian Ocean Dipole.
Groundwater recharge using the chloride mass balance method in the Kanye area, in southeast Botswana
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