Groundwater recharge/discharge in semi-arid regions interpreted from isotope and chloride concentrations in north White Nile Rift, Sudan
- 15 November 2008
- journal article
- Published by Springer Science and Business Media LLC in Hydrogeology Journal
- Vol. 17 (3), 679-692
- https://doi.org/10.1007/s10040-008-0388-9
Abstract
No abstract availableKeywords
This publication has 20 references indexed in Scilit:
- Groundwater discharge mechanism in semi‐arid regions and the role of evapotranspirationHydrological Processes, 2007
- Aquifer systems in Kordofan, Sudan: Subsurface lithological modelSouth African Journal of Geology, 2006
- Using environmental isotopes in the study of the recharge-discharge mechanisms of the Yarmouk catchment area in JordanHydrogeology Journal, 2004
- Indian Ocean Climate event brings floods to East Africa's lakes and the Sudd MarshGeophysical Research Letters, 1999
- Mesozoic and early Tertiary rift tectonics in East AfricaTectonophysics, 1992
- Tracing of water movement in the unsaturated zone using stable isotopes of hydrogen and oxygenJournal of Hydrology, 1988
- The relationship between 18O and deuterium in water in sand columns undergoing evaporationJournal of Hydrology, 1982
- Late Quaternary history of the NileNature, 1980
- Two plates in Africa during the Cretaceous?Nature, 1974
- Isotopic Variations in Meteoric WatersScience, 1961