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Gossel, W., Ebraheem, A. M., Wycisk, P. (2004) A very large scale GIS-based groundwater flow model for the Nubian sandstone aquifer in Eastern Sahara (Egypt, northern Sudan and eastern Libya). Hydrogeology Journal, 12 (6). 698-713 doi:10.1007/s10040-004-0379-4

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Reference TypeJournal (article/letter/editorial)
TitleA very large scale GIS-based groundwater flow model for the Nubian sandstone aquifer in Eastern Sahara (Egypt, northern Sudan and eastern Libya)
JournalHydrogeology Journal
AuthorsGossel, W.Author
Ebraheem, A. M.Author
Wycisk, P.Author
Year2004 (December)Volume12
Issue6
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/s10040-004-0379-4Search in ResearchGate
Generate Citation Formats
Mindat Ref. ID7675237Long-form Identifiermindat:1:5:7675237:9
GUID0
Full ReferenceGossel, W., Ebraheem, A. M., Wycisk, P. (2004) A very large scale GIS-based groundwater flow model for the Nubian sandstone aquifer in Eastern Sahara (Egypt, northern Sudan and eastern Libya). Hydrogeology Journal, 12 (6). 698-713 doi:10.1007/s10040-004-0379-4
Plain TextGossel, W., Ebraheem, A. M., Wycisk, P. (2004) A very large scale GIS-based groundwater flow model for the Nubian sandstone aquifer in Eastern Sahara (Egypt, northern Sudan and eastern Libya). Hydrogeology Journal, 12 (6). 698-713 doi:10.1007/s10040-004-0379-4
In(2004, December) Hydrogeology Journal Vol. 12 (6) Springer Science and Business Media LLC

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Ebraheem, A. M., Riad, S., Wycisk, P., Sefelnasr, A. M. (2004) A local-scale groundwater flow model for groundwater resources management in Dakhla Oasis, SW Egypt. Hydrogeology Journal, 12 (6). 714-722 doi:10.1007/s10040-004-0359-8
Sefelnasr, Ahmed, Gossel, Wolfgang, Wycisk, Peter (2015) Groundwater management options in an arid environment: The Nubian Sandstone Aquifer System, Eastern Sahara. Journal of Arid Environments, 122. 46-58 doi:10.1016/j.jaridenv.2015.06.009
Gossel, Wolfgang, Sefelnasr, Ahmed, Wycisk, Peter (2010) Modelling of paleo-saltwater intrusion in the northern part of the Nubian Aquifer System, Northeast Africa. Hydrogeology Journal, 18 (6). 1447-1463 doi:10.1007/s10040-010-0597-x
Voss, Clifford I., Soliman, Safaa M. (2014) The transboundary non-renewable Nubian Aquifer System of Chad, Egypt, Libya and Sudan: classical groundwater questions and parsimonious hydrogeologic analysis and modeling. Hydrogeology Journal, 22 (2). 441-468 doi:10.1007/s10040-013-1039-3
A., Ebraheem, S., Riad, P., Wycisk, El-Nasr, A. Seif (2002) Simulation of impact of present and future groundwater extraction from the non-replenished Nubian Sandstone Aquifer in southwest Egypt. Environmental Geology, 43 (1) 188-196 doi:10.1007/s00254-002-0643-7
Hussein, MohammedTahir (2004) Hydrochemical evaluation of groundwater in the Blue Nile Basin, eastern Sudan, using conventional and multivariate techniques. Hydrogeology Journal, 12 (2). doi:10.1007/s10040-003-0265-5
Calderón Palma, Heyddy, Bentley, Laurence R. (2007) A regional-scale groundwater flow model for the Leon-Chinandega aquifer, Nicaragua. Hydrogeology Journal, 15 (8). 1457-1472 doi:10.1007/s10040-007-0197-6
Mahmod, Wael Elham, Watanabe, Kunio, Zahr-Eldeen, Ashraf A. (2013) Analysis of groundwater flow in arid areas with limited hydrogeological data using the Grey Model: a case study of the Nubian Sandstone, Kharga Oasis, Egypt. Hydrogeology Journal, 21 (5). 1021-1034 doi:10.1007/s10040-013-0959-2
Sanford, WardE., Plummer, L.Niel, McAda, DouglasP., Bexfield, LauraM., Anderholm, ScottK. (2004) Hydrochemical tracers in the middle Rio Grande Basin, USA: 2. Calibration of a groundwater-flow model. Hydrogeology Journal, 12 (4). doi:10.1007/s10040-004-0326-4
Gemitzi, Alexandra, Tolikas, Demetrios (2004) Development of a sharp interface model that simulates coastal aquifer flow with the coupled use of GIS. Hydrogeology Journal, 12 (3). doi:10.1007/s10040-003-0295-z
Samie, S. Abd El, M., Sadek (2001) Groundwater recharge and flow in the Lower Cretaceous Nubian Sandstone aquifer in the Sinai Peninsula, using isotopic techniques and hydrochemistry. Hydrogeology Journal, 9 (4). 378-389 doi:10.1007/s100400100140
 
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