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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

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Reference TypeJournal (article/letter/editorial)
TitleA local-scale groundwater flow model for groundwater resources management in Dakhla Oasis, SW Egypt
JournalHydrogeology Journal
AuthorsEbraheem, A. M.Author
Riad, S.Author
Wycisk, P.Author
Sefelnasr, A. M.Author
Year2004 (December)Volume12
Issue6
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/s10040-004-0359-8Search in ResearchGate
Generate Citation Formats
Mindat Ref. ID7675231Long-form Identifiermindat:1:5:7675231:5
GUID0
Full ReferenceEbraheem, 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
Plain TextEbraheem, 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
In(2004, December) Hydrogeology Journal Vol. 12 (6) Springer Science and Business Media LLC

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Sefelnasr, Ahmed, Gossel, Wolfgang, Wycisk, Peter (2014) Three-dimensional groundwater flow modeling approach for the groundwater management options for the Dakhla oasis, Western Desert, Egypt. Environmental Earth Sciences, 72 (4). 1227-1241 doi:10.1007/s12665-013-3041-4
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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
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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
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