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Hydrogeology and groundwater flow in a basalt-capped Mesozoic sedimentary series of the Ethiopian highlands |
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| Authors: | Ine Vandecasteele Jan Nyssen Wim Clymans Jan Moeyersons Kristine Martens Marc Van Camp Tesfamichael Gebreyohannes Florimond Desmedt Jozef Deckers Kristine Walraevens |
| Institution: | 1. Royal Museum for Central Africa, Leuvensesteenweg 13, 3080, Tervuren, Belgium 2. Laboratory for Applied Geology and Hydrogeology, Ghent University, Krijgslaan 281-S8, 9000, Gent, Belgium 3. Department of Geography, Ghent University, Krijgslaan 281-S8, 9000, Gent, Belgium 4. Physical and Regional Geography Research Group, KU Leuven, Redingenstraat 16, 3000, Leuven, Belgium 5. Mekelle University, PO Box 231, Mekelle, Ethiopia 6. Hydrology Department, Free University of Brussels, Pleinlaan 2, 1050, Brussels, Belgium 7. Department of Earth and Environmental Sciences, Division for Land and Water Management, KU Leuven, Celestijnenlaan 200E, 3001, Leuven, Belgium |
| Abstract: | A hydrogeological study was undertaken in the Zenako-Argaka catchment, near Hagere Selam in Tigray, northern Ethiopia, during the rainy season of 2006. A geological map was produced through geophysical measurements and field observations, and a fracture zone identified in the north west of the catchment. A perched water table was found within the Trap Basalt series above the laterized upper Aram Aradam Sandstones. A map of this water table was compiled. Water-level variation during the measurement period was at least 4.5?m. Variation in basal flow for the whole catchment for the measurement period was between 12 and 276?m3/day. A groundwater flow model was produced using Visual MODFLOW, indicating the general direction of flow to be towards the south, and illustrating that the waterways have only a limited influence on groundwater flow. The soil water budget was calculated for the period 1995?C2006, which showed the important influence of the distribution of rainfall in time. Although Hagere Selam received some 724?mm of rainfall per year over this period, the strong seasonal variation in rainfall meant there was a water deficit for on average 10?months per year. |
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