| dc.description.abstract |
Appropriate quantification and identification of the groundwater distribution in a hydrological
basin may provide necessary information for effective management, planning and development of
groundwater resources. Groundwater potential assessment and delineation in a highly heterogeneous
environment with limited Spatiotemporal data derived from Gelana watershed of Abaya Chamo lake basin
is performed, using integrated multi-criteria decision analysis (MCDA), water and energy transfer between
soil and plant and atmosphere under quasi-steady state (WetSpass) models. The outputs of the WetSpass
model reveal a favorable structure of water balance in the basin studied, mainly using surface runoff. The
simulated total flow and groundwater recharge are validated using river measurements and estimated
baseflow at two gauging stations located in the study area, which yields a good agreement. The WetSpass
model effectively integrates a water balance assessment in a geographical information system (GIS)
environment. The WetSpass model is shown to be computationally reputable for such a remote complex
setting as the African rift, with a correlation coefficient of 0.99 and 0.99 for total flow and baseflow at a
significant level of p-value<0.05, respectively. The simulated annual water budget reveals that 77.22% of
annual precipitation loses through evapotranspiration, of which 16.54% is lost via surface runoff while
6.24% is recharged to the groundwater. The calibrated groundwater recharge from the WetSpass model is
then considered when determining the controlling factors of groundwater occurrence and formation,
together with other multi-thematic layers such as lithology, geomorphology, lineament density and drainage
density. The selected five thematic layers through MCDA are incorporated by employing the analytical
hierarchy process (AHP) method to identify the relative dominance in groundwater potential zoning. The
weighted factors in the AHP are procedurally aggregated, based on weighted linear combinations to provide
the groundwater potential index. Based on the potential indexes, the area then is demarcated into low,
moderate, and high groundwater potential zones (GWPZ). The identified GWPZs are finally examined
using the existing groundwater inventory data (static water level and springs) in the region. About 70.7% of
groundwater inventory points are coinciding with the delineated GWPZs. The weighting comparison shows
that lithology, geomorphology, and groundwater recharge appear to be the dominant factors influence on
the resources potential. The assessment of groundwater potential index values identify 45.88% as high,
39.38% moderate, and 14.73% as low groundwater potential zones. WetSpass model analysis is more
preferable in the area like Gelana watershed when the topography is rugged, inaccessible and having limited
gauging stations. |
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