An integrated approach for aquifer characterization and groundwater productivity evaluation in the Lake Haramaya watershed, Ethiopia

Shishaye, Haile A.; Tait, Douglas R.; Befus, Kevin M.; Maher, Damien T.

An integrated approach for aquifer characterization and groundwater productivity evaluation in the Lake Haramaya watershed, Ethiopia | Une approche intégrée pour la caractérisation et l’évaluation de la productivité d’un aquifère dans le bassin versant du lac Haramaya, Ethiopie Un enfoque integrado para la caracterización de acuíferos y la evaluación de la productividad del agua subterránea en la cuenca del Lago Haramaya, Etiopía 埃塞俄比亚哈拉玛雅湖流域含水层特征和地下水生产力的综合评估方法 Uma abordagem integrada para caracterização de aquífero e avaliação da produtividade de água subterrânea na bacia do Lago Haramaya, Etiópia

2019

Shishaye, Haile A. | Tait, Douglas R. | Befus, Kevin M. | Maher, Damien T.

Accurate characterization of aquifers remains challenging for large-scale systems because of the spatial heterogeneity of hydraulic properties and temporal variability of hydrologic inputs. This study highlights the importance of integrating geological, hydrogeological and geophysical approaches to characterize an aquifer and evaluate groundwater productivity. Data from geological maps, drill logs, a pumping test, vertical electrical soundings (VES) and different field hydrogeological studies were combined and applied to a heavily extracted aquifer system—Lake Haramaya watershed, Ethiopia. From the geological characterization, the aquifer was found to be a single heterogeneous and anisotropic unconfined unit. Significant differences were found between the three-dimensional geological models of the aquifer developed from the drill logs and VES data; the VES data were likely affected by moisture content. The pumping-test and VES data were combined to estimate transmissivity (T; 126.5 ± 25.8 m²/day) and hydraulic conductivity (K; 4.1 ± 1.0 m/day). This combined use allowed for a reduction in uncertainty (40.1% for T and 33.3% for K) compared with values estimated from the VES data alone. The combined approach also allowed for much greater spatial coverage and a higher resolution characterization of the aquifer. The available volume of groundwater resource in the system was estimated at ~0.62 ± 0.09 km³. The groundwater extraction rate was ~30,120 m³/day, approximately double the estimated sustainable yield of the aquifer (15,720 m³/day). This showed that the current exploitation rate could exhaust groundwater resources in 27–32 years and should be reduced by 50% to ensure sustainability of the groundwater resource.

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