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Groundwater Modelling of Motloutse Alluvial Aquifer, Eastern Botswana
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作者 Edwin O. Keaitse Nata T. Tafesse +2 位作者 berhanu F. Alemaw Kebabonye Laletsang read b. m. mapeo 《Journal of Water Resource and Protection》 CAS 2024年第10期627-639,共13页
The potential groundwater reserve in alluvial aquifers and sandy river beds has not been well studied, and yet their benefit in meeting rural water supply demands cannot be underestimated. A three-dimensional steady-s... The potential groundwater reserve in alluvial aquifers and sandy river beds has not been well studied, and yet their benefit in meeting rural water supply demands cannot be underestimated. A three-dimensional steady-state finite difference numerical groundwater flow model was used to assess the groundwater resource potential on a one-kilometre river stretch scale along the Motloutse River catchment in eastern Botswana. The model area is a single-layer unconfined aquifer system. A uniform grid was laid over this phreatic aquifer, and an overall size of 50 columns x 54 rows was developed. The model yielded calibrated K values of 145 m/day and 11 m/day for the riverbed and riverbank sediments, respectively, and calibrated recharge and evaporation of 172 mm/yr and 120 mm/yr, respectively. A sustainable groundwater yield of 120 m3/day with the potential to irrigate an area of 2.4 hectares was determined. The result also shows that the Motloutse alluvial aquifer yields a safe yield of 29,400 m3 for a kilometre of river stretch. 展开更多
关键词 Alluvial Aquifer GROUNDWATER Hydraulic Conductivity Motloutse River Eastern Botswana
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