Three-dimensional groundwater flow modeling to assess the impacts of the increase in abstraction and recharge reduction on the groundwater, groundwater availability and groundwater-surface waters interaction: A case of the rib catchment in the Lake Tana sub-basin of the Upper Blue Nile River, Ethiopia

被引:15
作者
Mamo, Sileshi [1 ]
Birhanu, Behailu [2 ]
Ayenew, Tenalem [3 ]
Taye, Getnet [1 ]
机构
[1] Bahir Dar Univ, Sch Earth Sci, Dept Geol, POB 79, Bahir Dar, Ethiopia
[2] Addis Ababa Sci & Technol Univ, Coll Appl Sci, Geol Dept, POB 16417, Addis Ababa, Ethiopia
[3] Addis Ababa Univ, Sch Earth Sci, POB 1176, Addis Ababa, Ethiopia
关键词
Groundwater recharge; Groundwater flow; Groundwater-surface waters interaction; Modeling; Rib catchment; Ethiopia; CLIMATE-CHANGE; BASIN;
D O I
10.1016/j.ejrh.2021.100831
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Study region: Rib catchment in the Lake Tana sub-basin, Upper Blue Nile River, Ethiopia. Study focus: This paper aimed to assess the impacts of future increase in abstraction and recharge reduction on the groundwater, groundwater availability, and groundwater-surface waters interaction based on a three-dimensional groundwater flow modeling. Calibration was made under the steady state condition. Scenario analysis performed for 1) increase in abstraction, 2) decrease in recharge, 3) the worst-case scenario that combined the aforementioned two scenarios and with additional extraction for irrigation, and 4) for the optimal-case scenario, which considers 5% recharge increase for the worst-case scenario model. New hydrological insights for the region: It is found that the groundwater flows from uplands toward the Tana Lake. The total inflow to and outflow from the system in the calibrated model are 1733480 m(3)/d and 1840451 m(3)/d, respectively. Groundwater level drop, reduction in base flows to surface waters, and in evapotranspiration flux compared to the calibrated values encountered for all scenarios, which are significant (mean 38.4 m, 28.5-100 %, and 97.8 %, respectively) for the worst-case scenario. On the other hand, an increase in groundwater level (mean 9.8 m), base flows (0-14.4 %), and evapotranspiration flux (29.5 %) observed for the optimal scenario when compared to the worst-case scenario results. Results suggest that groundwater management measures should be implemented to mitigate the impacts.
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页数:17
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