Mapping potential zones for groundwater recharge and its evaluation in arid environments using a GIS approach: Case study of North Gafsa Basin (Central Tunisia)

被引:40
|
作者
Mokadem, Naziha [1 ,5 ]
Boughariou, Emna [1 ]
Mudarra, Matias [2 ,3 ]
Ben Brahim, Fatma [1 ]
Andreo, Bartolome [2 ,3 ]
Hamed, Younes [4 ,5 ]
Bouri, Salem [1 ]
机构
[1] ENIS, Water Energy & Environm Lab L3E, St Soukra Km 3-5,BP W, Sfax 3038, Tunisia
[2] Univ Malaga CEHIUMA, Dept Geol, Malaga, Spain
[3] Univ Malaga CEHIUMA, Ctr Hydrogeol, Malaga, Spain
[4] Fac Sci Gabes, Georesources Geosyst & Geoenvironm 3G Lab, Zrig, Tunisia
[5] Fac Sci Gafsa, Int Assoc Water Resources Southern Mediterranean, Gafsa, Tunisia
关键词
Potential recharge zones; GIS; Gafsa; Aquifer; Groundwater; Recharge rate; CLIMATE-CHANGE; AQUIFER; EVOLUTION; ALGERIA; REGION; ATLAS; AREA;
D O I
10.1016/j.jafrearsci.2018.02.007
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
With the progressive evolution of industrial sector, agricultural, urbanization, population and drinking water supply, the water demand continuously increases which necessitates the planning of groundwater recharge particularly in arid and semi-arid regions. This paper gives a comprehensive review of various recharges studies in the North Gafsa basin (South Tunisia). This latter is characterized by a natural groundwater recharge that is deeply affected by the lack of precipitations. The aim of this study is to determine the recharge potential zones and to quantify (or estimate) the rainfall recharge of the shallow aquifers. The mapping of the potential recharge Tones was established in North Gafsa basin, using geological and hydrological parameters such as slope, lithology, topography and stream network. Indeed, GIS provide tools to reclassify these input layers to produce the final map of groundwater potential zones of the study area. The final output map reveals two distinct zones representing moderate and low groundwater potential recharge. Recharge estimations were based on the four methods: (1) Chloride Method, (2) ERAS Method, (3) DGRE coefficient and (4) Fersi equations. Therefore, the overall results of the different methods demonstrate that the use of the DGRE method applying on the potential zones is more validated. (C) 2018 Elsevier Ltd. All rights reserved.
引用
收藏
页码:107 / 117
页数:11
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