Assessment of Groundwater Quality and the Main Controls on Its Hydrochemistry in a Changing Climate in Morocco (Essaouira Basin)

被引:9
|
作者
El Mountassir, Otman [1 ]
Bahir, Mohammed [1 ,2 ]
Chehbouni, Abdelghani [2 ,3 ]
Dhiba, Driss [2 ]
El Jiar, Hicham [2 ]
机构
[1] Cadi Ayyad Univ, Fac Sci Semlalia, High Energy & Astrophys Lab, POB 2390, Marrakech 40000, Morocco
[2] Mohammed VI Polytech Univ, Int Water Res Inst, Ben Guerir 43150, Morocco
[3] Inst Rech Dev IRD, Unite Mixte Rech UMR, Ctr Etud Spatiales Biosphere Cesbio, F-31401 Toulouse, France
关键词
WQI; groundwater quality; Essaouira basin; IWQI; hydrogeochemical processes; irrigation; stable isotope; climate change; WATER-QUALITY; COASTAL AQUIFERS; STABLE-ISOTOPE; INDEX WQI; GIS; SALINIZATION; RESOURCES; EVOLUTION; COALFIELD; PORTUGAL;
D O I
10.3390/su14138012
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Groundwater is essential for both water supply and environmental conservation, especially in semi-arid and desert areas. Managing groundwater resources requires a thorough understanding of groundwater characteristics and dynamics. The hydrogeochemical properties and evolution of groundwater in the Essaouira synclinal basin in northwest Morocco were studied in this research, with 105 water samples collected in 2009, 2017, 2018, and 2019. The Water Quality Index (WQI) and Irrigation Water Quality Index (IWQI) were developed to determine groundwater quality for consumption and irrigation purposes. The chemical evolution of groundwater is mainly dominated by evaporite, mineral carbonate dissolutions, and cation exchange. Contamination by nitrates is particularly severe in agricultural and tourist areas. The WQI of the 2019 campaign showed that 6.7% of groundwater samples are unsuitable for drinking; 76.7% are poor quality water; and 13.3% are very poor-quality water; while only 3.3% are drinkable. According to IWQI, the total study area has been split into 50% (good), 43.3% (bad), and 6.6% (unfit), respectively, and no excellent groundwater areas have been identified. Therefore, the water is suitable for agriculture but must be treated for drinking. The presence of evaporation and maritime intrusion and the contribution of recent precipitations to aquifer recharging were demonstrated by stable isotope content.
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页数:31
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