Study of Hydrochemical Characteristics in the Middle Moulouya Basin of Morocco
			
	
 
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				1
				Laboratory of Engineering Sciences and Applications (LISA); Research Team: Materials Sciences, Energy and Environment (SM2E), ENSAH, Abdelmallek Essaâdi University, Al Hoceima, Morocco
				 
			 
						
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				Laboratory of Applied Geosciences (LAG); Research Team: Environmental Management & Civil Engineering (EMCE), ENSAH,  Abdelmallek Essaâdi University, Al Hoceima, Morocco
				 
			 
						
				3
				Laboratory of Geophysics and Natural Hazards, Scientific Institute, Geophysics, Heritage Center Natural “GEOPAC”, Mohammed-V University in Rabat, Morocco
				 
			 
										
				
				
		
		 
			
			
		
		
		
		
		
		
	
							
					    		
    			 
    			
    				    					Autor do korespondencji
    					    				    				
    					Omar  Saadi   
    					Laboratory of Engineering Sciences and Applications (LISA); Research Team: Materials Sciences, Energy and Environment (SM2E), ENSAH, Abdelmallek Essaâdi University, Al Hoceima, Morocco
    				
 
    			
				 
    			 
    		 		
			
																											 
		
	 
		
 
 
Ecol. Eng. Environ. Technol. 2024; 3:220-232
		
 
 
SŁOWA KLUCZOWE
DZIEDZINY
STRESZCZENIE
This study analyzes the effects of dry land salinity, climate severity, and pollution on groundwater quality in the Middle Moulouya basin. Our research provides insights into certain pollutants and their sources and discusses the impact of saline soil and dry weather. A comprehensive understanding of these factors is essential for managing water resources and promoting sustainable resource use in the area. In fact, the use of a database relating to the major elements, viz. potassium (K^+), calcium (〖Ca〗^(2+)), sodium (〖Na〗^(2+)), magnesium (〖Mg〗^(2+)), bicarbonates (〖HCO〗_3^-), sulfates 〖(SO〗_4^(2-)), nitrates (〖NO〗_3^-), chlorides 〖(Cl〗^-) has proved to be effective to assess the hydrochemical features of groundwaters and their suitability for both aims (i.e., irrigation and drinking). The Middle Moulouya basin's subterranean water is slightly acidic to basic, with a pH range of 6.8 to 7.66 and mild to brackish water at specific sites. Furthermore, in line with the hydrochemistry diagrams, groundwater can be classified into three main types: Ca-Cl, Ca-〖HCO〗_3, and Ca-Mg-Cl type. Moreover, the results pertaining to the overall quality of groundwater regarding Moroccan control standards guidelines indicate that: (i) 32.43% of the groundwater samples are of excellent quality, (ii) 24.32 % of the collected water points are of good quality, (iii) 32.43 % have medium quality, (iiii) and only 10.82 % are of poor and very poor quality (i.e., 5.41 % for each class). Finally, based on the Wilcox method, a significant percentage of groundwater sites are suitable for farming.