\http://www.iaeme.com/IJCIET/index.asp 2706 editor@iaeme.com International Journal of Civil Engineering and Technology (IJCIET) Volume 10, Issue 03, March 2019, pp. 2706-2715, Article ID: IJCIET_10_03_270 Available online at http://www.iaeme.com/ijciet/issues.asp?JType=IJCIET&VType=10&IType=03 ISSN Print: 0976-6308 and ISSN Online: 0976-6316 © IAEME Publication Scopus Indexed GEOCHEMISTRY, QUALITY APPRAISAL OF GROUNDWATER AND HYDROGEOCHEMICAL PROCESS IN MIDDLE OUERRHA, TAOUNATE, RIF MOROCCO Ahmed El Bakouri* Team of Waters, Wastewaters, Laboratory of Environment and Quality, Faculty of Sciences, Ibn Tofail University, Kenitra, Morocco Khadija El Kharrim Team of Waters, Wastewaters, Laboratory of Environment and Quality, Faculty of Sciences, Ibn Tofail University, Kenitra, Morocco Mohamed Tayebi Team of Valorisation of Georesources and Territorial Planning, Laboratory of Geosciences and Environment, Faculty of Sciences, Ibn Tofail University, Kenitra, Morocco Driss Belghyti Team of Waters, Wastewaters, Laboratory of Environment and Quality, Faculty of Sciences, Ibn Tofail University, Kenitra, Morocco *Corresponding Author ABSTRACT A hydrogeochemical study was conducted in the Middle Ouerrha, Taounate, Morocco, to identify the mechanisms responsible for the chemical compositions of the shallow groundwater and to document water quality. Different physicochemical parameters are determined, and correlation were used to reveal the hydrogeochemical characteristics of the shallow groundwater, and the potential water-rock interactions. Groundwater samples were collected from a natural source and two wells. Unfortunately, the groundwater of Taounate district have know the problem of salinity, which threatens their quality. In the Hammam source were characterized by high levels of salinity. The temperature, pH, electrical conductivity, salinity, Ca, Mg, Cl, SO 4 , K, NO 3 , Na and HCO 3 were determined. The predominant mechanism controlling groundwater chemistry proved to be the dissolution of carbonates, salt red marls and gypsum. The purpose of this study was to identify salinity water sources and quantitatively analyze their composition using