Impact of rock-water interactions and recharge on water resources quality of the Agadir-Essaouira basin, southwestern Morocco

• Published in: Arabian journal of geosciences 2017-04, Vol.10 (7), p.1-16, Article 169
• Main Authors: Latifa, Al Yacoubi, Lhoussaine, Bouchaou, Etienne, Jaillard, Moussa, Masrour, Yassine, Ait Brahim, Ahmed, El Mouden, Jana, Schneider, Barbara, Reichert
• Format: Article
• Language: English
• Subjects: Aquifers; Arid climates; Aridity; Boreholes; Calcite; Carbonates; Chemical composition; Cretaceous; Dolomite; Dolostone; Drinking water; Drought; Earth and Environmental Science; Earth science; Earth Sciences; Evaporation; Groundwater; Groundwater quality; Groundwater recharge; Gypsum; Infiltration; Interactions; Ion exchange; Isotopes; Jurassic; Karst; Mineralization; Mountains; Organic chemistry; Original Paper; Outcrops; Rivers; Rocks; Runoff; Semiarid climates; Stable isotopes; Sustainable development; Water quality; Water resources; Water scarcity; Water springs; Weathering
• ISSN: 1866-7511; 1866-7538
• DOI: 10.1007/s12517-017-2968-2

The Agadir-Essaouira area in the occidental High Atlas Mountains of Morocco is characterized by a semi-arid climate. The scarcity and quality of water resources, exacerbated by long drought periods, constitute a major problem for a sustainable development of this region. Groundwater resources of carbonate units within Jurassic and Cretaceous aquifers are requested for drinking and irrigation purposes. In this study, we collected 84 samples from wells, boreholes, springs, and rivers. Hydrochemical and isotopic data were used to examine the mineralization and origin of water, which control groundwater quality. The chemical composition of water seems to be controlled by water-rock interactions, such as dissolution of carbonates (calcite and dolomite), weathering of gypsum, as well as ion exchange processes, which explain the observed variability. Stable isotopes results show that groundwater from the mainly marly Cretaceous aquifer are submitted to an evaporation effect, while samples from the chiefly calcareous Jurassic aquifer indicate a meteoric origin, due to a rapid infiltration of recharge runoff through the karstic outcrops. The low values of δ 18 O and δ 2 H suggest a local recharge from areas with elevations ranging from 400 to 1200 m for the Cretaceous aquifer and from 800 to 1500 m for the Jurassic units.