Integration of geochemical and isotopic tracers for elucidating water sources and salinization of shallow aquifers in the sub-Saharan Drâa Basin, Morocco
In the arid sub-Saharan of southern Morocco, groundwater salinization poses a direct threat for agricultural production in six oases' basins that are irrigated by water imported from the High Atlas Mountains. Here the geospatial distribution of salinity is evaluated in shallow groundwater, springs and surface waters in the Drâa Basin, integrating major and trace element geochemistry and isotopic tracers (O, H, Sr and B). The data show that water discharge from the High Atlas Mountains to the Upper section of the Drâa Basin is characterized by both low and high salinity, a distinctive low δ 18 O and δ 2 H composition (as low as -9‰ and -66‰, respectively), typical for meteoric water from high elevation, a 87 Sr/ 86 Sr range of 0.7078-0.7094, and δ 11 B of 12-17‰. The Ca-Mg-HCO 3 , Na-Cl-SO 4 , and Ca-SO 4 compositions as well as the Br/Cl, 87 Sr/ 86 Sr, and δ 11 B values of the saline water suggest dissolution of Lower Jurassic carbonates and evaporite rocks in the High Atlas Mountain catchment. Storage and evaporation of the imported water in a man-made open reservoir causes an enrichment of the stable isotope ratios with a δ 18 O/δ 2 H slope of <8 but no change in the Sr and B isotope fingerprints. Downstream from the reservoir, large salinity variations were documented in the shallow groundwater from the six Drâa oases, with systematically higher salinity in the three southern oases, up to 12,000mg/L. The increase of the salinity is systematically associated with a decrease of the Br/Cl ratio, indicating that the main mechanism of groundwater salinization in the shallow aquifers in the Drâa oases is via salt dissolution (gypsum, halite) in the unsaturated zone. Investigation of shallow groundwater that flows to the northern Drâa oases revealed lower salinity (TDS of 500-4225) water that is characterized by depleted 18 O and 2 H (as low as -9‰ and -66‰, respectively) and higher 87 Sr/ 86 Sr ratios (~0.7107-0.7115) relative to irrigation water and groundwater flow from the Upper Drâa Basin. This newly-discovered low-saline groundwater with a different isotopic imprint flows from the northeastern Anti-Atlas Jabel Saghro Mountains to the northern oases of the Lower Drâa Basin. This adjacent subsurface flow results in a wide range of Sr isotope ratios in the shallow oases groundwater (0.7084-0.7131) and appears to mitigate salinization in the three northern Drâa oases. In contrast, in the southern oases, the higher salinity suggests that this mitigation is not as affective and increasing salinization through cycles of water irrigation and salt dissolution appears inevitable. © 2013 Elsevier Ltd.
Warner, N; Lgourna, Z; Bouchaou, L; Boutaleb, S; Tagma, T; Hsaissoune, M; Vengosh, A
Volume / Issue
Start / End Page
International Standard Serial Number (ISSN)
Digital Object Identifier (DOI)