2013
DOI: 10.1016/j.apgeochem.2013.03.005
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Integration of geochemical and isotopic tracers for elucidating water sources and salinization of shallow aquifers in the sub-Saharan Drâa Basin, Morocco

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Cited by 56 publications
(31 citation statements)
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“…Kidney stones were the second important purpose of using MP. The water composition of this area shows high mineral concentrations [27] that can contribute to an insufficient high urine volume and consequently to a decline in the concentration of lithogenic substances and a high risk of calcium oxalate crystallization [28]. Furthermore, this region is characterized by a high level of temperature in summer, which can also be associated with kidney lithiasis stone attacks cases increase [29].…”
Section: Discussionmentioning
confidence: 99%
“…Kidney stones were the second important purpose of using MP. The water composition of this area shows high mineral concentrations [27] that can contribute to an insufficient high urine volume and consequently to a decline in the concentration of lithogenic substances and a high risk of calcium oxalate crystallization [28]. Furthermore, this region is characterized by a high level of temperature in summer, which can also be associated with kidney lithiasis stone attacks cases increase [29].…”
Section: Discussionmentioning
confidence: 99%
“…Halite is the most frequent manner of enhancing water with Na and Cl ions (i.e. Farhat et al 2010;Warner et al 2013). It can be easily and quickly dissolved.…”
Section: Discussionmentioning
confidence: 99%
“…This reduction induces dissolved SO 4 2− to become isotopically enriched in 34 S with decreasing concentration (Canfield, 2001;Chambers and Trudinger, 1979;Gammons et al, 2013;Nakai and Jensen, 1964). Strontium (Sr) isotope compositions are usually reported using the ratio of 87 Sr/ 86 Sr, which is a useful tracer for identifying hydrogeochemical processes, especially the origin and flow pathways of groundwater (Armstrong et al, 1998;Bohlke and Horan, 2000;Chapman et al, 2013;Heidel et al, 2007;Khaska et al, 2013;Nordstrom et al, 1992;Paces and Wurster, 2014;Raiber et al, 2009;Vilomet et al, 2001;Warner et al, 2013). Moreover, the suitability of this tracer is enhanced by the lack of Sr isotope fractionation during hydrogeological processes (Barbieri and Morotti, 2003;Naftz et al, 1997;Negrel et al, 2001).…”
Section: Introductionmentioning
confidence: 97%