Ahmed El-Azhari1, Yassine Ait Brahim2, Florent Barbecot3

  • 1International Water Research Institute, University Mohammed VI Polytechnic (UM6P), Benguerir, Morocco; Geotop-UQAM, Hydro Sciences, Department of Earth and Atmospheric Sciences, University of Quebec at Montreal (UQAM), Montreal, Quebec H3C 3P8, Canada.

概括

干旱的内盆地地下水的盐度是一个主要问题. 这项研究揭示了由于蒸发和土壤出而导致的非封闭含水层的超度,与封闭含水层的较低盐度形成鲜明对比.

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