Hydrogeochemical processes in a small eastern mediterranean karst watershed (Nahr Ibrahim, Lebanon)

التفاصيل البيبلوغرافية
العنوان: Hydrogeochemical processes in a small eastern mediterranean karst watershed (Nahr Ibrahim, Lebanon)
المؤلفون: Nabil Amacha, Véronique Kazpard, E. Maatouk, A.G. El Samrani, N. Hanna, S. Sassine, Bruno Lartiges
المساهمون: Géosciences Environnement Toulouse (GET), Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Observatoire Midi-Pyrénées (OMP), Météo France-Centre National d'Études Spatiales [Toulouse] (CNES)-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Météo France-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS)
المصدر: Aquatic Geochemistry
Aquatic Geochemistry, Springer Verlag, 2018, ⟨10.1007/s10498-018-9346-x⟩
Aquatic Geochemistry, 2018, ⟨10.1007/s10498-018-9346-x⟩
بيانات النشر: HAL CCSD, 2018.
سنة النشر: 2018
مصطلحات موضوعية: Calcite, Hydrology, geography, geography.geographical_feature_category, 010504 meteorology & atmospheric sciences, [SDE.IE]Environmental Sciences/Environmental Engineering, Dolomite, Weathering, Groundwater recharge, 010501 environmental sciences, Karst, 01 natural sciences, 6. Clean water, chemistry.chemical_compound, Geophysics, chemistry, 13. Climate action, Geochemistry and Petrology, Snowmelt, Spring (hydrology), [SDE]Environmental Sciences, Carbonate, Environmental science, ComputingMilieux_MISCELLANEOUS, 0105 earth and related environmental sciences
الوصف: Watersheds located in semiarid areas such as the eastern Mediterranean are particularly sensitive to the impact of climate change. To gain knowledge on the hydrogeochemical processes occurring in the Nahr Ibrahim watershed, a Critical Zone Observatory in Lebanon, we analyze the isotopic composition of the river water as well as the concentrations of the major ions exported (Ca2+, Mg2+, HCO3−, Na+, Cl−, K+, SO42−). Sampling campaigns were conducted from March 2014 to August 2016 to capture contrasting hydrological conditions. The results indicate that the carbonate lithology of the watershed is the predominant source of Ca2+, Mg2+ and HCO3−, whereas the low contents of Na+, Cl−, K+, SO42− mainly originate from sea spray. Except in the headwaters, the Nahr Ibrahim River is oversaturated with respect to calcite and dolomite. During wet seasons, calcite weathering and dolomite weathering contribute in an equivalent manner to the solute budget, whereas during dry seasons, calcite precipitates in the river. The isotopic composition of the river water reveals little seasonal dependency, the groundwater recharge by snowmelt infiltration leading to spring waters depleted in heavier isotopes during the dry seasons. A carbonate weathering rate of about 176 t/km2/year was determined at the outlet of the Nahr Ibrahim watershed. The calculated values of CO2 partial pressure, on average twice the atmospheric pressure, suggest that the river is a significant source of CO2 to the atmosphere (111 t/year).
اللغة: English
تدمد: 1380-6165
1573-1421
URL الوصول: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a6b15c6c486fe944194e84d6a1b00a67
https://hal.archives-ouvertes.fr/hal-02265626/document
حقوق: OPEN
رقم الأكسشن: edsair.doi.dedup.....a6b15c6c486fe944194e84d6a1b00a67
قاعدة البيانات: OpenAIRE