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Carbon 13 of TDIC to quantify the role of the unsaturated zone: the example of the Vaucluse karst systems (Southeastern France)

C. Emblanch 1 G.M Zuppi J. Mudry 2 B Blavoux Christelle Batiot-Guilhe 3 
1 EMMAH - Environnement Méditerranéen et Modélisation des Agro-Hydrosystèmes
2 LCE - Laboratoire Chrono-environnement - CNRS - UBFC (UMR 6249)
3 HSM - Hydrosciences Montpellier
Keywords : Karst Hydrogeology TOC Magnesium Unsaturated zone Saturated zone
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https://hal-univ-avignon.archives-ouvertes.fr/hal-02295156
Contributor : Sonja Böttger Connect in order to contact the contributor
Submitted on : Tuesday, September 24, 2019 - 8:35:48 AM
Last modification on : Tuesday, July 5, 2022 - 9:15:36 AM

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INSU | UNIV-AVIGNON | CNRS | UNIV-FCOMTE | CHRONO-ENVIRONNEMENT | HSM | AGROPOLIS | B3ESTE | UNIV-MONTPELLIER | INRAE | EMMAH | FORKARST

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C. Emblanch, G.M Zuppi, J. Mudry, B Blavoux, Christelle Batiot-Guilhe. Carbon 13 of TDIC to quantify the role of the unsaturated zone: the example of the Vaucluse karst systems (Southeastern France). Journal of Hydrology, 2003, 279 (1-4), pp.262-274. ⟨10.1016/S0022-1694(03)00180-X⟩. ⟨hal-02295156⟩

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