Use of Total Organic Carbon (TOC) as tracer of diffuse infiltration in a dolomitic karstic system: The Nerja Cave (Andalusia, southern Spain)

Author:

Batiot Christelle1,Liñán Cristina2,Andreo Bartolomé3,Emblanch Christophe4,Carrasco Francisco3,Blavoux Bernard4

Affiliation:

1. Laboratoire Hydrosciences; Université Montpellier II, C.C. Maison des Sciences de l'Eau; Montpellier Cedex 5 France

2. Institute of Research; Nerja Cave Foundation. Ctra. Maro s/n; Nerja, Málaga Spain

3. Department of Geology, Faculty of Sciences; University of Málaga; Málaga Spain

4. Laboratoire d'Hydrogéologie; Université d'Avignon; Avignon France

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference10 articles.

1. Oxidation of organic matter in a karstic hydrologic unit supplied through stream sinks (Loiret, France);Albéric;Water Res.,1998

2. Andreo , B. F. Carrasco C. Liñán I. Vadillo Epigenic CO 2 controlling the drip water chemistry and speleothem growth in a Mediterranean karst area (Nerja Cave, southern Spain) Karst processes and the Carbon cycle Y. Daoxian Z. Cheng 51 64 2002

3. Carbone Organique Total (COT) et Magnésium (Mg2+): Deux traceurs complémentaires du temps de séjour dans l'aquifère karstique;Batiot;C. R. Geosciences,2003

4. A stable isotope study of cave seepage waters;Caballero;App. Geochem.,1996

5. Chemistry of the water in the Nerja Cave System (Andalusia, Spain);Carrasco;Cave and Karst Science,1995

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