Programme Poster session 2
Characterisation of underground flows in karstic aquifers by studying
DOM fluorescence. Example of two Mediterranean systems (Lez and Causse d’Aumelas, Southeastern France)
Author(s): Christelle Batiot-Guilhe, Jean-Luc Seidel, Antoine Lafare, Hervé Jourde, Marie-Ange Cordier, Sandra
Van-Exter, Claire Rodier
Christelle Batiot-Guilhe (1), Jean-Luc Seidel
(1), Antoine Lafare (2), Hervé Jourde (1), Marie-Ange Cordier (1), Sandra Van-Exter (1), Claire Rodier (1)
(1) HydroSciences Montpellier, UMR 5569, University of Montpellier 2, Place E. Bataillon, F-34095
Montpellier Cedex 5, France
(2) BRGM Eau/RMD, 1039 Rue de Pinville, 34000 Montpellier
Keyword(s): karstic aquifers,
Session: Poster session 2
aquifers are very particular hydrogeological systems, characterised by preferential flows and mixing of waters with
different residence time. Recent works have shown that Total Organic Carbon (TOC) and Dissolved Organic
Carbon (DOC) are relevant tracers of water infiltration within aquifers and specially in karstic areas. By using
fluorescence spectroscopy, the type of organic compounds in solution and their natural or anthropogenic origin can
be identify. Indeed, the fluorescence in natural waters originates mainly from organic acids (humic substances) and
amino-acids. Recent works (, , , ) focused on the study of Dissolved Organic Matter (DOM) in natural
waters by Excitation-Emission Matrix Spectroscopy (EEMS) and demonstrated that this technique is a relevant tool
to perform a DOM qualitative and quantitative identification.
We investigated this tracer on two karst
systems, the “Lez” and the “Causse d’Aumelas” aquifers located in southeastern France, near Montpellier. These
two karsts are constituted by secondary carbonate deposits, partly recovered by low permeable tertiary and/or
secondary terrains. Their watersheds are respectively about 380 km2 and 200km2. These systems are more or less
connected with intermittent streams, which may act as a contaminant source from surface waters to groundwaters.
The study aims at understanding their behaviour during flood events and comparing infiltration flows within these two
In order to understand the interactions between surface waters and groundwaters,
hydrodynamical and hydrochemical monitorings have been carried out at temporary and perennial springs,
boreholes, swallow holes, and on the surface waters. Electrical conductivity, temperature and pH are also measured
on each point and water samplings are completed twice a month or daily during flood events, in order to study
hydrochemical tracers (major and trace elements, TOC, DOC, fluorescence of organic matter).
results of the study upon the main perennial and temporary springs of these aquifers show very strong variations in
TOC concentrations, about 0.5 ppm during dry season to more 10 ppm during flood events, which are clearly linked
with fast infiltration. The main part of DOM at these outlets are characterised by couples of excitation-emission
wavelengths (ExcMax/EmMax): 320-260 / 435-445 nm which corresponds to fulvic acids and identify a pedogenic
The study of DOM appears as a new relevant and easy tool to use in order to investigate karstic flows and
highlight the existence of fast infiltration which is fundamental to estimate the vulnerability of the aquifer and to protect
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