Punctual and continuous estimation of transit time from dissolved organic matter fluorescence properties in karst aquifers, application to groundwaters of ‘Fontaine de Vaucluse’ experimental basin (SE France)

Author:

Blondel T.,Emblanch C.,Batiot-Guilhe C.,Dudal Y.,Boyer D.

Publisher

Springer Science and Business Media LLC

Subject

Earth-Surface Processes,Geology,Pollution,Soil Science,Water Science and Technology,Environmental Chemistry,Global and Planetary Change

Reference49 articles.

1. Baker A, Genty D (1999) Fluorescence wavelength and intensity variations of cave waters. J Hydrol 217(1–2):19–34

2. Baker A, Lamont-BIack J (2001) Fluorescence of dissolved organic matter as a natural tracer of ground water. Ground Water 39(5):745–750

3. Batiot C (2002) Etude expérimentale du cycle du carbone en régions karstiques. Apport du carbone organique et du carbone minéral à la connaissance hydrogéologique des systèmes. Site expérimental de Vaucluse, Jura, Larzac, Région Nord-Montpelliéraine, Nerja (Espagne). PhD Thesis, Université d’Avignon et des Pays de Vaucluse, Avignon, France

4. Batiot C, Emblanch C, Blavoux B (2003) Total organic carbon (TOC) and magnesium (Mg2+): two complementary tracers of residence time in karstic systems. Comptes Rendus Geosci 335(2):205–214

5. Birdwell JE, Engel AS (2010) Variability in terrestrial and microbial contributions to dissolved organic matter fluorescence in the Edwards aquifer, central Texas. J Cave Karst Stud 71(2):144–156

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