Articles | Volume 13, issue 18
https://doi.org/10.5194/bg-13-5379-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/bg-13-5379-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Carbonate chemistry in sediment porewaters of the Rhône River delta driven by early diagenesis (northwestern Mediterranean)
Laboratoire des Sciences du Climat et de l'Environnement, LSCE/IPSL,
CEA-CNRS-UVSQ-Université Paris Saclay, 91198 Gif-sur-Yvette, France
Bruno Lansard
Laboratoire des Sciences du Climat et de l'Environnement, LSCE/IPSL,
CEA-CNRS-UVSQ-Université Paris Saclay, 91198 Gif-sur-Yvette, France
Lara Pozzato
Laboratoire des Sciences du Climat et de l'Environnement, LSCE/IPSL,
CEA-CNRS-UVSQ-Université Paris Saclay, 91198 Gif-sur-Yvette, France
Institut Méditerranéen d'Océanologie,
CNRS-IRD-Université de Toulon-Aix Marseille, 13288 Marseille, France
Christophe Rabouille
Laboratoire des Sciences du Climat et de l'Environnement, LSCE/IPSL,
CEA-CNRS-UVSQ-Université Paris Saclay, 91198 Gif-sur-Yvette, France
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- FESDIA (v1.0): exploring temporal variations of sediment biogeochemistry under the influence of flood events using numerical modelling S. Nmor et al. 10.5194/gmd-15-7325-2022
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Latest update: 20 Nov 2024
Short summary
In situ O2 and pH measurements as well as determination of porewater concentrations of dissolved inorganic carbon, total alkalinity, sulfate and calcium have been measured in the sediments of the Rhône prodelta. Biogeochemical activity decreased with distance from the river mouth. Oxic processes decreased the carbonate saturation state (Ω) by lowering pH, whereas anaerobic organic matter degradation, dominated by sulfate reduction, was accompanied by increasing Ω and carbonate precipitation.
In situ O2 and pH measurements as well as determination of porewater concentrations of dissolved...
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