Marie Pettenati
University of Paris-Sud
21 Papers
23 Citations
Marie Pettenati is an academic researcher from University of Paris-Sud. The author has contributed to research in topics: Aquifer & Groundwater. The author has an hindex of 7, co-authored 19 publications.
Chat about Author
Papers
Managed Aquifer Recharge: An Overview of Issues and Options
Joël Casanova,Nicolas Devau,Marie Pettenati +2 more
- 01 Jan 2016
TL;DR: In this paper, the authors discuss the salinization of coastal aquifers and the importance of preserving local groundwater resources in coastal zones and is vital in an island context, which is consistent with the groundwater objective of the European Union Water Framework Directive.
Simulating fluoride evolution in groundwater using a reactive multicomponent transient transport model: Application to a crystalline aquifer of Southern India
TL;DR: In this article, a transient simulation was performed with a 1D reactive transport PHREEQC column and took into account IRF evaporation, kinetically controlled mineral dissolution/precipitation, ion adsorption on Fe hydroxides, and mixing with fresh groundwater.
61
Autotrophic denitrification supported by biotite dissolution in crystalline aquifers (1): New insights from short-term batch experiments.
Luc Aquilina,Clément Roques,A. Boisson,Virginie Vergnaud-Ayraud,Thierry Labasque,Hélène Pauwels,Emmanuelle Petelet-Giraud,Marie Pettenati,Alexis Dufresne,Lorine Bethencourt,Olivier Bour +10 more
TL;DR: Results are interpreted as the development of microbial activity which induces mineral dissolution in order to uptake Fe(II) which is used for denitrification, which could account for all the observed Fe production.
24
Capillary geochemistry in non-saturated zone of soils. Water content and geochemical signatures
TL;DR: In this article, a volumetric water content of the soil at high suction can be calculated extrapolating the water retention curves (WRC) with the Rossi-Nimmo model, and two field situations are interpreted using the capillary thermodynamic properties: (1) the trapping of sand grains during the growth of desert roses (gypsum), and (2) the development of abnormal paragenetic sequences in some saprolites.
23
The combined effect of abandoned mines and agriculture on groundwater chemistry
TL;DR: The currently observed high arsenic concentrations in the groundwater are interpreted as resulting mainly from the former mining activities through a remobilization of As sorbed on or co-precipitated with the iron oxides that formed when the gallery was excavated.
21