Comment on "Streaming potential dependence on water-content in Fontainebleau sand" by V. Allegre, L. Jouniaux, F. Lehmann and P. Sailhac
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2011
- doi: 10.1111/j.1365-246X.2010.04850.x
- issn: 0956-540X
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Suspended water zone Zone of suspended water Vadose zone Aeration, Zone of Unsaturated zone Quartz sand Porous media Flow of water Water--Flow Pattern ModelCiter ce document
A. Revil et al., « Comment on "Streaming potential dependence on water-content in Fontainebleau sand" by V. Allegre, L. Jouniaux, F. Lehmann and P. Sailhac », Serveur académique Lausannois, ID : 10.1111/j.1365-246X.2010.04850.x
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Allegre et al. recently presented new experimental data regarding the dependence of the streaming potential coupling coefficient with the saturation of the water phase. Such experiments are important to model the self-potential response associated with the flow of water in the vadose zone and the electroseismic/seismoelectric conversions in unsaturated porous media. However, the approach used to interpret the data is questionable and the conclusions reached by Allegre et al. likely incorrect