Actualités et séminaires

  • 09 déc Séminaire

    Understanding the vulnerability of water management under global change is the premise for designing adaptation actions. A comprehensive assessment of current water management vulnerability to future changes hinges on new tools that are able to represent human impact on water resources and innovative frameworks that are able to generate new insights to inform adaptation designing.

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  • 18 nov Séminaire

    Volcano could be distinguished into two groups due to its chemical origin properties. First is basaltic volcanoes from hotspots or rift-zone activity, and the second is andesitic volcanoes around subduction zone. The first type has been highly studied in the last 50 years (Peterson, 1972; Custodio, 1989), but the second one is less known (Charlier et al., 2011; Vittecoq et al., 2019). Located on the subduction zone, Indonesia has a lot of andesitic volcanoes.  One of amazing volcanic complex with a high potentcy of groundwater resouces is Gede – Pangrango – Salak.

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  • 21 oct Actualité

    Titre : De la production spécifique à l'homogénéisation des matières organiques dissoutes issues de végétaux

    Les membres du jury sont :

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  • 21 oct Séminaire

    Effective assessment of the fate of water-soluble contaminants leaked to aquifers is crucial for the management and preservation of groundwater resources. Contaminant solute transport unfolds over multiple spatial and temporal scales and is, thus, very challenging to characterize using conventional sparsely-sampled and local hydrological measurement techniques alone. Complementarily, the time-lapse direct-current (DC) geophysical method provides spatially and temporally-distributed information on equivalent DC electrical conductivity, the latter being sensitive to the transport of electrica

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  • 14 oct Séminaire

    Dissolution and precipitation processes modify the structure of the
    porous media at microscale which significantly affects the macroscopic
    properties of the media. These variations in the pore geometry result
    in changes in the hydraulic properties that control the groundwater
    flow and also in the electrokinetic properties associated to the
    displacement of electrical charges carried by the flow. Therefore the
    evolution of the streaming potential during dissolution and
    precipitation can be estimated from the changes in the electrokinetic

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