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Titel Spatio-temporal monitoring of water infiltration in weathered clay-shale slopes with electrical resistivity tomography
VerfasserIn J. Travelletti, P. Sailhac, G. Grandjean, J.-P. Malet, J. Ponton, S. Garambois
Konferenz EGU General Assembly 2009
Medientyp Artikel
Sprache Englisch
Digitales Dokument PDF
Erschienen In: GRA - Volume 11 (2009)
Datensatznummer 250024257
 
Zusammenfassung
Time-laps Electrical Resistivity Tomography (ERT) surveys have been used for monitoring hydrological processes linked to time-varying resistivity changes in the topsoil. The ERT monitoring has been performed at high spatial (electrode spacing of 0.5m to 1.0m) and temporal (3h) resolution during controlled rainfall experiments on some landslides developed in black marls. Several representative plots of a few meters square with different initial hydrological conditions (unsaturated, nearly saturated) and soil surface characteristics (slope gradient, fissure density, grain size of the matrix) have been investigated with a ~15 mm.h-1 rainfall during several days. After filtering the electrical tension values lower than the resistivimeter device sensibility (