Hydrological response of weathered clay-shale slopes: Water infiltration monitoring with time-lapse electrical resistivity tomography

Hydrological Processes

Volumn 26, Issue 14, 2012, Pages 2106-2119

  Travelletti, J ^a,b   Sailhac, P ^a   Malet, J P ^a   Grandjean, G ^c   Ponton, J ^a  

^a UNIVERSITÉ DE STRASBOURG   (France)

^b UNIVERSITÉ DE CAEN   (France)

^c BRGM   (France)

Author keywords

Electrical resistivity tomography; Geophysical monitoring; Landslide; Steady state flow; Water infiltration

Indexed keywords

CHEMICAL TRACERS; CLAY SHALE; CONSTANT LEVEL; CROSS MODEL; DOWNSLOPE; ELECTRICAL RESISTIVITY; ELECTRICAL RESISTIVITY TOMOGRAPHY; FRENCH ALPS; GEOPHYSICAL MONITORING; HIGH WATER; HYDROLOGICAL RESPONSE; HYDROLOGICAL SYSTEM; INITIAL STATE; LATERAL FLOW; PREFERENTIAL FLOWS; RESISTIVITY VALUES; SATURATED HYDRAULIC CONDUCTIVITY; STEADY-STATE CONDITION; STEADY-STATE FLOW CONDITIONS; STEADY-STATE FLOWS; SUBSURFACE FLOW; TEMPORAL DEVELOPMENT; UNSATURATED CONDITION; WATER CIRCULATION; WATER INFILTRATION;

CATCHMENTS; CHEMICAL ANALYSIS; ELECTRIC CONDUCTIVITY; EXPERIMENTS; GROUNDWATER; LANDSLIDES; RAIN; SHALE; STEADY FLOW; WATER LEVELS;

INFILTRATION;

CLAY; ELECTRICAL RESISTIVITY; GEOPHYSICAL METHOD; HYDRAULIC CONDUCTIVITY; HYDROLOGICAL RESPONSE; INFILTRATION; LANDSLIDE; MONITORING; PREFERENTIAL FLOW; SHALE; SLOPE; SOIL WATER; STEADY FLOW; SUBSURFACE FLOW; TOMOGRAPHY; WEATHERED MEDIUM;

EID: 84863474637     PISSN: 08856087     EISSN: 10991085     Source Type: Journal    
DOI: 10.1002/hyp.7983     Document Type: Article

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