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The streamflow components were determined in a small catchment located in Eastern France for a 40 mm rain event using isotopic and chemical tracing with particular focus on the spatial and temporal variations of catchment sources.Precipitation, soil solution, springwater and streamwaters were sampled and analysed for stable water isotopes ( 18 O and 2 H), major chemical parameters...
Flood generation processes are studied in a small mountainous Mediterranean catchment using natural chemical and isotopic water tracing. The study takes place during the autumn of 1996 for three successive floods of uneven magnitude. The flow resumption following the summer period is a prime opportunity to establish the impact of the soil moisture status on the catchment response. A dynamic scheme...
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