BRUNET , Pascal

In the Cevennes mountainous area, flood processes are due to excess of soil water storage capacity depending on soil porosity, depth and water content at the beginning of the flood (Bouvier et al., 2007; Cosandey, 1994). For hydrological modeling, it is thus important to estimate the hydrodynamic properties of the whole vertical soil profile....

This study focuses on a 10‐m2 plot within a granitic hillslope in Cevennes mountainous area in France, in order to study infiltration and subsurface hydrological processes during heavy rainfalls and flash floods. The monitoring device included water content at several depths (0–70 cm for the shallow soil water; 0–10 m for the deep water) during...

This study focuses on a 10-m2 plot within a granitic hillslope in Cevennes mountainous area in France, in order to study infiltration and subsurface hydrological processes during heavy rainfalls and flash floods. The monitoring device included water content at several depths (0-70cm for the shallow soil water; 0-10m for the deep water) during...