%0 Conference Paper %F Oral %T Measuring fallout radionuclides to constrain the origin and the dynamics of suspended sediment in an agricultural drained catchment (Loire River basin, France) %+ Laboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette] (LSCE) %+ Géochimie Des Impacts (GEDI) %+ GéoHydrosystèmes COntinentaux (GéHCO EA6293) %+ Bureau de Recherches Géologiques et Minières (BRGM) (BRGM) %A Le Gall, Marion %A Evrard, Olivier %A Foucher, Anthony %A Laceby, J., Patrick %A Sébastien, Salvador-Blanes %A Lefèvre, Irène %A Cerdan, Olivier %A Ayrault, Sophie %< avec comité de lecture %B EGU General Assembly 2015 %C Vienne, Austria %S Geophysical Research Abstracts %V 17 %P EGU2015-5621-1 %8 2015-04-12 %D 2015 %Z Environmental Sciences %Z Environmental Sciences/Global Changes %Z Sciences of the Universe [physics]/Continental interfaces, environment %Z Sciences of the Universe [physics]/Earth Sciences/Geomorphology %Z Sciences of the Universe [physics]/Earth Sciences/Hydrology %Z Life Sciences [q-bio]/Agricultural sciences/Soil studyConference papers %X Soil erosion reaches problematic levels in agricultural areas of Northwestern Europe where tile drains may accelerate sediment transfer to rivers. This supply of large quantities of fine sediment to the river network leads to the degradation of water quality by increasing water turbidity, filling reservoirs and transporting contaminants. Agricultural patterns and landscapes features have been largely modified by human activities during the last century. To investigate erosion and sediment transport in lowland drained areas, a small catchment, the Louroux (24 km$^2$), located in the French Loire River basin was selected. In this catchment, channels have been reshaped and more than 220 tile drains outlets have been installed after World War II. As a result, soil erosion and sediment fluxes strongly increased. Sediment supply needs to be better understood by quantifying the contribution of sources and the residence times of particles within the catchment. To this end, a network of river monitoring stations was installed, and fallout radionuclides (Cs-137, excess Pb-210 and Be-7) were measured in rainwater (n=3), drain tile outlets (n=4), suspended sediment (n=15), soil surface (n=30) and channel bank samples (n=15) between January 2013 and February 2014. Cs-137 concentrations were used to quantify the contribution of surface vs. subsurface sources of sediment. Results show a clear dominance of particles originating from surface sources (99 ± 1%). Be-7 and excess Pb-210 concentrations and calculation of Be-7/excess Pb-210 ratios in rainfall and suspended sediment samples were used to estimate percentages of recently eroded sediment in rivers. The first erosive winter storm mainly exported sediment depleted in Be-7 that likely deposited on the riverbed during the previous months. Then, during the subsequent floods, sediment was directly eroded and exported to the catchment outlet. Our results show the added value of combining spatial and temporal tracers to characterize and quantify sources of sediment and particle transport processes within an agricultural catchment. %G English %2 https://cea.hal.science/cea-02648081/document %2 https://cea.hal.science/cea-02648081/file/EGU2015-5621-1.pdf %L cea-02648081 %U https://cea.hal.science/cea-02648081 %~ SDE %~ CEA %~ INSU %~ BRGM %~ UNIV-TOURS %~ CNRS %~ GIP-BE %~ UVSQ %~ CEA-UPSAY %~ LSCE %~ UNIV-PARIS-SACLAY %~ CEA-UPSAY-SACLAY %~ UVSQ-SACLAY %~ GEHCO %~ LSCE-CEA %~ UVSQ-UPSACLAY %~ GS-GEOSCIENCES %~ GS-BIOSPHERA %~ INSTITUT-SCIENCES-LUMIERE %~ TEST3-HALCNRS