Examining suspended sediment sources and dynamics during flood events in a drained catchment using radiogenic strontium isotope ratios (87Sr/86Sr)

Abstract Soil erosion is recognized as one of the main processes of land degradation in agricultural areas. High suspended sediment loads, often generated from eroding agricultural landscapes, are known to degrade downstream environments. Accordingly, there is a need to identify suspended sediment sources and to investigate their dynamics. Here, soil and sediment strontium isotopic ratios were used to examine suspended sediment sources and dynamics in a lowland drained catchment in France. Suspended sediment ( n  = 14) was collected in stream and at tile drain ( n  = 4) outlets during three flood events between December 2013 and February 2014. Potential source soils ( n  = 28) representative of the carbonate and silicate substrates found in the catchment were sampled and analyzed. Strontium isotopic ratios ( 87 Sr/ 86 Sr) were measured in different particle size fractions ( Soil 87 Sr/ 86 Sr ratios significantly discriminated between source samples classified as carbonate (0.712625 to 0.717815) and silicate (0.719287 to 0.724631) soils. 87 Sr/ 86 Sr ratios measured in suspended sediment (0.713660 to 0.720571) reflect variations in source contributions during different hydrological conditions. The 87 Sr/ 86 Sr ratios varied in the different fractions of soil samples (i.e. The results also show that the tile drainage system enhances the connectivity between cultivated hillslopes and the river network, providing a preferential pathway for fine (