Maarten will focus on the combined analysis of suspended sediment transport records and seismically-derived bedload transport measurements in order to gain insight in:
1) the provenance of the suspended sediment (hillslope/tributary supply vs. release from the active channel bed);
2) how the provenance varies on seasonal and (flood) event-based temporal scales; and
3) how suspended sediment (and bedload) dynamics relate to upstream channel morphology/morphological changes.