Role of Active Floodplains for Nutrient Retention in the River Rhine

We evaluated the importance of floodplains for nutrient retention in two distributaries of the river Rhine (Waal and IJssel) by monitoring N and P retention in a body of water during downstream transport. We hypothesized that (i) retention of P is much larger than retention of N and (ii) nutrient retention increases with an increasing amount of the discharge flowing through floodplains (Q F). The second hypothesis was tested by comparing retention between the rivers Waal (low Q F) and IJssel (high Q F), as well as at different discharges. Total nitrogen (TN) did not decrease significantly during downstream transport in both rivers, whereas 20 to 45% of total phosphorus (TP) disappeared during transport in the river IJssel. This difference between N and P retention—supporting the first hypothesis—was probably caused by differences in sedimentation through a much lower proportion of N adsorbed to particles than of P (2–3% of N vs. 50–70% of P). Phosphorus retention was only observed in the IJssel and not in the Waal, and absolute P retention (g P s−1 km−1) in the IJssel increased with increasing Q F The second hypothesis was, nevertheless, not fully supported, because the percentage P retention (% of P load) decreased (instead of increased) with increasing Q F. The percentage P retention increased with decreasing river depth and flow velocity; it seemed related to the efficiency of sediment trapping.