Abstract. While the history of a fluvial hydrosystem can provide essential
knowledge on present functioning, historical context remains rarely
considered in river restoration. Here we show the relevance of an
interdisciplinary study for improving restoration within the framework of a
European LIFE+ project on the French side of the Upper Rhine (Rohrschollen
Island). Investigating the planimetric evolution combined with historical
high-flow data enabled us to reconstruct pre-disturbance hydromorphological
functioning and major changes that occurred on the reach. A deposition
frequency assessment combining vertical evolution of the Rhine thalweg,
chronology of deposits in the floodplain, and a hydrological model revealed
that the period of incision in the main channel corresponded to high rates of
narrowing and lateral channel filling. Analysis of filling processes using
Passega diagrams and IRSL dating highlights that periods of engineering works
were closely related to fine sediment deposition, which also presents
concomitant heavy metal accumulation. In fact, current fluvial forms,
processes and sediment chemistry around Rohrschollen Island directly reflect
the disturbances that occurred during past correction works, and up to today.
Our results underscore the advantage of combining functional restoration with
detailed knowledge of the past trajectory to (i) understand the functioning
of the hydrosystem prior to anthropogenic disturbances, (ii) characterize the
human-driven morphodynamic adjustments during the last 2 centuries,
(iii) characterize physico-chemical sediment properties to trace
anthropogenic activities and evaluate the potential impact of the restoration
on pollutant remobilization, (iv) deduce the post-restoration evolution
tendency and (v) evaluate the efficiency and sustainability of the
restoration effects. We anticipate our approach will expand the toolbox of
decision-makers and help orientate functional restoration actions in the
future.