Abstract. The
nature of abandoned channels' sedimentary fills has a
significant influence on the development and evolution of floodplains and
ultimately on fluvial reservoir geometry. A control of bifurcation geometry
(i.e., bifurcation angle) on channel abandonment dynamics and resulting
channel fills, such as sand plugs, has been intuited many times but never
quantified. In this study, we present a series of experiments focusing on
bedload transport designed to test the conditions for channel abandonment by
modifying the bifurcation angle between channels, the flow incidence angles
and the differential channel bottom slopes. We find that disconnection is
possible in the case of asymmetrical bifurcations with high diversion angle
(≥30∘) and quantify for the first time an inverse
relationship between diversion angle and sand plug length and volume. The
resulting sand plug formation is initiated in the flow separation zone at the
external bank of the mouth of the diverted channel. Sedimentation in this
zone induces a feedback loop leading to sand plug growth, discharge decrease
and eventually to channel disconnection. Finally, the formation processes
and final complex architecture of sand plugs are described, allowing for a
better understanding of their geometry. Although our setup lacks some of the
complexity of natural rivers, our results seem to apply at larger scales.
Taken into account, these new data will improve fluvial (reservoir) models
by incorporating more realistic topography and grain size description in
abandoned channels.