ABSTRACT
One-decade-long observations of post-cut-off channel development and oxbow lake formation are presented to offer insight into the morphological response of the Morava River to neck cut-off. The main objectives were: calculation of the amount of sediment released to the channel by collapse of the meander neck; comparison of floodplain erosion and deposition rates before and after cut-off; and description of the rate and pattern of oxbow lake sedimentation. The amount of sediment released due to cut-off (~35 000 m3) equalled 2–5 years of sediment input by lateral erosion averaged for the past six decades. Bank erosion rates substantially exceeded long-term averages (0.63–6.21 m year−1, post cut-off). Despite a low entrance angle, alluvial plugs in a newly formed oxbow lake were established within a few months. Between 2006 and 2016, sedimentation of the alluvial plugs proceeded at an average rate of 0.55 m year−1, reflecting the time since cut-off and the frequency of overbank flows.
Editor A. Castellarin Associate editor G. Di Baldassarre
Editor A. Castellarin Associate editor G. Di Baldassarre
Acknowledgements
The authors would like to thank Lenka Ondráčková and Martin Knot for their help during the field campaigns. Two anonymous reviewers are highly acknowledged for their valuable comments and recommendations, which helped to improve the previous version of the manuscript.
Disclosure statement
No potential conflict of interest was reported by the authors.