2018
Response of channel dynamics to recent meander neck cut-off in a lowland meandering river with artificial training history: the Morava River, Czech Republic
ONDRUCH, Jakub, Zdeněk MÁČKA, Monika ŠULC MICHALKOVÁ, René PUTIŠKA, Martin KNOT et. al.Základní údaje
Originální název
Response of channel dynamics to recent meander neck cut-off in a lowland meandering river with artificial training history: the Morava River, Czech Republic
Autoři
ONDRUCH, Jakub (203 Česká republika, garant, domácí), Zdeněk MÁČKA (203 Česká republika, domácí), Monika ŠULC MICHALKOVÁ (703 Slovensko, domácí), René PUTIŠKA (703 Slovensko), Martin KNOT (203 Česká republika), Petr HOLÍK (203 Česká republika, domácí), Jakub MIŘIJOVSKÝ a Marián JENČO
Vydání
Hydrological Sciences Journal, Taylor & Francis, 2018, 0262-6667
Další údaje
Jazyk
angličtina
Typ výsledku
Článek v odborném periodiku
Obor
10508 Physical geography
Stát vydavatele
Velká Británie a Severní Irsko
Utajení
není předmětem státního či obchodního tajemství
Odkazy
Impakt faktor
Impact factor: 2.180
Kód RIV
RIV/00216224:14310/18:00103224
Organizační jednotka
Přírodovědecká fakulta
UT WoS
000442624000009
Klíčová slova anglicky
neck cut-off; meander; Morava River; oxbow; sedimentation
Změněno: 23. 4. 2024 11:23, Mgr. Michal Petr
Anotace
V originále
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 cutoff. 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.