J 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.