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; Zdeněk MÁČKA; Monika ŠULC MICHALKOVÁ; René PUTIŠKA; Martin KNOT; Petr HOLÍK; 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

Označené pro přenos do RIV

Ano

Kód RIV

RIV/00216224:14310/18:00103224

Organizační jednotka

Přírodovědecká fakulta

EID Scopus

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.