Sedimentary-vegetation response to the channel by-pass: A case study of the Danube river

The Gabčíkovo-Nagymaros waterworks construction on Danube river in Slovakia (1977−1992) was followed with major ecological consequences. The water level and flow velocity was decreased in the original by-passed channel in order to keep high water level for shipping in the bypass canal. The decrease...

Full description

Bibliographic Details
Main Authors: Horáčková Šárka, Lehotský Milan, Štefanička Tomáš, Viczián István
Format: Article
Language:English
Published: Sciendo 2017-06-01
Series:Ekológia (Bratislava)
Subjects:
Online Access:https://doi.org/10.1515/eko-2017-0015
id doaj-c8555817be1749089ad17d5aa4307a16
record_format Article
spelling doaj-c8555817be1749089ad17d5aa4307a162021-09-05T20:44:47ZengSciendoEkológia (Bratislava)1337-947X2017-06-0136217218310.1515/eko-2017-0015eko-2017-0015Sedimentary-vegetation response to the channel by-pass: A case study of the Danube riverHoráčková Šárka0Lehotský Milan1Štefanička Tomáš2Viczián István3Department of Physical Geography and Geoecology, Comenius University in Bratislava, Mlynská dolina, Ilkovičova 6, 842 15, Bratislava, Slovak RepublicSection of Physical Geography, Geomorphology and Natural Hazards, Slovak Academy of Sciences, Štefánikova 49, 814 73 Bratislava, Slovak RepublicDepartment of Theoretical Geodesy, Slovak University of Technology in Bratislava, Radlinského 11, Block A, 810 05 Bratislava, Slovak RepublicDepartment of Physical Geography, Geographical Institute, Hungarian Academy of Sciences Budaörsi str. 45 (MTA Research Building), H - 1112 Budapest, HungaryThe Gabčíkovo-Nagymaros waterworks construction on Danube river in Slovakia (1977−1992) was followed with major ecological consequences. The water level and flow velocity was decreased in the original by-passed channel in order to keep high water level for shipping in the bypass canal. The decrease in discharge and lowering flow velocity resulted in the channel narrowing and increase in the vertical accretion magnitude in new floodplain pockets along both sides of by-passed channel. What is more, anthropic intervention in form of groynes structures built for channel adjustment before 1992 dramatically accelerated this process. Vegetation colonisation took place on the new floodplain. In this paper, we analysed land cover changes - vegetation succession using aerial photographs taken in 1986, 1996, 2004 and 2013 as well as field surveys. After the flood in 2013, the area of the new floodplain reached 57% (310 ha) of the original channel area.https://doi.org/10.1515/eko-2017-0015danubeby-passed channelland coveralluvial forestsuccession
collection DOAJ
language English
format Article
sources DOAJ
author Horáčková Šárka
Lehotský Milan
Štefanička Tomáš
Viczián István
spellingShingle Horáčková Šárka
Lehotský Milan
Štefanička Tomáš
Viczián István
Sedimentary-vegetation response to the channel by-pass: A case study of the Danube river
Ekológia (Bratislava)
danube
by-passed channel
land cover
alluvial forest
succession
author_facet Horáčková Šárka
Lehotský Milan
Štefanička Tomáš
Viczián István
author_sort Horáčková Šárka
title Sedimentary-vegetation response to the channel by-pass: A case study of the Danube river
title_short Sedimentary-vegetation response to the channel by-pass: A case study of the Danube river
title_full Sedimentary-vegetation response to the channel by-pass: A case study of the Danube river
title_fullStr Sedimentary-vegetation response to the channel by-pass: A case study of the Danube river
title_full_unstemmed Sedimentary-vegetation response to the channel by-pass: A case study of the Danube river
title_sort sedimentary-vegetation response to the channel by-pass: a case study of the danube river
publisher Sciendo
series Ekológia (Bratislava)
issn 1337-947X
publishDate 2017-06-01
description The Gabčíkovo-Nagymaros waterworks construction on Danube river in Slovakia (1977−1992) was followed with major ecological consequences. The water level and flow velocity was decreased in the original by-passed channel in order to keep high water level for shipping in the bypass canal. The decrease in discharge and lowering flow velocity resulted in the channel narrowing and increase in the vertical accretion magnitude in new floodplain pockets along both sides of by-passed channel. What is more, anthropic intervention in form of groynes structures built for channel adjustment before 1992 dramatically accelerated this process. Vegetation colonisation took place on the new floodplain. In this paper, we analysed land cover changes - vegetation succession using aerial photographs taken in 1986, 1996, 2004 and 2013 as well as field surveys. After the flood in 2013, the area of the new floodplain reached 57% (310 ha) of the original channel area.
topic danube
by-passed channel
land cover
alluvial forest
succession
url https://doi.org/10.1515/eko-2017-0015
work_keys_str_mv AT horackovasarka sedimentaryvegetationresponsetothechannelbypassacasestudyofthedanuberiver
AT lehotskymilan sedimentaryvegetationresponsetothechannelbypassacasestudyofthedanuberiver
AT stefanickatomas sedimentaryvegetationresponsetothechannelbypassacasestudyofthedanuberiver
AT viczianistvan sedimentaryvegetationresponsetothechannelbypassacasestudyofthedanuberiver
_version_ 1717785220768333824