Response of the Danube River floodplain to flood events during 2002–2007 period

dc.contributor.authorLehotský, Milan
dc.contributor.authorNovotný, Ján
dc.contributor.authorSzmańda, Jacek B.
dc.date.accessioned2014-03-04T13:03:52Z
dc.date.available2014-03-04T13:03:52Z
dc.date.issued2010
dc.description.abstractThe relationship between floods and their geomorphic effect is discussed in this article. Almost every flood event is registered in overbank alluvia. We investigated sediment structures and textures as a response to three flood events occurred during 2002–2007 period on the Danube River floodplain in Bratislava. The change in sedimentation is the effect of floodwater flow energy changeability in the channel and floodplain. Generally, three main phases of energy flow changes of floods are recognised and thus the complete flood record can be expressed as the set of three layers. We also analysed conditions of the overbank sedimentation based on the shape and size of sedimented particles. Results show a relatively high variability of sedimentation processes during floods. The total amount of new overbank sediment accumulated in the 2002–2007 period, its texture characteristics and spatial distribution do not depend only on flood discharge, but also on the drainage basin sources of floodwater and sediment.pl_PL
dc.identifier.citationQuaestiones Geographicae vol. 29 (3), 2010, pp.37-45pl_PL
dc.identifier.isbn978-83-62662-62-3
dc.identifier.issn0137-477X
dc.identifier.urihttp://hdl.handle.net/10593/10250
dc.language.isoenpl_PL
dc.publisherWydział Nauk Geograficznych i Geologicznych Uniwersytetu im. Adama Mickiewiczapl_PL
dc.subjectthe Danube Riverpl_PL
dc.subjectflood recordpl_PL
dc.subjectgrain-size datapl_PL
dc.subjectvertical accretionpl_PL
dc.subjectfloodplain faciespl_PL
dc.titleResponse of the Danube River floodplain to flood events during 2002–2007 periodpl_PL
dc.typeArtykułpl_PL

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Uniwersytet im. Adama Mickiewicza w Poznaniu
Biblioteka Uniwersytetu im. Adama Mickiewicza w Poznaniu
Ministerstwo Nauki i Szkolnictwa Wyższego