Coarse bed sediments in headwater streams: imprints of slope-channel coupling and development of a channel

Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61988987%3A17310%2F13%3AA140180R" target="_blank" >RIV/61988987:17310/13:A140180R - isvavai.cz</a>
Result on the web
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DOI - Digital Object Identifier
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Result language
angličtina
Original language name
Coarse bed sediments in headwater streams: imprints of slope-channel coupling and development of a channel
Original language description
Analyzed longitudinal profile of the Lubina (1.03 km) showed close relationship between slope-channel processes, trends of aggradation or incision and mean sizes of five largest boulders. The largest sizes of boulders were observed in the uppermost partsof the profile with high intensity of sediment delivery from steep adjacted hillslopes. By contrast, much finer sediments were found in reaches of alluvial cone with recent depositional trends. General fining of bed sediments occurred at 0.0-0.8 km at the transition from slope-channel coupling segment to alluvial cone, later switched to coarsening trend in recently deeply incising channel-reaches (0.8-1.03 km).
Czech name
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Czech description
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Project
<a href="/en/project/GAP209%2F10%2F0309" target="_blank" >GAP209/10/0309: Effect of historical climatic and hydrometeorological extremes on slope and fluvial processes in the Western Beskydy Mts. and their forefield</a><br>
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Publication year
2013
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Article name in the collection
Geomorfologický sborník 11
ISBN
978-80-86407-37-1
ISSN
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e-ISSN
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Number of pages
1
Pages from-to
11-11
Publisher name
Ústav geoniky AV ČR, v.v.i.; Geografický ústav, PřF, Masarykova univerzita
Place of publication
Ostrava,Brno
Event location
Mikulov
Event date
Apr 24, 2013
Type of event by nationality
EUR - Evropská akce
UT code for WoS article
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