Coarse bed sediments in a headwater channel as indicators of fluvial processes and slope-channel coupling: a case study from the Carpathian Mountains (Czech Republic)

Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61988987%3A17310%2F13%3AA14018DH" target="_blank" >RIV/61988987:17310/13:A14018DH - isvavai.cz</a>
Výsledek na webu
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DOI - Digital Object Identifier
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Jazyk výsledku
angličtina
Název v původním jazyce
Coarse bed sediments in a headwater channel as indicators of fluvial processes and slope-channel coupling: a case study from the Carpathian Mountains (Czech Republic)
Popis výsledku v původním jazyce
The character of riverbed sediments usually reflects fluvial processes and the dynamics of sediment transport in fluvial systems. The approach in this study was based on the measurement of the largest boulders located within a bankfull channel, and on the observation of changes in their size in the longitudinal profile of a headwater stream in the Moravian-Silesian Beskids Mountains.
Název v anglickém jazyce
Coarse bed sediments in a headwater channel as indicators of fluvial processes and slope-channel coupling: a case study from the Carpathian Mountains (Czech Republic)
Popis výsledku anglicky
The character of riverbed sediments usually reflects fluvial processes and the dynamics of sediment transport in fluvial systems. The approach in this study was based on the measurement of the largest boulders located within a bankfull channel, and on the observation of changes in their size in the longitudinal profile of a headwater stream in the Moravian-Silesian Beskids Mountains.

Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
DE - Zemský magnetismus, geodesie, geografie
OECD FORD obor
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Rok uplatnění
2013
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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