Počet záznamů: 1
Confirmation of a theory: reconstruction of an alluvial plain development in a flume experiment
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SYSNO ASEP 0471459 Druh ASEP J - Článek v odborném periodiku Zařazení RIV J - Článek v odborném periodiku Poddruh J Článek ve WOS Název Confirmation of a theory: reconstruction of an alluvial plain development in a flume experiment Tvůrce(i) Bertalan, L. (HU)
Tóth, C. A. (HU)
Szabó, G. (HU)
Nagy, G. (HU)
Kuda, František (UGN-S) RID, ORCID
Szabó, S. (HU)Celkový počet autorů 6 Zdroj.dok. Erdkunde. - : Universitaet Bonn - ISSN 0014-0015
Roč. 70, č. 3 (2016), s. 271-285Poč.str. 16 s. Jazyk dok. eng - angličtina Země vyd. DE - Německo Klíč. slova fluvial geomorphology ; flume experiment ; avulsion Vědní obor RIV DE - Zemský magnetismus, geodézie, geografie Institucionální podpora UGN-S - RVO:68145535 UT WOS 000384466800005 EID SCOPUS 84983738795 DOI 10.3112/erdkunde.2016.03.05 Anotace Fluvial geomorphologists have tried to describe the outstanding tectonically affected avulsion process of Tisza River at the Great Hungarian Plain by various theoretical concepts. Flume experiments provide the ability to examine the main characteristic processes of a highlighted surface development theory under controlled settings within an accelerated time scale. Our goal was to reconstruct and refine these hypotheses from a new experimental point of view. In this study we performed an experiment of the avulsion process mentioned above on a 12 x 5 x 2.5 m flume where a special instrument was planted under the sand layers in order to simulate the vertical tectonic movements. A terrestrial laser scanner was used to record the different stages of the topographic evolution. Pracoviště Ústav geoniky Kontakt Lucie Gurková, lucie.gurkova@ugn.cas.cz, Tel.: 596 979 354 Rok sběru 2017
Počet záznamů: 1