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Confirmation of a theory: reconstruction of an alluvial plain development in a flume experiment
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SYSNO ASEP 0471459 Document Type J - Journal Article R&D Document Type Journal Article Subsidiary J Článek ve WOS Title Confirmation of a theory: reconstruction of an alluvial plain development in a flume experiment Author(s) Bertalan, L. (HU)
Tóth, C. A. (HU)
Szabó, G. (HU)
Nagy, G. (HU)
Kuda, František (UGN-S) RID, ORCID
Szabó, S. (HU)Number of authors 6 Source Title Erdkunde. - : Universitaet Bonn - ISSN 0014-0015
Roč. 70, č. 3 (2016), s. 271-285Number of pages 16 s. Language eng - English Country DE - Germany Keywords fluvial geomorphology ; flume experiment ; avulsion Subject RIV DE - Earth Magnetism, Geodesy, Geography Institutional support UGN-S - RVO:68145535 UT WOS 000384466800005 EID SCOPUS 84983738795 DOI 10.3112/erdkunde.2016.03.05 Annotation 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. Workplace Institute of Geonics Contact Lucie Gurková, lucie.gurkova@ugn.cas.cz, Tel.: 596 979 354 Year of Publishing 2017
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