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Confirmation of a theory: reconstruction of an alluvial plain development in a flume experiment

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    SYSNO ASEP0471459
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleConfirmation 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 authors6
    Source TitleErdkunde. - : Universitaet Bonn - ISSN 0014-0015
    Roč. 70, č. 3 (2016), s. 271-285
    Number of pages16 s.
    Languageeng - English
    CountryDE - Germany
    Keywordsfluvial geomorphology ; flume experiment ; avulsion
    Subject RIVDE - Earth Magnetism, Geodesy, Geography
    Institutional supportUGN-S - RVO:68145535
    UT WOS000384466800005
    EID SCOPUS84983738795
    DOI10.3112/erdkunde.2016.03.05
    AnnotationFluvial 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.
    WorkplaceInstitute of Geonics
    ContactLucie Gurková, lucie.gurkova@ugn.cas.cz, Tel.: 596 979 354
    Year of Publishing2017
Number of the records: 1  

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