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Downstream fining trends of gravel bar sediments: A case study of czech carpathian rivers

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61988987%3A17310%2F20%3AA21026YF" target="_blank" >RIV/61988987:17310/20:A21026YF - isvavai.cz</a>

  • Result on the web

    <a href="http://aucgeographica.cz/index.php/aucg/article/view/214" target="_blank" >http://aucgeographica.cz/index.php/aucg/article/view/214</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.14712/23361980.2020.17" target="_blank" >10.14712/23361980.2020.17</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Downstream fining trends of gravel bar sediments: A case study of czech carpathian rivers

  • Original language description

    This study examines downstream grain-size trends in gravel bars, a typical feature of natural gravel-bed rivers, from two neighbouring heavily channelized rivers: The Lubina River and the Ondrejnice River draining the Czech part of the Outer Western Carpathians. It aims to examine the effects of the grade control structures, significant tributaries, and lateral sediment inputs on the downstream fining trends. Additionally, the relationship between the channel width and the grain sizes in bars was analysed, as well as the depositional trends in frontal, central and distal parts of the examined gravel bars. The Ondrejnice River has, in most cases, higher D50 and median values of grain size of bar sediment and a higher downstream reduction coefficient (D50 = 0.033 mm km-1; D84 = 0.036 mm km-1) than the Lubina River (D50 = 0.026 mm km-1; D84 = 0.032 mm km-1). These intense reduction trends in the grain size are often observed in single and multiple-threaded rivers in the Western Carpathians. On both rivers, the predominant deposition of the highest D50 was detected in the central parts of the bars, and the wider channel widths often corresponded with finer sediment deposition in the Lubina River. The disruption of the downstream fining corresponded in some cases with the frequent grade control structures. However, in most cases, the downstream fining trends were not affected. A tributary and adjacent hillslope area could be possibly linked to the disruption of the downstream fining trend in the Ondrejnice River.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>SC</sub> - Article in a specialist periodical, which is included in the SCOPUS database

  • CEP classification

  • OECD FORD branch

    10508 - Physical geography

Result continuities

  • Project

  • Continuities

    S - Specificky vyzkum na vysokych skolach

Others

  • Publication year

    2020

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Acta Universitatis Carolinae, Geographica

  • ISSN

    0300-5402

  • e-ISSN

  • Volume of the periodical

    55

  • Issue of the periodical within the volume

    2

  • Country of publishing house

    CZ - CZECH REPUBLIC

  • Number of pages

    14

  • Pages from-to

    229-242

  • UT code for WoS article

  • EID of the result in the Scopus database

    2-s2.0-85096876178