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Linking sediment connectivity with sediment transport risk assessment in small forested catchments in the Czech Republic

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F24%3A00137703" target="_blank" >RIV/00216224:14310/24:00137703 - isvavai.cz</a>

  • Result on the web

    <a href="https://onlinelibrary.wiley.com/doi/10.1002/rra.4295" target="_blank" >https://onlinelibrary.wiley.com/doi/10.1002/rra.4295</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1002/rra.4295" target="_blank" >10.1002/rra.4295</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Linking sediment connectivity with sediment transport risk assessment in small forested catchments in the Czech Republic

  • Original language description

    Steep mountain environments are typically characterized by high sediment production. In the case of high hillslope-channel connectivity, high production and intensive transport of sediments are problematic and can cause damage in inhabited areas. At the end of the 19th century, due to flood events, large-scale torrent control measures were inappropriately applied, disrupting the natural processes, and riparian and water ecosystems in watersheds. Connectivity in watersheds affects the course and magnitude of hazards that threaten human society. This is also why the topic of connectivity should be considered in the management of watercourses. Our study links the issue of sediment connectivity (lateral/longitudinal) and the sediment transport-related risk in unmeasured forested watersheds Hu &amp; ccaron;iv &amp; aacute; Desn &amp; aacute; and Upper Moravice. We applied a methodology for sediment transport-related risk assessment and the well-established effective catchment area (ECA) approach and connectivity index (IC) to two headwater streams. The results showed the parts of the streams with the highest degree of hazard related to sediment transport and sediment contribution areas connected to them. Based on the field survey, it was found that the best suitable threshold for ECA delineation for Hu &amp; ccaron;iv &amp; aacute; Desn &amp; aacute; catchments is 8 degrees and for Upper Moravice is 10 degrees. Area of sediment contribution areas for Hu &amp; ccaron;iv &amp; aacute; Desn &amp; aacute; is four times bigger than for Upper Moravice. The Hu &amp; ccaron;iva Desn &amp; aacute;, therefore, has a higher potential sediment supply from the slopes, which also increases the possibility of occurrence of hazards associated with the sediment transport regime. All three applied methods confirmed that the parallel roads along channels decrease slope-channel connectivity, especially in the Upper Moravice catchment. The combination of methodologies created a suitable tool to identify the most problematic stretches of streams in terms of sediment connectivity and risk related to sediment transport, which can be useful for water and sediment management in unmeasured forested watersheds.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10500 - Earth and related environmental sciences

Result continuities

  • Project

  • Continuities

    S - Specificky vyzkum na vysokych skolach<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2024

  • Confidentiality

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

Data specific for result type

  • Name of the periodical

    River Research and Applications

  • ISSN

    1535-1459

  • e-ISSN

    1535-1467

  • Volume of the periodical

    40

  • Issue of the periodical within the volume

    7

  • Country of publishing house

    US - UNITED STATES

  • Number of pages

    20

  • Pages from-to

    1343-1362

  • UT code for WoS article

    001228492100001

  • EID of the result in the Scopus database

    2-s2.0-85193744353