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Experimental observation of subsurface flow along the compacted subsoil with use of rainfall simulator

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68407700%3A21110%2F14%3A00222258" target="_blank" >RIV/68407700:21110/14:00222258 - isvavai.cz</a>

  • Result on the web

  • DOI - Digital Object Identifier

Alternative languages

  • Result language

    čeština

  • Original language name

    Experimentální sledování podpovrchového odtoku po zhutnělé podorniční vrstvě s využitím dešťového simulátoru

  • Original language description

    The aim of the study is to explain the runoff formation and confirm validity of our conceptual model of quick runoff generation on inclined cultivated soils. Within former observations a compacted subsoil layer was identified, which could significantly contribute to quick runoff response even during low-intensity rainfall events. Using a mobile rainfall simulator the 16 m2 inclined experimental plot was successively exposed to artificial rainfalls with intensity and duration ranging from 23 to 64 mm/hour and from 60 to 155 minutes respectively. The dynamics of surface and shallow subsurface runoff and soil water regime in three depths were monitored. Various initial soil moisture conditions as well as vegetation stages from cultivated fallow to stubbledelimited the simulations. In relation to rainfall intensity and duration variable proportions of both monitored runoff components were observed, ranging from zero surface runoff to its distinct dominance. Both components interacted very

  • Czech name

    Experimentální sledování podpovrchového odtoku po zhutnělé podorniční vrstvě s využitím dešťového simulátoru

  • Czech description

    The aim of the study is to explain the runoff formation and confirm validity of our conceptual model of quick runoff generation on inclined cultivated soils. Within former observations a compacted subsoil layer was identified, which could significantly contribute to quick runoff response even during low-intensity rainfall events. Using a mobile rainfall simulator the 16 m2 inclined experimental plot was successively exposed to artificial rainfalls with intensity and duration ranging from 23 to 64 mm/hour and from 60 to 155 minutes respectively. The dynamics of surface and shallow subsurface runoff and soil water regime in three depths were monitored. Various initial soil moisture conditions as well as vegetation stages from cultivated fallow to stubbledelimited the simulations. In relation to rainfall intensity and duration variable proportions of both monitored runoff components were observed, ranging from zero surface runoff to its distinct dominance. Both components interacted very

Classification

  • Type

    D - Article in proceedings

  • CEP classification

    DA - Hydrology and limnology

  • OECD FORD branch

Result continuities

  • Project

    <a href="/en/project/GP13-20388P" target="_blank" >GP13-20388P: Dynamics of water runoff generation and soil erosion as a result of temporary variable soil structure and soil properties on a cultivated catchment</a><br>

  • Continuities

    S - Specificky vyzkum na vysokych skolach

Others

  • Publication year

    2014

  • Confidentiality

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

Data specific for result type

  • Article name in the collection

    Zborník recenzovaných príspevkov - 21. Posterový deň s medzinárodnou účasťou

  • ISBN

    978-80-89139-33-0

  • ISSN

  • e-ISSN

  • Number of pages

    12

  • Pages from-to

    300-311

  • Publisher name

    Ústav hydrológie SAV

  • Place of publication

    Bratislava

  • Event location

    Bratislava

  • Event date

    Nov 13, 2014

  • Type of event by nationality

    WRD - Celosvětová akce

  • UT code for WoS article