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  • Two long lasting ponded infiltration experiments with application of a pulse of Rhodamine- G, as a tracer, detected continuously by means of two Turner 10-AU fluorometers equipped with the flow cells, were performed on the hillslope at the small experimental watershed Uhlirska during vegetation season of 1999. During semi-steady flow of each infiltration experiment, distinct long lasting pulse of Rhodamine - G was added. Both experiments were performed under different initial hydrological conditions and resulted in different hydraulic behavior and spatially heterogeneous non-Darcian distribution of subsurface runoff. Despite that, the shape of solute breakthrough curves for both experiments is similar, indicating portions of the outflow from the watershed (shallow subsurface outflow and deep percolation) as a result of infiltration.
  • Two long lasting ponded infiltration experiments with application of a pulse of Rhodamine- G, as a tracer, detected continuously by means of two Turner 10-AU fluorometers equipped with the flow cells, were performed on the hillslope at the small experimental watershed Uhlirska during vegetation season of 1999. During semi-steady flow of each infiltration experiment, distinct long lasting pulse of Rhodamine - G was added. Both experiments were performed under different initial hydrological conditions and resulted in different hydraulic behavior and spatially heterogeneous non-Darcian distribution of subsurface runoff. Despite that, the shape of solute breakthrough curves for both experiments is similar, indicating portions of the outflow from the watershed (shallow subsurface outflow and deep percolation) as a result of infiltration. (en)
  • Dva dlouhodobé výtopové infiltrační experimenty s aplikací pulsu značkovače Rhodamin G, který byl kontinuálně detekován dvojicí fluorometrů Turner 10-AU, byly provedeny na svahu malého experimentálního povodí Uhlířská během vegetační sezóny 1999. Během kvazi ustáleného proudění každé infiltrace byl aplikován dlouhý puls Rhodaminu G. Oba experimenty byly provedeny za různých hydrologických podmínek. Výsledky experimentů se mezi sebou lišily hydraulickým chováním a vykazovaly prostorově heterogenní nedarcyovskou distribuci podpovrchového odtoku. I přes to byl tvar průnikových křivek podobný pro oba experimenty a indikoval podíly výtoku z povodí (mělký podpovrchový a hluboký perkolační) . (cs)
Title
  • Ponded Infiltration Test in Field Using Fluorescent Dye
  • Ponded Infiltration Test in Field Using Fluorescent Dye (en)
  • Terénní výpová infiltrace s použitím fluorescenčního značkovače (cs)
skos:prefLabel
  • Ponded Infiltration Test in Field Using Fluorescent Dye
  • Ponded Infiltration Test in Field Using Fluorescent Dye (en)
  • Terénní výpová infiltrace s použitím fluorescenčního značkovače (cs)
skos:notation
  • RIV/68407700:21110/05:01116001!RIV06-MZP-21110___
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(IBS2060104), P(SA/650/5/03)
http://linked.open...vai/riv/dodaniDat
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  • 536734
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  • RIV/68407700:21110/05:01116001
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  • Cambisols; Infiltration experiment; Preferential flow; Tracer; Vadose zone (en)
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http://linked.open...i/riv/kodPristupu
http://linked.open...ontrolniKodProRIV
  • [6357B793802F]
http://linked.open...i/riv/mistoVydani
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http://linked.open...vavai/riv/projekt
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  • Císlerová, Milena
  • Šanda, Martin
  • Picek, Tomáš
http://localhost/t...ganizacniJednotka
  • 21110
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