Number of the records: 1  

Behavior of spring discharge dynamic at forest and grassland mountain catchments

  1. 1.
    SYSNO ASEP0090712
    Document TypeA - Abstract
    R&D Document TypeThe record was not marked in the RIV
    R&D Document TypeNení vybrán druh dokumentu
    TitleBehavior of spring discharge dynamic at forest and grassland mountain catchments
    TitleBehavior of spring discharge dynamic at forest and grassland mountain catchmentsDynamika jarních odtoků z pramene v horském lesním a lučním povodí
    Author(s) Pavelka, Marian (UEK-B) RID, ORCID, SAI
    Acosta, Manuel (UEK-B) RID, ORCID, SAI
    Janouš, Dalibor (UEK-B) RID, SAI
    Czerný, Radek (UEK-B) ORCID, SAI
    Tomášková, Ivana (UEK-B)
    Source TitleThe Beskyds Buletin - ISBN 978-80-7375-069-5
    Roč. 1, č. 20 (2007), s. 55-60
    Number of pages6 s.
    Languageeng - English
    CountryCZ - Czech Republic
    Keywordsprecipitation ; spring discharge ; evapotranspiration ; Norway spruce ; grassland ; roots
    Subject RIVGK - Forestry
    R&D Projects1P05OC027 GA MŠMT - Ministry of Education, Youth and Sports (MEYS)
    CEZAV0Z60870520 - UEK-B (2005-2011)
    AnnotationIn this study we measured precipitation, spring discharge and evapotranspiration in order to explain the existence of diurnal oscillation of spring discharge presented at forest stand catchment and its comparison with grassland spring discharge. Measurements were carried out in forest stand and a grassland site at the Ecological Experimental Study Site Bily Kriz, Moravian-Silesian Beskydy Mts., the Czech Republic. Even thought, precipitation at the forest and the grassland sites were without significant differences and both spring are of the same type, difference between courses of spring discharge were found during the period after raining. Our time series analysis supported the hypothesis that the forest spring discharge oscillation responds to the evapotranspiration.
    Description in EnglishIn this study we measured precipitation, spring discharge and evapotranspiration in order to explain the existence of diurnal oscillation of spring discharge presented at forest stand catchment and its comparison with grassland spring discharge. Measurements were carried out in forest stand and a grassland site at the Ecological Experimental Study Site Bily Kriz, Moravian-Silesian Beskydy Mts., the Czech Republic. Even thought, precipitation at the forest and the grassland sites were without significant differences and both spring are of the same type, difference between courses of spring discharge were found during the period after raining. Our time series analysis supported the hypothesis that the forest spring discharge oscillation responds to the evapotranspiration.
    WorkplaceGlobal Change Research Institute
    ContactNikola Šviková, svikova.n@czechglobe.cz, Tel.: 511 192 268
    Year of Publishing2008
Number of the records: 1  

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