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Seasonal course of CO2 efflux in grassland and forest ecosystem in Beskydy mts

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    SYSNO ASEP0312468
    Document TypeK - Proceedings Paper (Czech conf.)
    R&D Document TypeThe record was not marked in the RIV
    TitleSeasonal course of CO2 efflux in grassland and forest ecosystem in Beskydy mts
    Author(s) Dařenová, Eva (UEK-B) RID, ORCID, SAI
    Pavelka, Marian (UEK-B) RID, ORCID, SAI
    Acosta, Manuel (UEK-B) RID, ORCID, SAI
    Janouš, Dalibor (UEK-B) RID, SAI
    Number of authors4
    Source TitleBioklimatologické aspekty hodnocení procesů v krajině. Sborník příspěvků z mezinárodní konference. - Praha : ČHMÚ, 2008 / Rožnovský J. ; Litschmann T. - ISBN 978-80-86690-55-1
    Number of pages10 s.84
    Publication formCD - CD
    ActionBioklimatologické aspekty hodnocení procesů v krajině
    Event date09.09.2008-11.09.2008
    VEvent locationMikulov
    CountryCZ - Czech Republic
    Event typeEUR
    Languageeng - English
    CountryCZ - Czech Republic
    KeywordsCO2 efflux ; grassland ; forest ; soil ; stem
    Subject RIVGK - Forestry
    R&D Projects2B06068 GA MŠMT - Ministry of Education, Youth and Sports (MEYS)
    1P05OC027 GA MŠMT - Ministry of Education, Youth and Sports (MEYS)
    CEZAV0Z60870520 - UEK-B (2005-2011)
    AnnotationOur aim was to determine seasonal changes of CO2 efflux of the grassland and of the soil and stems in the Spruce forest at Bílý Kříž (Beskydy Mts). For elimination of the temperature dependency of CO2 efflux, standardized CO2 efflux R10 is used. Mean R10 was about 2.50, 5.0 and 0.97 umolCO2 m-2 s-1 for grassland, forest soil and stems. In grassland the R10 course did not show obvious trend. Whereas in the forest soil, the significant increase in R10 at the beginning and decrease at the end of the season occurred, but without any distinct maximum. Similar increase and decrease in R10 was observed in the stem CO2 efflux course as well. But there was a maximum in June and July. The temperature CO2 efflux sensitivity (Q10) was 3.04, 1.90 and 2.25 for the grassland, forest soil and stems. The temperature sensitivity in the forest soil increased shortly after rain. It resulted in a rapid increase in CO2 efflux of the soil as a response to rain.
    WorkplaceGlobal Change Research Institute
    ContactNikola Šviková, svikova.n@czechglobe.cz, Tel.: 511 192 268
    Year of Publishing2011
Number of the records: 1  

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