Number of the records: 1  

Chamber techniques versus eddy covariance method during nighttime measurements

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    SYSNO ASEP0341976
    Document TypeG - Proceedings (int. conf.)
    R&D Document TypeO - Ostatní
    TitleChamber techniques versus eddy covariance method during nighttime measurements
    TitleKomorové techniky versus eddy kovariační metody během nočních měření
    Author(s) Pavelka, Marian (UEK-B) RID, ORCID, SAI
    Sedlák, Pavel (UEK-B) RID, ORCID, SAI
    Acosta, Manuel (UEK-B) RID, ORCID, SAI
    Czerný, Radek (UEK-B) ORCID, SAI
    Taufarová, Klára (UEK-B) RID, SAI
    Janouš, Dalibor (UEK-B) RID, SAI
    Issue dataZvolen: Slovak bioclimatological society, 2007
    ISBN978-80-228-1760-8
    Number of pages8 s.
    Publication formCD-Rom - CD-Rom
    ActionBioclimatology and natural hazards
    Event date17.09.2007-20.09.2007
    VEvent locationPolana nad Detvou
    CountrySK - Slovakia
    Event typeEUR
    Languageeng - English
    CountrySK - Slovakia
    KeywordsEddy covariance ; Friction velocity ; chamber ; grassland ; net radiation
    Subject RIVEF - Botanics
    R&D ProjectsSM/640/18/03 GA MŽP - Ministry of Environment (MŽP)
    SM/630/2/03 GA MŽP - Ministry of Environment (MŽP)
    CEZAV0Z60870520 - UEK-B (2005-2011)
    AnnotationThe parameter Q10 is commonly used to express the relationship between soil CO2 efflux and soil temperature. Soil surface CO2 efflux and soil temperature at different depths were measured in a 21-year-old Norway spruce stand and a mountain grassland site (Bily Kriz, Beskydy Mts., Czech Republic), using automated gasometric systems. A time-delay and goodness-of-fit between soil CO2 efflux and soil temperature at different measuring depths were determined. Wide ranges of values for the time-delay of CO2 efflux in response to temperature, Q10 and the determination coefficient (R2) between CO2 efflux and temperature were obtained. The values of Q10 and the CO2 time-delay increased with depth of soil temperature measurement point, while the R2 of the CO2-temperature relationship significantly decreased. Measurement of soil temperature at very shallow soil layer, preferably at the soil surface, is highly recommended to determine useable values of Q10.
    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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