Number of the records: 1  

Different harvest intensity and soil CO2 efflux in sessile oak coppice forests

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    SYSNO ASEP0461928
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleDifferent harvest intensity and soil CO2 efflux in sessile oak coppice forests
    Author(s) Dařenová, Eva (UEK-B) RID, ORCID, SAI
    Majtaz, C. (SI)
    Pavelka, Marian (UEK-B) RID, ORCID, SAI
    Source TitleiForest – Biogeosciences and Forestry. - : SISEF Societa Italiana di Selvicoltura ed Ecologia Forestale - ISSN 1971-7458
    Roč. 9, feb (2016), s. 546-552
    Number of pages7 s.
    Languageeng - English
    CountryIT - Italy
    KeywordsLow Forest ; Soil Moisture ; Soil Respiration ; Temperature Dependence
    Subject RIVGK - Forestry
    R&D ProjectsLO1415 GA MŠMT - Ministry of Education, Youth and Sports (MEYS)
    EE2.3.20.0267 GA MŠMT - Ministry of Education, Youth and Sports (MEYS)
    Research InfrastructureCzeCOS II - 90061 - Ústav výzkumu globální změny AV ČR, v. v. i.
    Institutional supportRVO:67179843 - RVO:67179843
    UT WOS000384724700005
    EID SCOPUS84991380036
    DOI10.3832/ifor1773-009
    AnnotationSoil CO2 efflux accounts for about 45-80% of total ecosystem respiration and is therefore an important part of the ecosystem carbon cycle. Soil CO2 efflux has been poorly studied in forests managed in the ancient coppicing manner. In our study, soil CO2 efflux, temperature, and moisture were measured in sessile oak stands with different harvesting intensity (control: 0% intensity; V1: 75%; V2: 80 %; V3: 85%; and V4: 100%) during the fifth and sixth years after harvesting. Soil CO2 efflux was in the range 2-8 µmol CO2 m-2 s-1 and indicated an increasing pattern with increasing harvesting intensity. The slope of that pattern became less steep from the fifth to the sixth year after harvesting, thus indicating gradual recovery of soil carbon dynamics in the coppiced stand toward the equilibrium state existing before harvesting. Temperature sensitivity of soil CO2 efflux ranged between 2.1 and 2.8, with the lowest values measured in the control stand. Soil CO2 efflux in the control stand was more sensitive to changes in soil moisture than was that on harvested plots. By our calculations, 6.2 tC ha-1 was released from the control stand and 6.2-6.8 tC ha-1 from the harvested stands during the sixth year after harvesting. If mean temperature were to rise by 1 °C, the amount of soil carbon released would increase by 7.7% in the control stand and, depending on harvesting intensity, by 9.0-10.8% in the harvested stands.
    WorkplaceGlobal Change Research Institute
    ContactNikola Šviková, svikova.n@czechglobe.cz, Tel.: 511 192 268
    Year of Publishing2017
Number of the records: 1  

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