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Different harvest intensity and soil CO2 efflux in sessile oak coppice forests
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SYSNO ASEP 0461928 Druh ASEP J - Článek v odborném periodiku Zařazení RIV J - Článek v odborném periodiku Poddruh J Článek ve WOS Název Different harvest intensity and soil CO2 efflux in sessile oak coppice forests Tvůrce(i) Dařenová, Eva (UEK-B) RID, ORCID, SAI
Majtaz, C. (SI)
Pavelka, Marian (UEK-B) RID, ORCID, SAIZdroj.dok. iForest – Biogeosciences and Forestry. - : SISEF Societa Italiana di Selvicoltura ed Ecologia Forestale - ISSN 1971-7458
Roč. 9, feb (2016), s. 546-552Poč.str. 7 s. Jazyk dok. eng - angličtina Země vyd. IT - Itálie Klíč. slova Low Forest ; Soil Moisture ; Soil Respiration ; Temperature Dependence Vědní obor RIV GK - Lesnictví CEP LO1415 GA MŠMT - Ministerstvo školství, mládeže a tělovýchovy EE2.3.20.0267 GA MŠMT - Ministerstvo školství, mládeže a tělovýchovy Výzkumná infrastruktura CzeCOS II - 90061 - Ústav výzkumu globální změny AV ČR, v. v. i. Institucionální podpora RVO:67179843 - RVO:67179843 UT WOS 000384724700005 EID SCOPUS 84991380036 DOI 10.3832/ifor1773-009 Anotace Soil 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. Pracoviště Ústav výzkumu globální změny Kontakt Nikola Šviková, svikova.n@czechglobe.cz, Tel.: 511 192 268 Rok sběru 2017
Počet záznamů: 1