Počet záznamů: 1  

Trees as net sinks for nitrous oxide (N2O) and methane (CH4) in tropical rain forest on La Reunion island

  1. 1.
    SYSNO ASEP0518577
    Druh ASEPA - Abstrakt
    Zařazení RIVZáznam nebyl označen do RIV
    Zařazení RIVNení vybrán druh dokumentu
    NázevTrees as net sinks for nitrous oxide (N2O) and methane (CH4) in tropical rain forest on La Reunion island
    Tvůrce(i) Macháčová, Kateřina (UEK-B) RID, ORCID, SAI
    Borák, Libor (UEK-B) SAI, ORCID
    Agyei, Thomas (UEK-B) ORCID, SAI, RID
    Zdroj.dok.Geophysical Research Abstracts, 21. - : European geoscience union, 2019
    Poč.str.1 s.
    AkceEGU General Assembly Conference 2019
    Datum konání07.04.2019 - 12.04.2019
    Místo konáníVídeň
    ZeměAT - Rakousko
    Typ akceEUR
    Jazyk dok.eng - angličtina
    Klíč. slovan2o ; ch4 ; greenhouse gas ; tropical rain forest ; lava flow ; volcanic ; tree stem ; soil ; ftir ; exchange ; flux ; uptake ; sink
    Vědní obor RIVGK - Lesnictví
    Obor OECDForestry
    CEPGJ17-18112Y GA ČR - Grantová agentura ČR
    Výzkumná infrastrukturaCzeCOS III - 90123 - Ústav výzkumu globální změny AV ČR, v. v. i.
    Institucionální podporaUEK-B - RVO:86652079
    AnotaceTropical forests are considered a natural sink for methane (CH4) and a natural source of nitrous oxide (N2O), both important greenhouse gases (GHGs). Forest ecosystem exchange of CH4 and N2O has been mostly estimated based on GHGs exchange at the soil–atmosphere interface only. However, trees of various climatic zones are known to emit CH4 and N2O into the atmosphere. Recent research revealed tropical wetland trees as considerable sources of CH4. Nevertheless, there is little known about CH4 and N2O exchange capacity of tropical trees growing under „non-flooded“ conditions. We determined CH4 and N2O exchange of soil and stems of mostly endemic tree species in a tropical lowland rain forest on lava flow of La Reunion Island in the South Western Indian Ocean. We investigated (1) whether the tree stems exchange CH4 and N2O with the atmosphere, (2) how the tree fluxes contribute to the forest GHGs exchange, and (3) whether the tropical rain forest is a source or sink for CH4 and N2O at the beginning of the rain season. The experiment was performed in Mare-Longue Nature Reserve in October-November 2018. The studied forest is situated on 400 years old basaltic lava flow covered with irregular and thin soil layer. Fluxes of CH4 and N2O in mature tree stems and soil were measured using non-steady-state chamber systems and a portable FTIR gas analyser. The stems of studied tree species were net sinks for both CH4 (-15.1 ± 2.2 µg CH4 m-2 stem area h-1) and N2O (-3.1 ± 0.8 µg N2O m-2 h-1). Such uptake potential for CH4 and N2O by tropical tree species represents a novel and unique finding which is in contrast to current limited studies presenting tropical trees as CH4 emitters. The soil was a significant net CH4 sink (-79.5 ± 11.5 µg CH4 m-2 soil area h-1). The soil N2O fluxes showed a high spatial heterogeneity including both N2O emissions and uptake (net flux -0.18 ± 1.61 µg N2O m-2 h-1). Concluded, the studied tropical tree species were net sinks for CH4 and N2O.
    PracovištěÚstav výzkumu globální změny
    KontaktNikola Šviková, svikova.n@czechglobe.cz, Tel.: 511 192 268
    Rok sběru2020
Počet záznamů: 1  

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