Vše

Co hledáte?

Vše
Projekty
Výsledky výzkumu
Subjekty

Rychlé hledání

  • Projekty podpořené TA ČR
  • Významné projekty
  • Projekty s nejvyšší státní podporou
  • Aktuálně běžící projekty

Chytré vyhledávání

  • Takto najdu konkrétní +slovo
  • Takto z výsledků -slovo zcela vynechám
  • “Takto můžu najít celou frázi”

SEASONAL DYNAMICS OF N2O AND CH4 FLUXES OF BOREAL TREE STEMS

Identifikátory výsledku

  • Kód výsledku v IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F86652079%3A_____%2F19%3A00517361" target="_blank" >RIV/86652079:_____/19:00517361 - isvavai.cz</a>

  • Výsledek na webu

  • DOI - Digital Object Identifier

Alternativní jazyky

  • Jazyk výsledku

    angličtina

  • Název v původním jazyce

    SEASONAL DYNAMICS OF N2O AND CH4 FLUXES OF BOREAL TREE STEMS

  • Popis výsledku v původním jazyce

    Boreal forest soils are a natural source of nitrous oxide (N2O) and a sink of methane (CH4). Trees can contribute to ecosystem N2O and CH4 exchange (1) by transporting the gases from soil to the atmosphere, (2) by producing these gases in situ in the plant tissues, (3) by consuming these gases from the atmosphere, or (4) indirectly by altering the soil biochemical or physical conditions. Studies on the N2O and CH4 exchange of mature trees growing in natural field conditions are rare, and the boreal zone trees have not gained much attention. Studies on the seasonality of the tree CH4 and N2O fluxes have been lacking. We measured the stem fluxes of N2O and CH4 from mature pine, spruce and birch trees at three plots with naturally different soil moisture ( soil volumetric water content): Wet (0.81 m 3 m −3 ), moderately wet (0.40 m 3 m −3 ), and dry (0.21 m 3 m −3 ). The fluxes were determined between June 2014 and May 2015, using static chambers and gas chromatographic analyses. There were significant seasonal dynamics in the stem N2O and CH4 exchange. The N2O exchange was clearly connected to the tree physiological activity, while the CH4 flux had only weak relation to physiological activity. Positive correlation between N2O flux and evapotranspiration supports our hypothesis that N2O is transported from soil via the transpiration stream. The CH4 fluxes of birch and pine trees were clearly connected to the soil moisture, unlike the spruce fluxes. The forest floor was a source of N2O at all plots, while the CH4 flux was connected to the soil moisture (wet plot was a source, other plots were sinks).

  • Název v anglickém jazyce

    SEASONAL DYNAMICS OF N2O AND CH4 FLUXES OF BOREAL TREE STEMS

  • Popis výsledku anglicky

    Boreal forest soils are a natural source of nitrous oxide (N2O) and a sink of methane (CH4). Trees can contribute to ecosystem N2O and CH4 exchange (1) by transporting the gases from soil to the atmosphere, (2) by producing these gases in situ in the plant tissues, (3) by consuming these gases from the atmosphere, or (4) indirectly by altering the soil biochemical or physical conditions. Studies on the N2O and CH4 exchange of mature trees growing in natural field conditions are rare, and the boreal zone trees have not gained much attention. Studies on the seasonality of the tree CH4 and N2O fluxes have been lacking. We measured the stem fluxes of N2O and CH4 from mature pine, spruce and birch trees at three plots with naturally different soil moisture ( soil volumetric water content): Wet (0.81 m 3 m −3 ), moderately wet (0.40 m 3 m −3 ), and dry (0.21 m 3 m −3 ). The fluxes were determined between June 2014 and May 2015, using static chambers and gas chromatographic analyses. There were significant seasonal dynamics in the stem N2O and CH4 exchange. The N2O exchange was clearly connected to the tree physiological activity, while the CH4 flux had only weak relation to physiological activity. Positive correlation between N2O flux and evapotranspiration supports our hypothesis that N2O is transported from soil via the transpiration stream. The CH4 fluxes of birch and pine trees were clearly connected to the soil moisture, unlike the spruce fluxes. The forest floor was a source of N2O at all plots, while the CH4 flux was connected to the soil moisture (wet plot was a source, other plots were sinks).

Klasifikace

  • Druh

    D - Stať ve sborníku

  • CEP obor

  • OECD FORD obor

    10611 - Plant sciences, botany

Návaznosti výsledku

  • Projekt

    <a href="/cs/project/GJ17-18112Y" target="_blank" >GJ17-18112Y: Toky metanu a oxidu dusného z různých druhů stromů temperátního a boreálního lesa</a><br>

  • Návaznosti

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Ostatní

  • Rok uplatnění

    2019

  • Kód důvěrnosti údajů

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Údaje specifické pro druh výsledku

  • Název statě ve sborníku

    REPORT SERIES IN AEROSOL SCIENCE - Proceedings of The Center of Excellence in Atmospheric Science (CoE ATM)

  • ISBN

    978-952-7276-34-1

  • ISSN

    0784-3496

  • e-ISSN

  • Počet stran výsledku

    3

  • Strana od-do

    423-426

  • Název nakladatele

    Aerosolitutkimusseura ry – Finnish Association for Aerosol Research FAAR

  • Místo vydání

    Helsinki

  • Místo konání akce

    Helsinki

  • Datum konání akce

    25. 11. 2019

  • Typ akce podle státní příslušnosti

    EUR - Evropská akce

  • Kód UT WoS článku