Ecosystem respiration in a heterogeneous temperate peatland and its sensitivity to peat temperature and water table depth
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67179843%3A_____%2F13%3A00380461" target="_blank" >RIV/67179843:_____/13:00380461 - isvavai.cz</a>
Výsledek na webu
<a href="http://dx.doi.org/10.1007/s11104-012-1441-y" target="_blank" >http://dx.doi.org/10.1007/s11104-012-1441-y</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1007/s11104-012-1441-y" target="_blank" >10.1007/s11104-012-1441-y</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Ecosystem respiration in a heterogeneous temperate peatland and its sensitivity to peat temperature and water table depth
Popis výsledku v původním jazyce
Background and aims Ecosystem respiration (R eco ) is controlled by thermal and hydrologic regimes, but their relative importance in defining the CO2 emissions in peatlands seems to be site specific. The aim of the paper is to investigate the sensitivityof R eco to variations in temperature and water table depth (WTD) in a wet, geogenous temperate peatland. Methods The CO2 fluxes were measured using chambers. Measurements were made at four microsites with different vegetation communities every 3 to 4 weeks during the period 2008?2009, 2 years with contrasting WTD patterns. Models were used to examine the relative response of each microsite to variations in peat temperature and WTD and used to estimate annual total Reco. Results Temporal variations inReco were strongly related to peat temperature at the 5 cm depth. However, two of the microsites did not show any significant change in this relationship while two others showed contrasting responses including an increase and decrease in
Název v anglickém jazyce
Ecosystem respiration in a heterogeneous temperate peatland and its sensitivity to peat temperature and water table depth
Popis výsledku anglicky
Background and aims Ecosystem respiration (R eco ) is controlled by thermal and hydrologic regimes, but their relative importance in defining the CO2 emissions in peatlands seems to be site specific. The aim of the paper is to investigate the sensitivityof R eco to variations in temperature and water table depth (WTD) in a wet, geogenous temperate peatland. Methods The CO2 fluxes were measured using chambers. Measurements were made at four microsites with different vegetation communities every 3 to 4 weeks during the period 2008?2009, 2 years with contrasting WTD patterns. Models were used to examine the relative response of each microsite to variations in peat temperature and WTD and used to estimate annual total Reco. Results Temporal variations inReco were strongly related to peat temperature at the 5 cm depth. However, two of the microsites did not show any significant change in this relationship while two others showed contrasting responses including an increase and decrease in
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
EH - Ekologie – společenstva
OECD FORD obor
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Návaznosti výsledku
Projekt
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Návaznosti
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2013
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Plant and Soil
ISSN
0032-079X
e-ISSN
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Svazek periodika
366
Číslo periodika v rámci svazku
1-2
Stát vydavatele periodika
NL - Nizozemsko
Počet stran výsledku
16
Strana od-do
505-520
Kód UT WoS článku
000317988600037
EID výsledku v databázi Scopus
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