The response of a mid- and high latitude peat bog to predicted climate change: methane production in a 12-month peat incubation

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F14%3A10282467" target="_blank" >RIV/00216208:11310/14:10282467 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/00025798:_____/14:00000020 RIV/00025798:_____/14:00000007 RIV/60460709:41210/14:60414 RIV/86652079:_____/14:00521334

Výsledek na webu

<a href="http://dx.doi.org/10.1007/s11027-013-9456-0" target="_blank" >http://dx.doi.org/10.1007/s11027-013-9456-0</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1007/s11027-013-9456-0" target="_blank" >10.1007/s11027-013-9456-0</a>

Jazyk výsledku

angličtina

Název v původním jazyce

The response of a mid- and high latitude peat bog to predicted climate change: methane production in a 12-month peat incubation

Popis výsledku v původním jazyce

There are fears that global warming will lead to degradation of peatlands, higher emissions of greenhouse gases from peat, and accelerated warming. Anaerobic decomposition of organic soils produces methane (CH4), a potent greenhouse gas. Two peat bogs differing in mean annual temperature, Velke Darko (VD, Czech Republic, 7.2 A degrees C), and Stor myran (SA, Sweden, 4.0 A degrees C), were selected for a comparative study of how organic soils in different climatic zones will respond to warmer and drier conditions. Twenty peat cores from each bog were incubated in growth chambers. Under present-day summer conditions, VD produced 14 times more CH4 than SA. Two different warming scenarios were used. Peat-core replicates were kept at temperatures of 11 versus 16 A degrees C, and 11 versus 22 A degrees C. From 11 to 16 A degrees C, the CH4 production slightly decreased at SA, and slightly increased at VD. From 11 to 22 A degrees C, the CH4 production increased 9 times at SA, but slightly dec

Název v anglickém jazyce

The response of a mid- and high latitude peat bog to predicted climate change: methane production in a 12-month peat incubation

Popis výsledku anglicky

There are fears that global warming will lead to degradation of peatlands, higher emissions of greenhouse gases from peat, and accelerated warming. Anaerobic decomposition of organic soils produces methane (CH4), a potent greenhouse gas. Two peat bogs differing in mean annual temperature, Velke Darko (VD, Czech Republic, 7.2 A degrees C), and Stor myran (SA, Sweden, 4.0 A degrees C), were selected for a comparative study of how organic soils in different climatic zones will respond to warmer and drier conditions. Twenty peat cores from each bog were incubated in growth chambers. Under present-day summer conditions, VD produced 14 times more CH4 than SA. Two different warming scenarios were used. Peat-core replicates were kept at temperatures of 11 versus 16 A degrees C, and 11 versus 22 A degrees C. From 11 to 16 A degrees C, the CH4 production slightly decreased at SA, and slightly increased at VD. From 11 to 22 A degrees C, the CH4 production increased 9 times at SA, but slightly dec

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

EH - Ekologie – společenstva

OECD FORD obor

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Projekt

<a href="/cs/project/ED1.1.00%2F02.0073" target="_blank" >ED1.1.00/02.0073: CzechGlobe ? Centrum pro studium dopadu globální zmeny klimatu</a><br>

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2014

Kód důvěrnosti údajů

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

Název periodika

Mitigation and Adaptation Strategies for Global Change

ISSN

1381-2386

e-ISSN

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Svazek periodika

19

Číslo periodika v rámci svazku

7

Stát vydavatele periodika

NL - Nizozemsko

Počet stran výsledku

14

Strana od-do

997-1010

Kód UT WoS článku

000342180000005

EID výsledku v databázi Scopus

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