Methane and carbon dioxide release from wetland ecosystems

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F86652079%3A_____%2F20%3A00524602" target="_blank" >RIV/86652079:_____/20:00524602 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/86652079:_____/20:00545308

Výsledek na webu

<a href="http://dx.doi.org/10.1016/B978-0-12-818032-7.00019-9" target="_blank" >http://dx.doi.org/10.1016/B978-0-12-818032-7.00019-9</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/B978-0-12-818032-7.00019-9" target="_blank" >10.1016/B978-0-12-818032-7.00019-9</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Methane and carbon dioxide release from wetland ecosystems

Popis výsledku v původním jazyce

Wetlands can be defined as transitional ecotone ecosystems between terrestrial and aquatic conditions and are characterized by the waterlogged soils. Prevailing anaerobic conditions in wetland soils slow down or suspend decomposition processes of organic matter. These processes are connected with the production of soil biogenic methane (CH4) and carbon dioxide (CO2). CH4 is a product of organic decomposition under anaerobic conditions, while CO2 is a product of organic matter decomposition under aerobic conditions. Anaerobic conditions stabilized in profiles of wetland soils determine a crucial role of wetlands in the carbon cycle at both the local and the global scale. Wetlands sequestrate well carbon into the soil for a long period, and their soils contain about one-third of the global soil carbon stock. It is a bit of a paradox that ecosystems, which are responsible for creating huge carbon storage, are now under scrutiny in case of CH4 emissions into the atmosphere.

Název v anglickém jazyce

Methane and carbon dioxide release from wetland ecosystems

Popis výsledku anglicky

Wetlands can be defined as transitional ecotone ecosystems between terrestrial and aquatic conditions and are characterized by the waterlogged soils. Prevailing anaerobic conditions in wetland soils slow down or suspend decomposition processes of organic matter. These processes are connected with the production of soil biogenic methane (CH4) and carbon dioxide (CO2). CH4 is a product of organic decomposition under anaerobic conditions, while CO2 is a product of organic matter decomposition under aerobic conditions. Anaerobic conditions stabilized in profiles of wetland soils determine a crucial role of wetlands in the carbon cycle at both the local and the global scale. Wetlands sequestrate well carbon into the soil for a long period, and their soils contain about one-third of the global soil carbon stock. It is a bit of a paradox that ecosystems, which are responsible for creating huge carbon storage, are now under scrutiny in case of CH4 emissions into the atmosphere.

Druh

C - Kapitola v odborné knize

CEP obor

—

OECD FORD obor

10510 - Climatic research

Projekt

—

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2020

Kód důvěrnosti údajů

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

Název knihy nebo sborníku

Climate change and soil interactions

ISBN

978-0-12-818032-7

Počet stran výsledku

44

Strana od-do

509-553

Počet stran knihy

806

Název nakladatele

Elsevier

Místo vydání

Amsterdam

Kód UT WoS kapitoly

000562856000020