Hydrology-driven ecosystem respiration determines the carbon balance of a boreal peatland.
Hydrology-driven ecosystem respiration determines the carbon balance of a boreal peatland.
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水文驱动的生态系统呼吸决定了北方泥炭地的碳平衡
DOI:
10.1016/j.scitotenv.2013.06.077
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发表时间:
2013
期刊:
影响因子:
--
通讯作者:
M. Wilmking
中科院分区:
文献类型:
--
作者:
Gazovic;Forbrich;Kutzbach;M. Wilmking
The carbon (C) balance of boreal peatlands is mainly the sum of three different C fluxes: carbon dioxide (CO2), methane (CH4) and dissolved organic carbon (DOC). Intra- and inter-annual dynamics of these fluxes are differentially controlled by similar factors, such as temperature and water-table. Different climatic conditions within and between years might thus result in varying absolute and relative contributions of each flux to net ecosystem productivity (NEP). In this study CO2fluxes were measured at a boreal peatland in eastern Finland during a dry year (2006) and a wet year (2007) and combined with DOC and CH4fluxes from the same site. CO2uptake in the wet year was 65% higher than in the dry year, caused by higher water table (WT) and subsequently reduced rates of soil respiration. Two to three-fold increases in DOC and CH4fluxes in the wet year did not completely offset the higher CO2uptake in that year, resulting in NEP of − 83.7 ± 14 g C m− 2in the dry and − 134.5 ± 21 g C m− 2in the wet year. Thus, in our study, WT was identified as the most important factor responsible for variations in the C balance between the observed years.
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影响因子:
4.9
作者:
E. Golovatskaya;E. Dyukarev
通讯作者:
E. Golovatskaya;E. Dyukarev
影响因子:
4.9
作者:
Becker;Kutzbach;Forbrich;Schneider;M. Wilmking
通讯作者:
M. Wilmking
影响因子:
6.2
作者:
Forbrich, Inke;Kutzbach, Lars;Wilmking, Martin
通讯作者:
Wilmking, Martin
影响因子:
64.8
作者:
Freeman, C;Fenner, N;Hudson, J
通讯作者:
Hudson, J