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Rewetting of Cutaway Peatlands: Are We Re‐Creating Hot Spots of Methane Emissions?
Author(s) -
Wilson David,
Alm Jukka,
Laine Jukka,
Byrne Kenneth A.,
Farrell Edward P.,
Tuittila EevaStiina
Publication year - 2009
Publication title -
restoration ecology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.214
H-Index - 100
eISSN - 1526-100X
pISSN - 1061-2971
DOI - 10.1111/j.1526-100x.2008.00416.x
Subject(s) - peat , microsite , environmental science , wetland , mire , global warming potential , methane , ecosystem , water table , hydrology (agriculture) , atmospheric sciences , greenhouse gas , physical geography , chemistry , ecology , geology , geography , agronomy , geotechnical engineering , biology , groundwater , organic chemistry , seedling
Hot spots of CH 4 emissions are a typical feature of pristine peatlands at the microsite and landscape scale. To determine whether rewetting and lake construction in a cutaway peatland would result in the re‐creation of hot spots, we first measured CH 4 fluxes over a 2‐year period with static chambers and estimated annual emissions. Second, to assess whether rewetting and lake creation would produce hot spots at the landscape level, we hypothesized a number of alternative land use scenarios for the peatland following the cessation of peat extraction. Using the results from this study and other studies from literature, we calculated the global warming potential (GWP) of each scenario and the respective contribution of CH 4 . The results showed that hot spots of CH 4 fluxes were observed as a consequence of microsite‐specific differences in water table (WT) position and plant productivity. CH 4 fluxes were closely related to peat temperature at 10 cm depth and WT position. Annual emissions ranged from 4.3 to 38.8 g CH 4 m −2 yr −1 in 2002 and 3.2 to 28.8 g CH 4 m −2 yr −1 in 2003. The scenario results suggest that lake creation is likely to result in the re‐creation of a hot spot at the landscape level. However, the transition from cutaway to wetland ecosystem may lead to a reduction in the GWP of the peatland.