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HERO ID
1570326
Reference Type
Journal Article
Title
Methane (CH4) emission from a tidal marsh in the Min River estuary, southeast China
Author(s)
Tong, C; Wang, WeiQi; Zeng, CS; Marrs, Rob
Year
2010
Is Peer Reviewed?
1
Journal
Journal of Environmental Science and Health, Part A: Toxic/Hazardous Substances & Environmental Engineering
ISSN:
1093-4529
EISSN:
1532-4117
Volume
45
Issue
4
Page Numbers
506-516
PMID
20390897
DOI
10.1080/10934520903542261
Web of Science Id
WOS:000275851900014
Abstract
The total methane emission to the atmosphere and
hydrosphere, and its seasonal variation, were estimated using an enclosed static chamber
technique from a tidal marshes dominated by Phragmites australis (common reed) in the Min River
estuary, southeast China. Measurements were taken at three tidal stages ( before flood, during
the flooding and ebbing process, and after ebb). Potential rates of methane production from the
marsh sediment layers were also measured using an incubation technique. This P. australis tidal
marsh was a net methane source, emitting 32.59 and 6.87 g CH4.m(-2).yr(-1) to the atmosphere and
hydrosphere, respectively. There was considerable monthly variation with emissions greater before
flood in some months, whereas at other months emission was greater after ebb. The average methane
fluxes were 5.13, 5.06 and 4.74 mg CH4 m(-2) h(-1) before flood, during flooding and ebbing, and
after ebb, respectively. Emissions to the tidewater and the atmosphere during the flooding and
ebbing process were 2.98 and 2.08 mg CH4 m(-2) h(-1), respectively. Sediment methane production
potential (0-40 cm depth) ranged from 0.028-0.123 mu g CH4.g(-1).d(-1), with the greatest
production was in the surface soil. Methane fluxes had a significant correlation with
atmospheric, sediment temperature and above ground biomass. The implications of these data for
global warming are discussed briefly.
Keywords
CH4 flux; tidal marsh; tidal stages; seasonal variation; environmental conditions
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