Spatiotemporal variability in peatland subsurface methane dynamics

• Published in: Journal of Geophysical Research - Biogeosciences Vol. 113; no. G2; pp. G02010 - n/a
• Main Authors: Strack, M., Waddington, J. M.
• Format: Journal Article
• Language: English
• Published: Washington, DC American Geophysical Union 01-06-2008; Blackwell Publishing Ltd
• Subjects: Biogeochemical cycles, processes, and modeling; biogeochemistry; Biogeosciences; bubbles; carbon; dissolved methane; Earth sciences; Earth, ocean, space; Eco-hydrology; entrapped gas; Exact sciences and technology; Freshwater; Hydrology; mean residence time; Soils; Wetlands; Canada; Quebec; Eastern Canada; Canada, Quebec; entrapped gas; bubbles; dissolved methane; mean residence time; biogeochemistry; carbon; atmosphere; sampling; water table; concentration; subsurface; variability; North America; stocks; greenhouse gas; dynamics; depth; Depth profile; pore water; methane; pH; temperature; residence time; peat
• ISSN: 0148-0227; 2156-2202
• DOI: 10.1029/2007JG000472

Peatlands are large natural sources of atmospheric methane (CH4). While many studies have measured CH4 emissions to the atmosphere, less is known about the stock and residence time of subsurface CH4. In this study we examined dissolved CH4 concentration in near‐surface peatland pore waters of a poor fen near Québec City, Canada, in order to (1) investigate the variability in and potential controls on these concentrations and (2) combine measured dissolved CH4 concentration with estimated bubble CH4 stock and measured CH4 fluxes to estimate the mean residence time of subsurface CH4. Concentrations ranged from 1 to 450 μM during both study seasons. Depth profiles were generally consistent at one location within the peatland throughout the sampling period but varied between locations. Patterns with depth were not well correlated to pore water pH or EC; however, changes in CH4 concentration through time in the upper 30 cm were related to temperature and water table at some locations. Depth profiles taken at 2‐ to 5‐cm intervals revealed discrete concentration “spikes” which were often maintained throughout the season and are likely related to bubble CH4 dynamics. Estimated subsurface CH4 stocks indicate that even when relatively low bubble volume (5% of peat volume) is assumed, bubble CH4 accounted for greater than half of total stocks. Calculated mean residence times were 28–120 days. This implies that CH4 flux may lag changes in water table and temperature which happen on shorter timescales (hours or days). To improve our description of subsurface CH4 stocks, links between dissolved and bubble CH4 stocks and peatland CH4 residence time, coincident measurement of pore water CH4 concentrations, entrapped gas content and composition, diffusive CH4 flux, and ebullition are required.