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Relationship between methane flux and peatland water-table and the feedback to global climate change

Conference · · Bulletin of the Ecological Society of America; (United States)
OSTI ID:5985439
 [1]
  1. Univ. of Minnesota, Minneapolis (United States)
This field study examined the relationship between methane flux and peatland water-table height while limiting variation of other factors. My goal was to quantify the feedback that water-table drawdown, as-predicted by global climate change, will have on methane emission. Closed-chamber ground measurements were used from June through October to quantify methane emission from one drained and one undrained forested sphagnum bog in Minnesota. Water-table height in the drained bog varied, along a water-table gradient, from [minus]60 cm to [minus]5 cm (1991) and [minus]45 cm to +14 cm (1992). Water-table height in the undrained peatland ranged, on hummocks, hollows, and flooded bog corrals, from [minus]29 cm to +10 cm (1992). Mean methane emission in the drained bog was 11.2 mg CH[sub 4] m[sup [minus]2] day[sup [minus]1] (1991) and 14.3 mg CH[sub 4]m[sup [minus]2] day[sup [minus]1] (1992). Mean methane emission in the undrained bog was 99.1 mg CH[sub 4] m[sup [minus]2] day[sup [minus]1] (1992). A significant positive relationship was found between 1n (methane flux) and pleated water-table. This relationship implies a negative feedback to global warming. The results of this study suggest that the first stages in water-table drawdown will be the most significant in reducing methane emission from peatlands.
OSTI ID:
5985439
Report Number(s):
CONF-930798--
Conference Information:
Journal Name: Bulletin of the Ecological Society of America; (United States) Journal Volume: 74:2
Country of Publication:
United States
Language:
English

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