Methane emissions from a gully mire in mid-Wales, U.K. under consecutive summer water table drawdown
- Univ. of Wales, Bangor (United Kingdom)
- Inst. of Hydrology, Llanbrynmair (United Kingdom)
Wetlands are a major contributor to the global methane (CH{sub 4}) budget. Currently there is a consensus view that drought restrains CH{sub 4} emissions from wetlands. However, a 6-year field experiment investigating the effects of persistent summer water table drawdown on a gully mire in mid-Wales, U.K. demonstrated a 2-year boom and bust cycle of CH{sub 4} emissions followed by a recovery during the third year, when compared with emissions from a control wetland in which the water table remained at or above the peat surface. This cyclical trend was subsequently replicated by the control wetland following natural summer drought. The experimental wetland was affected less by this natural drought following previous water table drawdown. Depth profiles of CH{sub 4} production suggested that consecutive water table drawdown resulted in a translocation of peak methanogen activity lower down the peat profile, where emissions were affected less by subsequent drawdown. These findings suggest that wetland CH{sub 4} flux models need to consider the possibility that methane emission-water table relationships are dependent on the pattern and frequency of drought events.
- OSTI ID:
- 318770
- Journal Information:
- Environmental Science and Technology, Vol. 33, Issue 2; Other Information: PBD: 15 Jan 1999
- Country of Publication:
- United States
- Language:
- English
Similar Records
Hydraulic reversals and episodic methane emissions during drought cycles in mires
Carbon Accumulation, Flux, and Fate in Stordalen Mire, a Permafrost Peatland in Transition