Development of floating rafts after the rewetting of cut-over bogs: the importance of peat quality
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SourceBiogeochemistry, 71, 1, (2004), pp. 69-87
Article / Letter to editor
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Aquatic Ecology and Environmental Biology
The usual method of restoring cut-over bogs is to rewet the peat surface. but this often leads to the remaining peat layers being deeply inundated. For Sphagnum-dominated vegetation to develop at deeply inundated locations. it is important for floating rafts of buoyant residual peat to develop. In this study. the chemical and physical characteristics of buoyant and inundated peat collected from rewetted cut-over bog were compared. In general. buoyant peat was poorly humified: high methane (CH4) production rates (greater than or equal to2 mumol g(-1) DW day(-1)) were important to ensure buoyancy. Although the peat water CH4 concentrations increased with depth. the CH4 production rates were higher in the uppermost peat layers. High CH4 production rates were related positively with P concentrations and negatively with lignin concentrations. The pH to bulk density ratio (greater than or equal to0.05) also appeared to be a good indicator of CH4 production rates, providing an easy and cheap way to measure. the variable for restoration practitioners. Our results indicated that analysing certain simple characteristics of the residual peat can greatly improve the success of the rewetting measures taken in cut-over bogs. If the analysis reveals that the residual peat is unsuitable for floating raft formation, deep inundation is inappropriate unless suitable peat from other locations can be introduced.
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