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• W2098982587 abstract "Pristine peatlands store approximately one-third of the world's soil carbon through the long-term accumulation of carbon as peat (Gorham, 1991). In Canada and Europe, peatlands are exploited for peat fuel and horticultural peat, which has an impact on the hydrological conditions and carbon balance of these ecosystems. Recent advances in peatland restoration techniques (e.g., Rochefort, 2000) have succeeded in the revegetation of Sphagnum moss on previously cutover surfaces. However, a peatland can only be considered functionally 'restored' after the newly formed moss layer has achieved a thickness such that the water table position in a drought year does not extend into the underlying formerly cutover peat surface (i.e. an acrotelm is developed). This study determines ecohydrological and hydrophysical properties of a newly formed peat layer, compares them to those of a nearby natural site and a naturally revegetated site and examines the spatio-temporal development of a new peat layer at a restored peatland, and from this, estimates of when the newly developing moss layer in a restored peatland will become a functional acrotelm are made. The properties of the new peat layer differed significantly between the sites, especially for the lower (8-12 cm) layer. Lower samples for the natural and naturally revegetated sites had a bulk density of 43 ± 5 kg mand 41 ± 11 kg mrespectively, almost twice as high as the value for lower samples from the restored site (24 ± 4 kg m-). Sphagnum rubellum capitula density (pc) was significantly higher (p < 0.05) for the restored peatland (28726 # m-) compared to the natural site (26050 # m-). Residual moisture content at 200 mb (-" @default.
• W2098982587 created "2016-06-24" @default.
• W2098982587 creator A5010495982 @default.
• W2098982587 date "2009-02-01" @default.
• W2098982587 modified "2023-09-27" @default.
• W2098982587 title "Peatland Restoration: An Ecohydrological Assessment" @default.
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• W2098982587 hasPublicationYear "2009" @default.
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