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- W2330960533 abstract "Surface peat becomes compacted by the combined effects of biological decomposition processes (mechanical breakdown and decay) and of the physical squeezing of peat into a smaller, more consolidated volume. We use corresponding determinations of age and depth of 1041 surface peat cores from 14 Scandinavian boreal mires to demonstrate that, at least for the first 40 years after the peat is deposited, the compaction process can be adequately described by assuming a constant compaction rate. This result is used to calculate vertical surface peat growth rates that are corrected for compaction. Estimated compaction rates did not differ significantly between lawn and hummock habitats while significant differences that were not related to latitude were found among mires. We interpret this as an indication that compaction rates depend on hydrology at the scale of mires. Vertical peat growth rates differed strongly among mires and between habitats within mires, indicating considerable variation at several spatial scales." @default.
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- W2330960533 date "1998-05-01" @default.
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- W2330960533 title "Age-Depth Relationships in Scandinavian Surface Peat: A Quantitative Analysis" @default.
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- W2330960533 doi "https://doi.org/10.2307/3546914" @default.
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