Greenhouse gas emissions from two rewetted peatlands previously managed for forestry

C. Rigney, D. Wilson, F. Renou-Wilson, C. Müller, G. Moser, Ken A. Byrne

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Abstract

The aim of this study was to investigate the controls on carbon dioxide (CO 2 ), methane (CH 4 ) and nitrous oxide (N 2 O) dynamics on a blanket bog (at Pollagoona) and a raised bog (at Scohaboy) in Ireland after felling of plantation forestry and rewetting, and to produce annual balances for each gas at both sites. Gas fluxes were measured during a twelve-month period using the chamber method. Microsite types reflecting the dominant plant species at the chamber plots were identified and classified as Eriophorum-Sphagnum, Cladonia-Calluna and Molinia at Pollagoona and Eriophorum-Sphagnum, Cladonia-mosses, Eriophorum and brash (logging residues) at Scohaboy. The relationships between gas fluxes and environmental variables were assessed, and regression models were used to estimate annual CO 2 and CH 4 gas balances for each microsite type. Annual estimates of N 2 O exchange were calculated using seasonal means. Over the course of the study both sites acted as CO 2 and CH 4 sources. Although Pollagoona was an overall net source of CO 2 -C (131.6 ± 298.3 g m -2 yr -1 ), one microsite type (Cladonia-Calluna) acted as a strong sink for CO 2 -C (-142.8 g m -2 yr -1 ). Molinia microsites exhibited the highest CH 4 -C emissions (2.53 ± 1.01 g m -2 yr -1 ). Nitrous oxide emissions at Pollagoona were calculated as 12 μg m -2 yr -1 . Scohaboy acted as a large CO 2 -C source (585.3 ± 241.5 g m -2 yr -1 ) (all microsite types) despite re-vegetation of non-brash plots, due to the availability of fresh organic matter across the site. Scohaboy was also a CH 4 -C source, emitting 3.25 ± 0.58 g m -2 yr -1 . Emissions of both CO 2 -C (819.31 ± 57.7 g m -2 yr -1 ) and CH 4 -C (4.76 ± 0.98 g m -2 yr -1 ) were highest from the brash plots. Annual N 2 O-N emissions were small over the study period (72 µg m -2 yr -1 ). Our results indicate that, despite remedial work being conducted on both peatlands to raise the water table, the C sink function has not yet been restored at either site.

Original languageEnglish
Article number24
JournalMires and Peat
Volume21
DOIs
Publication statusPublished - 2018

Keywords

  • Blanket bog
  • Carbon dioxide
  • Methane
  • Nitrous oxide
  • Raised bog
  • Rewetting

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