Restoration of a Degraded Raised Bog: Implications for Carbon Flux and Hydrological Recovery

Peatlands are globally important carbon stores that provide a range of ecological, climatic, and socio-economic benefits. However, large-scale peat extraction, drainage for agriculture, and conversion to forestry have changed many peatlands from long-term carbon sinks into carbon sources. While some of the best remaining examples of intact raised bogs in Western Europe occur on the island of Ireland, a large majority are degraded. In recent years, Ireland has undertaken an extensive programme of peatland restoration, with works carried out across approximately 30,000 ha of drained raised bog to enhance biodiversity and contribute towards international greenhouse gas reduction commitments. Understanding the impacts of such restoration efforts on peatland hydrology, carbon dynamics, and biodiversity is essential to ensure that measures are effective and achieving the outcomes required. This study presents data from the restoration of a drained area of All Saints Bog, a Natura 2000 raised bog site. Restoration measures included ditch blocking, re-profiling degraded areas, and contour bund construction with adjustable drains to regulate the hydrology. The effects of restoration are evaluated using a combination of eddy covariance, chamber measurements, water level monitoring, and remote sensing over a four-year period from 2021 to 2024. This period incorporated one year of pre-restoration, two years of active restoration, and one year of post-restoration. Hydrologically, restoration efforts appear to have been successful, with widespread rewetting across much of the site, recreating the conditions for active peat formation and the slow recovery of Sphagnum moss locally present. However, we found an approximate two-fold increase in net carbon fluxes between pre- and post-restoration, rising from 1.14 t CO₂-C ha⁻¹ y⁻¹ in 2021 to 2.37 t CO₂-C ha⁻¹ y⁻¹ in 2024. Furthermore, chamber-based spatial measurements showed a higher emission contribution from contour bunds compared to bare peat. Consequently, a programme of Sphagnum translocation and inoculation is planned for 2025 to hasten vegetation recovery. This long-term investigation will deepen our understanding of effective restoration efforts, which will provide insights to guide the development of future restoration strategies.

Authors

Institutions

Publication Details

Journal
ARPHA Conference Abstracts
Published
2025-05-28
DOI
https://doi.org/10.3897/aca.8.e148818
Primary Topic
Peatlands and Wetlands Ecology
Type
article
Field-Weighted Citation Impact
0.00
Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

Restoration of a Degraded Raised Bog: Implications for Carbon Flux and Hydrological Recovery

Mika Korkiakoski, Ultan McCarthy, Owen Naughton, Mark O’Connor et al.
ARPHA Conference Abstracts
Peatlands and Wetlands Ecology
article

Restoration of a Degraded Raised Bog: Implications for Carbon Flux and Hydrological Recovery

Mika Korkiakoski, Ultan McCarthy, Owen Naughton, Mark O’Connor, Shane Regan, Md Shamsuzzaman, Imelda Casey
article en

Abstract

Peatlands are globally important carbon stores that provide a range of ecological, climatic, and socio-economic benefits. However, large-scale peat extraction, drainage for agriculture, and conversion to forestry have changed many peatlands from long-term carbon sinks into carbon sources. While some of the best remaining examples of intact raised bogs in Western Europe occur on the island of Ireland, a large majority are degraded. In recent years, Ireland has undertaken an extensive programme of peatland restoration, with works carried out across approximately 30,000 ha of drained raised bog to enhance biodiversity and contribute towards international greenhouse gas reduction commitments. Understanding the impacts of such restoration efforts on peatland hydrology, carbon dynamics, and biodiversity is essential to ensure that measures are effective and achieving the outcomes required. This study presents data from the restoration of a drained area of All Saints Bog, a Natura 2000 raised bog site. Restoration measures included ditch blocking, re-profiling degraded areas, and contour bund construction with adjustable drains to regulate the hydrology. The effects of restoration are evaluated using a combination of eddy covariance, chamber measurements, water level monitoring, and remote sensing over a four-year period from 2021 to 2024. This period incorporated one year of pre-restoration, two years of active restoration, and one year of post-restoration. Hydrologically, restoration efforts appear to have been successful, with widespread rewetting across much of the site, recreating the conditions for active peat formation and the slow recovery of Sphagnum moss locally present. However, we found an approximate two-fold increase in net carbon fluxes between pre- and post-restoration, rising from 1.14 t CO₂-C ha⁻¹ y⁻¹ in 2021 to 2.37 t CO₂-C ha⁻¹ y⁻¹ in 2024. Furthermore, chamber-based spatial measurements showed a higher emission contribution from contour bunds compared to bare peat. Consequently, a programme of Sphagnum translocation and inoculation is planned for 2025 to hasten vegetation recovery. This long-term investigation will deepen our understanding of effective restoration efforts, which will provide insights to guide the development of future restoration strategies.

ARPHA Conference AbstractsVol. 8
Finnish Meteorological Institute (FI), South East Technological University (IE), Institute of Technology Carlow (IE), Waterford Institute of Technology (IE)
Openalex Percentile: Top 76%
Peatlands and Wetlands Ecology
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.