PulseExploreJournal ClubDebatesTrendingResearchersJournals
Instagram
HomeExploreJournal ClubTrending
Synapse
⌘+K
Synapse
April 29, 2026Soil Use and Management0 citationsOpen Access

Short Term Effects of Soil Disturbance on Greenhouse Gas Fluxes on a Nutrient‐Rich Peatland After Clearcutting

View Full Paper
JSJuuli SuominenQLQian LiALAleksi Lehtonen

Key Points

  • The study aims to evaluate how soil disturbances from forestry practices influence greenhouse gas emissions in peatlands.
  • Examined soil greenhouse gas fluxes from disturbed (mounded) and unprepared soil surfaces over three growing seasons.
  • Measured carbon dioxide, methane, and nitrous oxide emissions, alongside water table level and soil temperature.
  • Conducted the study in a drained peatland forest in southern Finland.
  • Mounding significantly increased methane (CH4) and nitrous oxide (N2O) fluxes compared to unprepared surfaces.
  • Carbon dioxide (CO2) fluxes were not affected by mounding treatment.
  • Soil temperature was the major driver for CO2 fluxes, while environmental factors did not significantly relate to CH4 and N2O emissions.

Abstract

ABSTRACT Forestry drained peatlands are currently a large source of greenhouse gas (GHG) emissions and expected to lose carbon (C) storage in long‐term. The GHG emissions and soil C stock are affected by management practices. In rotation forestry, soils are prepared with machine for regeneration after clearcutting. However, little is known about how the soil disturbances affect GHG emissions from soil. This study examines the effects of mounding on the soil GHG fluxes in a nutrient‐rich drained peatland forest in southern Finland. Carbon dioxide (CO 2 ), methane (CH 4 ) and nitrous oxide (N 2 O) fluxes were measured on disturbed (mounded) soil surfaces and unprepared soil surfaces over three growing seasons after soil preparation. In addition, water table (WT) level and soil temperature were measured to investigate the drivers of the gas fluxes. CO 2 fluxes were not impacted by mounding treatment, while CH 4 and N 2 O fluxes were significantly higher on the mounds compared to the unprepared surfaces. Soil temperature was the major parameter controlling CO 2 fluxes. No significant relationships were found between CH 4 and N 2 O fluxes and the measured environmental factors. This study provided evidence that on peatland soils, disturbance increases CH 4 and N 2 O emissions to the atmosphere and has climate warming effects, highlighting the importance of monitoring all GHG fluxes from varied surfaces after clearcutting and soil preparation to better estimate the climate impacts of rotation forestry on peatlands.

Ask AI
Helpful
Bookmark
Share
View Full Paper

Cite This Study

Suominen et al. (2026) studied this question.

synapsesocial.com/papers/69f19f9cedf4b46824806596https://doi.org/10.1111/sum.70218
Ask AI
Helpful
Bookmark
Share
View Full Paper

Also Consider

Synapse has enriched 5 closely related papers on similar clinical questions. Consider them for comparative context:

  1. 1Effect of a lowered water table on nitrous oxide fluxes from northern peatlands1993 · 381 citations
  2. 2Effect ofCarex rostrataon seasonal and interannual variability in peatland methane emissions2013 · 79 citations
  3. 3Nine-years effect of harvesting and mechanical site preparation on bryophyte decomposition and carbon stocks in a boreal forested peatland2023 · 7 citations
  4. 4Impact of site-preparation on soil-surface CO2 fluxes and litter decomposition in a clear-cut in Sweden2015 · 25 citations
  5. 5Effects of stump harvest and site preparation on N2O and CH4 emissions from boreal forest soils after clear-cutting2016 · 31 citations