Affiliations 

  • 1 Sarawak Tropical Peat Research Institute, Kota Samarahan, Malaysia. Electronic address: wong.gx@sarawak.gov.my
  • 2 Center for Global Environmental Research, National Institute for Environmental Studies, Tsukuba, Japan
  • 3 Research Faculty of Agriculture, Hokkaido University, Sapporo, Japan
  • 4 Sarawak Tropical Peat Research Institute, Kota Samarahan, Malaysia
  • 5 Department of Geography, University of Tartu, Estonia
Sci Total Environ, 2025 Jan 25;962:178466.
PMID: 39813841 DOI: 10.1016/j.scitotenv.2025.178466

Abstract

Tropical peatlands are significant sources of methane (CH₄), but their contribution to the global CH₄ budget remains poorly quantified due to the lack of long-term, continuous and high-frequency flux measurements. To address this gap, we measured net ecosystem CH4 exchange (NEE-CH4) using eddy covariance technique throughout the conversion of a tropical peat swamp forest to an oil palm plantation. This encompassed the periods before, during and after conversion periods from 2014 to 2020, during which substantial environmental shifts were observed. Draining the peatland substantially lowered mean monthly groundwater levels from -20.0 ± 14.2 cm before conversion to -102.3 ± 31.6 cm during conversion and increased slightly to -96.5 ± 19.3 cm after conversion. Forest removal increased mean monthly soil temperature by 2.3 to 3.1 °C, reducing net radiation (Rn) and raising vapor pressure deficit (VPD). Following the tree removal, controlled burning temporarily warmed air temperature by 8 °C, increased VPD and significantly attenuated Rn, resulting in negative values owing to radiation interception by smoke and increased surface warming. Contrary to expectations that drainage would lower CH4 emissions, the site remained a consistent net source, with even higher emissions observed during and after conversion. The mean monthly NEE-CH4 during conversion (23.3 ± 8.6 mg C m-2 d-1) was about 2-times higher than before conversion (12.1 ± 5.3 mg C m-2 d-1) and about 1.5-times higher than after conversion (16.3 ± 4.1 mg C m-2 d-1). The heightened CH4 release is likely attributable to emissions from drainage ditches, underscoring their significant role in post-conversion CH4 dynamics. Despite its short duration, controlled burning substantially elevated NEE-CH4, ranging from 0.04 to 0.91 mg C m-2 s-1. Our findings highlight the substantial impact of land conversion on peatland CH4 dynamics, emphasizing the need for accurate flux measurements across various conversion stages to refine global CH4 budgets.

* Title and MeSH Headings from MEDLINE®/PubMed®, a database of the U.S. National Library of Medicine.