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Spatial variability of soil greenhouse gas emissions in oil palm plantation under different management zones


Citation

Chang, Yu Yang and Sakrabani, Ruben and Golicz, Karolina Krystyna and Kim, Sang Yoon and Tan, Ngai Paing and Sim, Choon Cheak (2026) Spatial variability of soil greenhouse gas emissions in oil palm plantation under different management zones. Environmental Research Communications, 8 (4). art. no. 045025. pp. 1-13. ISSN 2515-7620

Abstract

As global demand for palm oil continues to rise, improving the accuracy of greenhouse gas (GHG) accounting in oil palm plantations is essential for evaluating their environmental sustainability. Spatial heterogeneity created by routine plantation management can strongly influence soil properties and GHG emissions. In this study, we assessed soil CO2, N2O, and CH4 emissions across three principal management zones in a mature oil palm (nine-year-old) plantation cultivated in mineral soils- frond heap (FH), palm circle (PC), and harvesting path (HP) under standard operational practices. Soil GHG fluxes were measured using static chambers coupled with a Fourier-transform infrared (FTIR) gas analyser, alongside surface soil (0–5 cm) sampling to characterise soil organic carbon, total nitrogen, moisture content, bulk density, porosity, and pH. In total, 90 measurement points were evaluated to capture within-plantation spatial variability. The FH zone exhibited significantly higher soil organic carbon, total nitrogen, porosity, and moisture content, and lower bulk density than the PC and HP zones. These properties translated into significant higher mean GHG fluxes in FH soils, with CO2, N2O, and CH4 emissions of 165.7 mg m−2 h−1, 0.25 mg mg m−2 h−1, and 0.25 mg m−2 h−1, respectively. In contrast, HP soils were more compacted, carbon-poor, and exhibited the lowest GHG emissions. Spearman’s rank correlation analyses indicated that CO2 emissions were primarily driven by increased soil porosity, while elevated soil moisture and organic matter inputs in FH zones promoted conditions conducive to N2O production and anaerobic microsite formation supporting CH4 emissions. When expressed as CO2-equivalents, the FH zone acted as biogeochemical hotspot, contributed disproportionately to plantation-scale GHG emissions despite occupying only one-third of the total area. These findings highlight the importance of incorporating fine-scale spatial variability when developing GHG inventories, emission factor development, and targeted, zone-specific mitigation strategies.


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Additional Metadata

Item Type: Article
Subject: Food Science
Subject: Environmental Science (all)
Subject: Agricultural and Biological Sciences (miscellaneous)
Divisions: Faculty of Agriculture
DOI Number: https://doi.org/10.1088/2515-7620/ae56d9
Publisher: Institute of Physics
Keywords: Greenhouse gas; Oil palm; Plant residue; Soil emission; Soil organic carbon
Sustainable Development Goals (SDGs): SDG 13: Climate Action, SDG 12: Responsible Consumption and Production, SDG 15: Life on Land
Depositing User: Ms. Siti Radziah Mohamed@mahmod
Date Deposited: 06 May 2026 08:06
Last Modified: 06 May 2026 08:06
Altmetrics: http://www.altmetric.com/details.php?domain=psasir.upm.edu.my&doi=10.1088/2515-7620/ae56d9
URI: http://psasir.upm.edu.my/id/eprint/125298
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