Guan Xhuan Wong, Ryuichi Hirata, Takashi Hirano, Frankie Kiew, Joseph Wenceslaus Waili, Ülo Mander, Kaido Soosaar, Lulie Melling
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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 (R<sub>n</sub>) and raising vapor pressure deficit (VPD). Following the tree removal, controlled burning temporarily warmed air temperature by 8 °C, increased VPD and significantly attenuated R<sub>n</sub>, resulting in negative values owing to radiation interception by smoke and increased surface warming. Contrary to expectations that drainage would lower CH<sub>4</sub> emissions, the site remained a consistent net source, with even higher emissions observed during and after conversion. The mean monthly NEE-CH<sub>4</sub> during conversion (23.3 ± 8.6 mg C m<sup>-2</sup> d<sup>-1</sup>) was about 2-times higher than before conversion (12.1 ± 5.3 mg C m<sup>-2</sup> d<sup>-1</sup>) and about 1.5-times higher than after conversion (16.3 ± 4.1 mg C m<sup>-2</sup> d<sup>-1</sup>). The heightened CH<sub>4</sub> release is likely attributable to emissions from drainage ditches, underscoring their significant role in post-conversion CH<sub>4</sub> dynamics. Despite its short duration, controlled burning substantially elevated NEE-CH<sub>4</sub>, ranging from 0.04 to 0.91 mg C m<sup>-2</sup> s<sup>-1</sup>. Our findings highlight the substantial impact of land conversion on peatland CH<sub>4</sub> dynamics, emphasizing the need for accurate flux measurements across various conversion stages to refine global CH<sub>4</sub> budgets.</p>","PeriodicalId":422,"journal":{"name":"Science of the Total Environment","volume":"962 ","pages":"178466"},"PeriodicalIF":8.2000,"publicationDate":"2025-01-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Impact of land conversion on environmental conditions and methane emissions from a tropical peatland.\",\"authors\":\"Guan Xhuan Wong, Ryuichi Hirata, Takashi Hirano, Frankie Kiew, Joseph Wenceslaus Waili, Ülo Mander, Kaido Soosaar, Lulie Melling\",\"doi\":\"10.1016/j.scitotenv.2025.178466\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p><p>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 CH<sub>4</sub> exchange (NEE-CH<sub>4</sub>) 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 (R<sub>n</sub>) and raising vapor pressure deficit (VPD). Following the tree removal, controlled burning temporarily warmed air temperature by 8 °C, increased VPD and significantly attenuated R<sub>n</sub>, resulting in negative values owing to radiation interception by smoke and increased surface warming. Contrary to expectations that drainage would lower CH<sub>4</sub> emissions, the site remained a consistent net source, with even higher emissions observed during and after conversion. The mean monthly NEE-CH<sub>4</sub> during conversion (23.3 ± 8.6 mg C m<sup>-2</sup> d<sup>-1</sup>) was about 2-times higher than before conversion (12.1 ± 5.3 mg C m<sup>-2</sup> d<sup>-1</sup>) and about 1.5-times higher than after conversion (16.3 ± 4.1 mg C m<sup>-2</sup> d<sup>-1</sup>). The heightened CH<sub>4</sub> release is likely attributable to emissions from drainage ditches, underscoring their significant role in post-conversion CH<sub>4</sub> dynamics. Despite its short duration, controlled burning substantially elevated NEE-CH<sub>4</sub>, ranging from 0.04 to 0.91 mg C m<sup>-2</sup> s<sup>-1</sup>. 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引用次数: 0
摘要
热带泥炭地是甲烷(CH₄)的重要来源,但由于缺乏长期、连续和高频通量测量,它们对全球CH₄预算的贡献仍然难以量化。为了解决这一差距,我们使用涡动相关技术测量了热带泥炭沼泽森林向油棕种植园转化过程中生态系统净CH4交换(NEE-CH4)。这包括2014年至2020年转换期之前、期间和之后的时期,在此期间观察到重大的环境变化。抽干泥炭地使月平均地下水位从转化前的-20.0±14.2 cm大幅降低至转化过程中的-102.3±31.6 cm,转化后略有上升至-96.5±19.3 cm。森林砍伐使月平均土壤温度升高2.3 ~ 3.1°C,减少净辐射(Rn),提高蒸汽压亏缺(VPD)。在树木被砍伐后,控制燃烧使空气温度暂时升高了8°C, VPD增加,Rn显著衰减,由于烟雾拦截辐射和增加地表升温,导致负值。与排水会降低CH4排放的预期相反,该场地仍然是一个稳定的净排放源,在转化期间和之后观测到的排放量甚至更高。转化期间月平均NEE-CH4(23.3±8.6 mg C m-2 d-1)是转化前(12.1±5.3 mg C m-2 d-1)的2倍左右,是转化后(16.3±4.1 mg C m-2 d-1)的1.5倍左右。CH4释放的增加可能归因于排水沟的排放,强调了它们在转化后CH4动态中的重要作用。尽管持续时间很短,但受控燃烧显著提高了NEE-CH4,范围从0.04到0.91 mg C m-2 s-1。我们的研究结果强调了土地转换对泥炭地CH4动态的重大影响,强调需要在不同转换阶段进行精确的通量测量,以完善全球CH4预算。
Impact of land conversion on environmental conditions and methane emissions from a tropical peatland.
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.
期刊介绍:
The Science of the Total Environment is an international journal dedicated to scientific research on the environment and its interaction with humanity. It covers a wide range of disciplines and seeks to publish innovative, hypothesis-driven, and impactful research that explores the entire environment, including the atmosphere, lithosphere, hydrosphere, biosphere, and anthroposphere.
The journal's updated Aims & Scope emphasizes the importance of interdisciplinary environmental research with broad impact. Priority is given to studies that advance fundamental understanding and explore the interconnectedness of multiple environmental spheres. Field studies are preferred, while laboratory experiments must demonstrate significant methodological advancements or mechanistic insights with direct relevance to the environment.