Erin Swails, Steve Frolking, Jia Deng, Kristell Hergoualc’h
{"title":"退化增加了未排水热带泥炭沼泽林的泥炭温室气体排放量","authors":"Erin Swails, Steve Frolking, Jia Deng, Kristell Hergoualc’h","doi":"10.1007/s10533-023-01110-2","DOIUrl":null,"url":null,"abstract":"<div><p>Tropical peat swamp degradation can modify net peat greenhouse gas (GHG) emissions even without drainage. However, current Intergovernmental Panel on Climate Change (IPCC) guidelines do not provide default emission factors (EF) for anthropogenically-degraded undrained organic soils. We reviewed published field measurements of peat GHG fluxes in undrained undegraded and degraded peat swamp forests in Southeast Asia (SEA) and Latin America and the Caribbean (LAC). Degradation without drainage shifted the peat from a net CO<sub>2</sub> sink to a source in both SEA (− 2.9 ± 1.8 to 4.1 ± 2.0 Mg CO<sub>2</sub>–C ha<sup>−1</sup> yr<sup>−1</sup>) and LAC (− 4.3 ± 1.8 to 1.4 ± 2.2 Mg CO<sub>2</sub>–C ha<sup>−1</sup> yr<sup>−1</sup>). It raised peat CH<sub>4</sub> emissions (kg C ha<sup>−1</sup> yr<sup>−1</sup>) in SEA (22.1 ± 13.6 to 32.7 ± 7.8) but decreased them in LAC (218.3 ± 54.2 to 165.0 ± 4.5). Degradation increased peat N<sub>2</sub>O emissions (kg N ha<sup>−1</sup> yr<sup>−1</sup>) in SEA forests (0.9 ± 0.5 to 4.8 ± 2.3) (limited N<sub>2</sub>O data). It shifted peat from a net GHG sink to a source in SEA (− 7.9 ± 6.9 to 20.7 ± 7.4 Mg CO<sub>2</sub>-equivalent ha<sup>−1</sup> yr<sup>−1</sup>) and increased peat GHG emissions in LAC (9.8 ± 9.0 to 24.3 ± 8.2 Mg CO<sub>2</sub>-equivalent ha<sup>−1</sup> yr<sup>−1</sup>). The large observed increase in net peat GHG emissions in undrained degraded forests compared to undegraded conditions calls for their inclusion as a new class in the IPCC guidelines. As current default IPCC EF for tropical organic soils are based only on data collected in SEA ombrotrophic peatlands, expanded geographic representation and refinement of peat GHG EF by nutrient status are also needed.</p></div>","PeriodicalId":8901,"journal":{"name":"Biogeochemistry","volume":"167 1","pages":"59 - 74"},"PeriodicalIF":3.9000,"publicationDate":"2024-01-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://link.springer.com/content/pdf/10.1007/s10533-023-01110-2.pdf","citationCount":"0","resultStr":"{\"title\":\"Degradation increases peat greenhouse gas emissions in undrained tropical peat swamp forests\",\"authors\":\"Erin Swails, Steve Frolking, Jia Deng, Kristell Hergoualc’h\",\"doi\":\"10.1007/s10533-023-01110-2\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>Tropical peat swamp degradation can modify net peat greenhouse gas (GHG) emissions even without drainage. However, current Intergovernmental Panel on Climate Change (IPCC) guidelines do not provide default emission factors (EF) for anthropogenically-degraded undrained organic soils. We reviewed published field measurements of peat GHG fluxes in undrained undegraded and degraded peat swamp forests in Southeast Asia (SEA) and Latin America and the Caribbean (LAC). Degradation without drainage shifted the peat from a net CO<sub>2</sub> sink to a source in both SEA (− 2.9 ± 1.8 to 4.1 ± 2.0 Mg CO<sub>2</sub>–C ha<sup>−1</sup> yr<sup>−1</sup>) and LAC (− 4.3 ± 1.8 to 1.4 ± 2.2 Mg CO<sub>2</sub>–C ha<sup>−1</sup> yr<sup>−1</sup>). It raised peat CH<sub>4</sub> emissions (kg C ha<sup>−1</sup> yr<sup>−1</sup>) in SEA (22.1 ± 13.6 to 32.7 ± 7.8) but decreased them in LAC (218.3 ± 54.2 to 165.0 ± 4.5). Degradation increased peat N<sub>2</sub>O emissions (kg N ha<sup>−1</sup> yr<sup>−1</sup>) in SEA forests (0.9 ± 0.5 to 4.8 ± 2.3) (limited N<sub>2</sub>O data). It shifted peat from a net GHG sink to a source in SEA (− 7.9 ± 6.9 to 20.7 ± 7.4 Mg CO<sub>2</sub>-equivalent ha<sup>−1</sup> yr<sup>−1</sup>) and increased peat GHG emissions in LAC (9.8 ± 9.0 to 24.3 ± 8.2 Mg CO<sub>2</sub>-equivalent ha<sup>−1</sup> yr<sup>−1</sup>). The large observed increase in net peat GHG emissions in undrained degraded forests compared to undegraded conditions calls for their inclusion as a new class in the IPCC guidelines. As current default IPCC EF for tropical organic soils are based only on data collected in SEA ombrotrophic peatlands, expanded geographic representation and refinement of peat GHG EF by nutrient status are also needed.</p></div>\",\"PeriodicalId\":8901,\"journal\":{\"name\":\"Biogeochemistry\",\"volume\":\"167 1\",\"pages\":\"59 - 74\"},\"PeriodicalIF\":3.9000,\"publicationDate\":\"2024-01-08\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://link.springer.com/content/pdf/10.1007/s10533-023-01110-2.pdf\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Biogeochemistry\",\"FirstCategoryId\":\"93\",\"ListUrlMain\":\"https://link.springer.com/article/10.1007/s10533-023-01110-2\",\"RegionNum\":3,\"RegionCategory\":\"环境科学与生态学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"ENVIRONMENTAL SCIENCES\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Biogeochemistry","FirstCategoryId":"93","ListUrlMain":"https://link.springer.com/article/10.1007/s10533-023-01110-2","RegionNum":3,"RegionCategory":"环境科学与生态学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"ENVIRONMENTAL SCIENCES","Score":null,"Total":0}
Degradation increases peat greenhouse gas emissions in undrained tropical peat swamp forests
Tropical peat swamp degradation can modify net peat greenhouse gas (GHG) emissions even without drainage. However, current Intergovernmental Panel on Climate Change (IPCC) guidelines do not provide default emission factors (EF) for anthropogenically-degraded undrained organic soils. We reviewed published field measurements of peat GHG fluxes in undrained undegraded and degraded peat swamp forests in Southeast Asia (SEA) and Latin America and the Caribbean (LAC). Degradation without drainage shifted the peat from a net CO2 sink to a source in both SEA (− 2.9 ± 1.8 to 4.1 ± 2.0 Mg CO2–C ha−1 yr−1) and LAC (− 4.3 ± 1.8 to 1.4 ± 2.2 Mg CO2–C ha−1 yr−1). It raised peat CH4 emissions (kg C ha−1 yr−1) in SEA (22.1 ± 13.6 to 32.7 ± 7.8) but decreased them in LAC (218.3 ± 54.2 to 165.0 ± 4.5). Degradation increased peat N2O emissions (kg N ha−1 yr−1) in SEA forests (0.9 ± 0.5 to 4.8 ± 2.3) (limited N2O data). It shifted peat from a net GHG sink to a source in SEA (− 7.9 ± 6.9 to 20.7 ± 7.4 Mg CO2-equivalent ha−1 yr−1) and increased peat GHG emissions in LAC (9.8 ± 9.0 to 24.3 ± 8.2 Mg CO2-equivalent ha−1 yr−1). The large observed increase in net peat GHG emissions in undrained degraded forests compared to undegraded conditions calls for their inclusion as a new class in the IPCC guidelines. As current default IPCC EF for tropical organic soils are based only on data collected in SEA ombrotrophic peatlands, expanded geographic representation and refinement of peat GHG EF by nutrient status are also needed.
期刊介绍:
Biogeochemistry publishes original and synthetic papers dealing with biotic controls on the chemistry of the environment, or with the geochemical control of the structure and function of ecosystems. Cycles are considered, either of individual elements or of specific classes of natural or anthropogenic compounds in ecosystems. Particular emphasis is given to coupled interactions of element cycles. The journal spans from the molecular to global scales to elucidate the mechanisms driving patterns in biogeochemical cycles through space and time. Studies on both natural and artificial ecosystems are published when they contribute to a general understanding of biogeochemistry.