dc.contributor.authorKuwata, Mikinori
dc.contributor.authorKai, Fuu Ming
dc.contributor.authorYang, Liudongqing
dc.contributor.authorItoh, Masayuki
dc.contributor.authorGunawan, Haris
dc.contributor.authorHarvey, Charles F.
dc.date.accessioned2017-03-01T04:34:30Z
dc.date.available2017-03-01T04:34:30Z
dc.date.issued2017
dc.identifier.citationKuwata, M., Kai, F. M., Yang, L., Itoh, M., Gunawan, H., & Harvey, C. F. (2017). Temperature and burning history affect emissions of greenhouse gases and aerosol particles from tropical peatland fire. Journal of Geophysical Research: Atmospheres, 122(2), 1281-1292.en_US
dc.identifier.issn2169-897Xen_US
dc.identifier.urihttp://hdl.handle.net/10220/42140
dc.description.abstractTropical peatland burning in Asia has been intensifying over the last decades, emitting huge amounts of gas species and aerosol particles. Both laboratory and field studies have been conducted to investigate emission from peat burning, yet a significant variability in data still exists. We conducted a series of experiments to characterize the gas and particulate matter emitted during burning of a peat sample from Sumatra in Indonesia. Heating temperature of peat was found to regulate the ratio of CH4 to CO2 in emissions (ΔCH4/ΔCO2) as well as the chemical composition of particulate matter. The ΔCH4/ΔCO2 ratio was larger for higher temperatures, meaning that CH4 emission is more pronounced at these conditions. Mass spectrometric analysis of organic components indicated that aerosol particles emitted at higher temperatures had more unsaturated bonds and ring structures than that emitted from cooler fires. The result was consistently confirmed by nuclear magnetic resonance analysis. In addition, CH4 emitted by burning charcoal, which is derived from previously burned peat, was lower by at least an order of magnitude than that from fresh peat. These results highlight the importance of both fire history and heating temperature for the composition of tropical peat-fire emissions. They suggest that remote sensing technologies that map fire histories and temperatures could provide improved estimates of emissions.en_US
dc.description.sponsorshipNRF (Natl Research Foundation, S’pore)en_US
dc.description.sponsorshipMOE (Min. of Education, S’pore)en_US
dc.format.extent12 p.en_US
dc.language.isoenen_US
dc.relation.ispartofseriesJournal of Geophysical Research: Atmospheresen_US
dc.rights© 2016 American Geophysical Union. This paper was published in Journal of Geophysical Research: Atmospheres and is made available as an electronic reprint (preprint) with permission of American Geophysical Union. The published version is available at: [http://dx.doi.org/10.1002/2016JD025897]. One print or electronic copy may be made for personal use only. Systematic or multiple reproduction, distribution to multiple locations via electronic or other means, duplication of any material in this paper for a fee or for commercial purposes, or modification of the content of the paper is prohibited and is subject to penalties under law.en_US
dc.subjectwildfireen_US
dc.subjectpeatlanden_US
dc.titleTemperature and burning history affect emissions of greenhouse gases and aerosol particles from tropical peatland fireen_US
dc.typeJournal Article
dc.contributor.researchEarth Observatory of Singapore
dc.contributor.schoolSchool of Physical and Mathematical Sciencesen_US
dc.identifier.doihttp://dx.doi.org/10.1002/2016JD025897
dc.description.versionPublished versionen_US


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