Effect of compaction on soil CO2 and CH4 fluxes from tropical peatland in Sarawak, Malaysia

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dc.contributor.authorNur Azima Busman
dc.contributor.authorNagamitsu Maie
dc.contributor.authorChe Fauziah Ishak
dc.contributor.authorMuhammad Firdaus Sulaiman
dc.contributor.authorLulie Melling
dc.coverage.publicationMalaysia
dc.date.accessioned2024-05-15T01:44:18Z
dc.date.available2024-05-15T01:44:18Z
dc.date.issued2021
dc.description.abstractTropical peatland stores a large amount of carbon (C) and is an important C sink. In Malaysia, about 25% of the peatland area has been converted to oil palm plantation where drainage, compaction and groundwater table control are prerequisite. To date, relationship between land compaction and C emission from tropical peatland is scarcely studied. To understand the effect of compaction on soil carbon dioxide (CO2) and methane (CH4) flux from tropical peatland, a laboratory soil column incubation was conducted.
dc.identifier.citationBusman, N. A., Maie, N., Ishak, C. F., Sulaiman, M. F., & Melling, L. (2021). Effect of compaction on soil CO 2 and CH 4 fluxes from tropical peatland in Sarawak, Malaysia. Environment, Development and Sustainability, 23, 11646-11659.
dc.identifier.urihttps://repoemc.ukm.my/handle/123456789/762
dc.languageen
dc.publisherSpringer
dc.publisher.alternativeEnvironment, Development and Sustainability
dc.subjectCO2 flux
dc.subjectCH4 flux
dc.subjectSoil compaction
dc.subjectSoil bulk density
dc.subjectTropical peatlands
dc.titleEffect of compaction on soil CO2 and CH4 fluxes from tropical peatland in Sarawak, Malaysia

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