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dc.contributor.authorAnas Ahmad Jamharien_US
dc.contributor.authorMohd Talib Latifen_US
dc.contributor.authorMuhammad Ikram A. Wahaben_US
dc.contributor.authorHanashriah Hassanen_US
dc.contributor.authorMurnira Othmanen_US
dc.contributor.authorHaris Hafizal Abd Hamiden_US
dc.contributor.authorPerapong Tekasakulen_US
dc.contributor.authorWorradorn Phairuangen_US
dc.contributor.authorMitsuhiko Hataen_US
dc.contributor.authorMasami Furuchien_US
dc.contributor.authorNor Fadilah Rajaben_US
dc.date.accessioned2022-05-27T08:28:42Z-
dc.date.available2022-05-27T08:28:42Z-
dc.date.issued2022-01-01en_US
dc.identifier.issn18791298en_US
dc.identifier.issn00456535en_US
dc.identifier.other2-s2.0-85115978362en_US
dc.identifier.other10.1016/j.chemosphere.2021.132309en_US
dc.identifier.urihttps://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=85115978362&origin=inwarden_US
dc.identifier.urihttp://cmuir.cmu.ac.th/jspui/handle/6653943832/72723-
dc.description.abstractThis study aims to determine the inorganic and carbonaceous components depending on the seasonal variation and size distribution of urban air particles in Kuala Lumpur. Different fractions of particulate matter (PM) were measured using a Nanosampler from 17 February 2017 until 27 November 2017. The water-soluble inorganic ions (WSIIs) and carbonaceous components in all samples were analysed using ion chromatography and carbon analyser thermal/optical reflectance, respectively. Total PM concentration reached its peak during the southwest (SW) season (70.99 ± 6.04 μg/m3), and the greatest accumulation were observed at PM0.5–1.0 (22%–30%, 9.55 ± 1.03 μg/m3) and PM2.5–10 (22%–25%, 10.34 ± 0.81 μg/m3). SO42−, NO3− and NH4+ were major contributors of WSIIs, and their formation was favoured mainly during SW season (80.5% of total ions). PM0.5–1.0 and PM2.5–10 exhibited the highest percentage of WSII size distribution, accounted for 28.4% and 13.5% of the total mass, respectively. The average contribution of carbonaceous species (OC + EC) to total carbonaceous concentrations were higher in PM0.5–1.0 (35.2%) and PM2.5–10 (26.6%). Ultrafine particles (PM<0.1) consistently indicated that the sources were from vehicle emission while the SW season was constantly dominated by biomass burning sources. Using the positive matrix factorization (PMF) model, secondary inorganic aerosol and biomass burning (30.3%) was known as a significant source of overall PM. As a conclusion, ratio and source apportionment indicate the mixture of biomass burning, secondary inorganic aerosols and motor vehicle contributed to the size-segregated PM and seasonal variation of inorganic and carbonaceous components of urban air particles.en_US
dc.subjectChemistryen_US
dc.subjectEnvironmental Scienceen_US
dc.subjectMedicineen_US
dc.titleSeasonal variation and size distribution of inorganic and carbonaceous components, source identification of size-fractioned urban air particles in Kuala Lumpur, Malaysiaen_US
dc.typeJournalen_US
article.title.sourcetitleChemosphereen_US
article.volume287en_US
article.stream.affiliationsUniversiti Sultan Zainal Abidinen_US
article.stream.affiliationsKanazawa Universityen_US
article.stream.affiliationsPrince of Songkla Universityen_US
article.stream.affiliationsUniversiti Kebangsaan Malaysiaen_US
article.stream.affiliationsChiang Mai Universityen_US
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