Seasonal variation and chemical characterization of PM<sub>2.5</sub> in northwestern Philippines

The seasonal and chemical characteristics of fine particulate matter (PM<sub>2.5</sub>) were investigated in Burgos, Ilocos Norte, located at the northwestern edge of the Philippines. Each 24 h sample of fine aerosol was collected for four seasons. Fine particulate in the region show...

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Bibliographic Details
Main Authors: G. Bagtasa, M. G. Cayetano, C.-S. Yuan
Format: Article
Language:English
Published: Copernicus Publications 2018-04-01
Series:Atmospheric Chemistry and Physics
Online Access:https://www.atmos-chem-phys.net/18/4965/2018/acp-18-4965-2018.pdf
Description
Summary:The seasonal and chemical characteristics of fine particulate matter (PM<sub>2.5</sub>) were investigated in Burgos, Ilocos Norte, located at the northwestern edge of the Philippines. Each 24 h sample of fine aerosol was collected for four seasons. Fine particulate in the region shows strong seasonal variation in both concentration and composition. Highest mass concentration was seen during the boreal spring season with a mean mass concentration of 21.6 ± 6.6 µg m<sup>−3</sup>, and lowest was in fall with a mean concentration of 8.4 ± 2.3 µg m<sup>−3</sup>. Three-day wind back trajectory analysis of air mass reveals the influence of the northwestern Pacific monsoon regimes on PM<sub>2.5</sub> concentration. During southwest monsoon, sea salt was the dominant component of fine aerosols carried by moist air from the South China Sea. During northeast monsoon, on the other hand, both wind and receptor model analysis showed that higher particulate concentration was due to the long-range transport (LRT) of anthropogenic emissions from northern East Asia. Overall, sea salt and soil comprise 33 % of total PM<sub>2.5</sub> concentration, while local biomass burning makes up 33 %. LRT of industrial emission, solid waste burning and secondary sulfate from East Asia have a mean contribution of 34 % to the total fine particulate for the whole sampling period.
ISSN:1680-7316
1680-7324