Sources and characteristics of size-resolved particulate organic acids and methanesulfonate in a coastal megacity: Manila, Philippines
Author
Stahl, C.Templonuevo, Cruz, M.
Angela, Banãga, P.
Betito, G.
Braun, R.A.
Azadi, Aghdam, M.
Obiminda, Cambaliza, M.
Rose, Lorenzo, G.
MacDonald, A.B.
Hilario, M.RicardoA.
Corazon, Pabroa, P.
Robin, Yee, J.
Bernard, Simpas, J.
Sorooshian, A.
Affiliation
Department of Chemical and Environmental Engineering, University of ArizonaDepartment of Hydrology and Atmospheric Sciences, University of Arizona
Issue Date
2020
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Copernicus GmbHCitation
Stahl, C., Cruz, M. T., Bañaga, P. A., Betito, G., Braun, R. A., Aghdam, M. A., ... & Sorooshian, A. (2020). Sources and characteristics of size-resolved particulate organic acids and methanesulfonate in a coastal megacity: Manila, Philippines. Atmospheric Chemistry and Physics, 20(24), 15907-15935.Rights
Copyright © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License.Collection Information
This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu.Abstract
A 16-month (July 2018-October 2019) dataset of size-resolved aerosol composition is used to examine the sources and characteristics of five organic acids (oxalate, succinate, adipate, maleate, phthalate) and methanesulfonate (MSA) in Metro Manila, Philippines. As one of the most polluted megacities globally, Metro Manila offers a view of how diverse sources and meteorology impact the relative amounts and size distributions of these species. A total of 66 sample sets were collected with a Micro-Orifice Uniform Deposit Impactor (MOUDI), of which 54 sets were analyzed for composition. Organic acids and MSA surprisingly were less abundant than in other global regions that are also densely populated. The combined species accounted for an average of 0.80 ± 0.66 % of total gravimetric mass between 0.056 and 18 μm, still leaving 33.74 % of mass unaccounted for after considering black carbon and water-soluble ions and elements. The unresolved mass is suggested to consist of non-water-soluble metals as well as both water-soluble and non-water-soluble organics. Oxalate was approximately an order of magnitude more abundant than the other five species (149 ± 94 ng m-3 versus others being < 10 ng m-3) across the 0.056-18 μm size range. Both positive matrix factorization (PMF) and correlation analysis are conducted with tracer species to investigate the possible sources of organic acids and MSA. Enhanced biomass burning influence in the 2018 southwest monsoon resulted in especially high levels of submicrometer succinate, MSA, oxalate, and phthalate. Peculiarly, MSA had negligible contributions from marine sources but instead was linked to biomass burning and combustion. Enhanced precipitation during the two monsoon seasons (8 June-4 October 2018 and 14 June-7 October 2019) coincided with a stronger influence from local emissions rather than long-range transport, leading to notable concentration enhancements in both the sub- A nd supermicrometer ranges for some species (e.g., maleate and phthalate). While secondary formation via gas-to-particle conversion is consistent with submicrometer peaks for the organic acids and MSA, several species (i.e., phthalate, adipate, succinate, oxalate) exhibited a prominent peak in the coarse mode, largely owing to their association with crustal emissions (i.e., more alkaline aerosol type) rather than sea salt. Oxalate's strong association with sulfate in the submicrometer mode supports an aqueous-phase formation pathway for the study region. However, high concentrations during periods of low rain and high solar radiation suggest photo-oxidation is an important formation pathway. © 2020 Author(s).Note
Open access journalISSN
1680-7316Version
Final published versionae974a485f413a2113503eed53cd6c53
10.5194/acp-20-15907-2020
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Except where otherwise noted, this item's license is described as Copyright © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License.

