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Tracing the Relative Significance of Primary versus Secondary Organic Aerosols from Biomass Burning Plumes over Coastal Ocean Using Sugar Compounds and Stable Carbon Isotopes
ACS Earth and Space Chemistry ( IF 2.9 ) Pub Date : 2019-07-08 00:00:00 , DOI: 10.1021/acsearthspacechem.9b00140
Srinivas Bikkina 1, 2 , Md. Mozammel Haque 1 , Manmohan Sarin 2 , Kimitaka Kawamura 1, 3
Affiliation  

Biomass burning (BB), a pivotal source of both primary and secondary organic aerosols (POA and SOA, respectively), affects the regional and global climate. We have used stable carbon isotopic composition (δ13CTC) of total carbon (TC) and BB tracers (anhydrosugars, sugars, and sugar alcohols) to elucidate the relative significance of POA and SOA over the Bay of Bengal, influenced by the long-range transport from the Indo-Gangetic Plain (IGP-outflow) and Southeast Asia (SEA-outflow) during a winter cruise. The molecular distributions of anhydrosugars (levoglucosan, Lev; galactosan, Gal; mannosan, Man) are different between IGP- (Lev > Gal > Man) and SEA-outflows (Lev > Man > Gal). The positive linear/nonlinear relationships of δ13CTC with total sugar-C, K+, water-soluble organic carbon (WSOC), and TC in BBOA from the SEA-outflow are in sharp contrast to those from Mt. Tai, China and Rondônia, Brazil in summer; mainly because of the prevailing differences in ambient photochemical processing. The Keeling plots (δ13CTC versus 1/TC, 1/WSOC, and 1/Lev) in the SEA-outflow revealed a mixing of “13C-enriched POA” and 13C-depleted “fresh-SOA” of BB origin. Because the sugar compounds are mostly water-soluble and become bioavailable in the surface waters, we estimate the air-to-sea depositions of sugar-C and WSOC over the Bay of Bengal to contribute to no more than 0.1% and 13%, respectively, of their supply via peninsular rivers.
更新日期:2019-07-08
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