Spatio-temporal distributions of dicarboxylic acids, ω-oxocarboxylic acids, pyruvic acid, α-dicarbonyls and fatty acids in the marine aerosols from the North and South Pacific

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• 作者：Mir Md. Mozammal Hoque^a ; ^b ; ¹ ; Kimitaka Kawamura^a ; ² ; ^{kkawamura@isc.chubu.ac.jp} ; Mitsuo Uematsu^c
• 关键词：Aerosols ; Spatio-temporal distributions ; Dicarboxylic acids ; Oxalic acid ; Glyoxylic acid
• 刊名：Atmospheric Research
• 出版年：2017
• 出版时间：1 March 2017
• 年：2017
• 卷：185
• 期：Complete
• 页码：158-168
• 全文大小：2042 K
• 卷排序：185

文摘

Aerosol samples (TSP) were collected during a cruise in the North (3°05′N–34°02′N) and South (6°59′S–25°46′S) Pacific to investigate the spatio-temporal distributions of water-soluble dicarboxylic acids and related compounds. The molecular distributions of diacids were characterized by the predominance of oxalic (C2) acid followed by malonic (C3) and then succinic (C4) acid. However, we found a predominance of C4 over C3 in the aerosol sample that was collected in the western North Pacific Rim with a heavy influence from continental air masses. Atmospheric abundances of short chain diacids (C2–C4) are 2–3 times higher in the North Pacific than in the South Pacific. During the cruise, abundances of C2 in the western North Pacific are 5 times higher than those in the rest of the samples collected. Moreover, the aerosol samples collected in the western North Pacific demonstrated that glyoxylic (ωC2) acid and methylglyoxal (MeGly) were dominant together with C2. We found a strong correlation between C2 and ωC2 (r = 0.87) and C2 and MeGly (r = 0.97) in the western North Pacific aerosols but the correlations are significantly weak in the samples from the central North Pacific and Southern Ocean. Diacids were found to account for 1.6 to 14% of organic carbon with higher values in the western North Pacific. These results, together with 7-day backward air mass trajectories, indicate that ωC2 and MeGly are both originated from the photochemical oxidation of continent-derived organic precursors including isoprene, which can serve as precursors for the production of C2 during long-range atmospheric transport.