Particulate organic acids and overall water‐soluble aerosol composition measurements from the 2006 Gulf of Mexico Atmospheric Composition and Climate Study (GoMACCS)

Abstract

The Center for Interdisciplinary Remotely‐Piloted Aircraft Studies (CIRPAS) Twin Otter participated in the Gulf of Mexico Atmospheric Composition and Climate Study (GoMACCS) mission during August–September 2006. A particle‐into‐liquid sampler (PILS) coupled to ion chromatography was used to characterize the water‐soluble ion composition of aerosol and cloud droplet residual particles (976 5‐min PM1.0samples in total). Sulfate and ammonium dominated the water‐soluble mass (NH4++ SO42−= 84 ± 14%), while organic acids contributed 3.4 ± 3.7%. The average NH4+:SO42−molar ratio was 1.77 ± 0.85. Particulate concentrations of organic acids increased with decreasing carbon number from C9to C2. Organic acids were most abundant above cloud, presumably as a result of aqueous phase chemistry in cloud droplets, followed by subsequent droplet evaporation above cloud tops; the main product of this chemistry was oxalic acid. The evolution of organic acids with increasing altitude in cloud provides evidence for the multistep nature of oxalic acid production; predictions from a cloud parcel model are consistent with the observed oxalate:glyoxylate ratio as a function of altitude in GoMACCS cumuli. Suppressed organic acid formation was observed in clouds with relatively acidic droplets, as determined by high particulate nitrate concentrations (presumably high HNO3levels too) and lower liquid water content, as compared to other cloud fields probed. In the Houston Ship Channel region, an area with significant volatile organic compound emissions, oxalate, acetate, formate, benzoate, and pyruvate, in decreasing order, were the most abundant organic acids. Photo‐oxidation ofm‐xylene in laboratory chamber experiments leads to a particulate organic acid product distribution consistent with the Ship Channel area observations.