Abstract
A total of 238 samples of PM2.5 and TSP were analyzed to study the characteristics, sources, and formation pathways of aerosol oxalate in Shanghai in four seasons of 2007. The concentrations of oxalate were 0.07–0.41 μg/m3 in PM2.5 and 0.10–0.48 μg/m3 in TSP, respectively. Oxalate displayed a seasonal variation of autumn > summer > winter > spring in both PM2.5 and TSP and was dominantly present in PM2.5 in all samples. Correlation between oxalate and K+ and high ratio of oxalate/K+ suggested that biomass burning was a secondary source of aerosol oxalate in Shanghai, in addition to urban VOCs sources (vehicular and industrial emissions), especially in autumn. Secondary formation accounted for the majority of aerosol oxalate in Shanghai, which was supported by the high correlation of oxalate with nss-SO4 2−, K+ and NO3 −, proceeding from different mechanisms. Relatively high ambient RH together with high cloud cover was found benefiting the secondary formation of aerosol oxalate. The in-cloud process (aqueous-phase oxidation) was proposed to be likely the major formation pathway of aerosol oxalate in Shanghai, which was supported by the high correlation of oxalate with nss-SO4 2− and K+, dominant residence of oxalate in droplet mode and result of favorable meteorological condition analysis. High correlation of oxalate and NO3 − reflected the OH radical involved oxidation chemistry of the two species in the atmosphere and also suggested that gas-particle surface reactions and the evaporation–condensation process were both possible secondary formation pathways of aerosol oxalate in coarser particle mode (>1.0 μm). As a major water-soluble organic compound in aerosols, concentration of oxalate showed a distinct negative correlation to the atmospheric visibility, which implied that aerosol organic compounds could play an important role in haze pollution as well as in air quality in Shanghai.
Similar content being viewed by others
References
Kawamura K, Ikushima K (1993) Seasonal changes in the distribution of dicarboxylic acids in the urban atmosphere. Environ Sci Technol 27:2227–2235
Facchini MC, Fuzzi S, Zappoli S et al (1999) Partitioning of the organic aerosol component between fog droplets and interstitial air. J Geophys Res 104:26821–26832
Mader BT, Yu JZ, Xu JH et al (2004) Molecular composition of the water-soluble fraction of atmospheric carbonaceous aerosols collected during ACE: Asia. J Geophys Res 109:D06206. doi:10.1029/2003JD004105
Cruz CN, Pandis SN (1998) The effect of organic coatings on the cloud condensation nuclei activation of inorganic atmospheric aerosol. J Geophys Res 103:13111–13123
Kumar PP, Broekhuizen K, Abbatt JPD (2003) Organic acids as cloud condensation nuclei: laboratory studies of highly soluble and insoluble species. Atmos Chem Phys 3:509–520
Facchini MC, Mircea M, Fuzzi S et al (1999) Cloud albedo enhancement by surface-active organic solutes in growing droplets. Nature 401:257–259
Kerminen VM (2001) Relative roles of secondary sulfate and organics in atmospheric cloud condensation nuclei production. J Geophys Res 106:17321–17333
Lu GX, Guo XL (2012) Distribution and origin of aerosol and its transform relationship with CCN derived from the spring multi-aircraft measurements of Beijing cloud experiment (BCE). Chin Sci Bull 57:2460–2469
Jickells TD, An ZS, Andersen KK et al (2005) Global iron connections between desert dust, ocean biogeochemistry, and climate. Science 308:67–71
Kawamura K, Sakaguchi F (1999) Molecular distributions of water soluble dicarboxylic acids in marine aerosols over the Pacific Ocean including tropics. J Geophys Res 104:3501–3509
Kerminen VM, Ojanen C, Pakkanen T et al (2000) Low-molecular weight dicarboxylic acids in an urban and rural atmosphere. J Aerosol Sci 31:349–362
Carlton AG, Turpin BJ, Altieri KE et al (2007) Atmospheric oxalic acid and SOA production from glyoxal: results of aqueous photooxidation experiments. Atmos Environ 41:7588–7602
Sullivan RC, Prather KA (2007) Investigations of the diurnal cycle and mixing state of oxalic acid in individual particles in Asian aerosol outflow. Environ Sci Technol 41:8062–8069
Huang XF, Yu JZ, He LY et al (2006) Water-soluble organic carbon and oxalate in aerosols at a coastal urban site in China: size distribution characteristics, sources, and formation mechanism. J Geophys Res 111:D22212. doi:10.1029/2006JD007408
Seinfeld JH, Pandis SN (1998) Atmospheric chemistry and physic: from air pollution to climate change. Wiley-Interscience, New York
Blando JD, Turpin BJ (2000) Secondary organic aerosol formation in cloud and fog droplets: a literature evaluation of plausibility. Atmos Environ 34:1623–1632
Yao XH, Lau APS, Fang M et al (2003) Size distribution and formation of ionic species in atmospheric particulate pollutants in Beijing, China: 2-dicarboxylic acids. Atmos Environ 37:3001–3007
Crahan KK, Hegg D, Covert DS et al (2004) An exploration of aqueous oxalic acid production in the coastal marine atmosphere. Atmos Environ 38:3757–3764
Yu JZ, Huang XF, Xu J et al (2005) When aerosol sulfate goes up, so does oxalate: implication for the formation mechanisms of oxalate. Environ Sci Technol 39:128–133
Sorooshian A, Varutbangkul V, Brechtel FJ et al (2006) Oxalic acid in clear and cloudy atmospheres: analysis of data from international consortium for atmospheric research on transport and transformation 2004. J Geophys Res 111:D23S45. doi:10.1029/2005JD006880
Martinelango PK, Dasgupta PK, Al-Horr RS (2007) Atmospheric production of oxalic acid/oxalate and nitric acid/nitrate in the Tampa Bay airshed: parallel pathways. Atmos Environ 41:4258–4269
Yin J, Tan J (2003) Effect of surface wind direction on air pollutant concentrations in Shanghai. Meteorol Sci Technol 31:366–369 (in Chinese)
Taha G, Box GP, Cohen DD et al (2007) Black carbon measurement using laser integrating plate method. Aerosol Sci Technol 41:266–276
Yuan H, Wang Y, Zhuang GS (2003) Simultaneous determination of organic acids, methane sulfonic acid and inorganic anions in aerosol and precipitation samples by ion chromatography. J Instrum Anal 22:11–14 (in Chinese)
Zhuang G, Guo JH, Yuan H et al (2001) The compositions, sources, and size distribution of the dust storm from China in spring of 2000 and its impact on the global environment. Chin Sci Bull 46:895–901
Sun YL, Zhuang GS, Wang Y et al (2004) The air-borne particulate pollution at Beijing—concentrations, composition, distribution, and sources of Beijing aerosol. Atmos Environ 38:5991–6004
Limbeck A, Puxbaum H, Otter L et al (2001) Semivolatile behavior of dicarboxylic acids and other polar organic species at a rural background site (Nylsvley, RSA). Atmos Environ 35:1853–1862
Pathak RK, Chan CK (2005) Inter-particle and gas-particle interactions in sampling artifacts of PM2.5 in filter-based samplers. Atmos Environ 39:1597–1607
Fu QY, Zhuang GS, Wang J et al (2008) Mechanism of formation of the heaviest pollution episode ever recorded in the Yangtze River Delta, China. Atmos Environ 42:2023–2036
Yao XH, Chan CK, Fang M et al (2002) The water-soluble ionic composition of PM2.5 in Shanghai and Beijing. China. Atmos Environ 36:4223–4234
Yang H, Yu JZ, Ho SS et al (2005) The chemical composition of inorganic and carbonaceous materials in PM2.5 in Nanjing, China. Atmos Environ 39:3735–3749
Yao XH, Fang M, Chan CK et al (2004) Characterization of dicarboxylic acids in PM2.5 in Hong Kong. Atmos Environ 38:963–970
Wang Y, Zhuang GS, Chen S et al (2007) Characteristics and sources of formic, acetic and oxalic acids in PM2.5 and PM10 in Beijing, China. Atmos Res 84:169–181
Sempere R, Kawamura K (1994) Comparative distribution of dicarboxylic acids and related polar compounds in snow, rain and aerosols from urban atmosphere. Atmos Environ 28:449–459
Uchiyama S (1996) The behavior of oxalic acid in atmospheric aerosols. J Jpn Soc Atmos Environ 31:141–148
Kawamura K, Kaplan IR (1987) Motor exhaust emissions as a primary source for dicarboxylic acids in Los Angeles ambient air. Environ Sci Technol 21:105–110
Dasgupta PK, Campbell SW, Al-Horr RS et al (2007) Conversion of sea salt aerosol to and the production of HCl: analysis of temporal behavior of aerosol chloride/nitrate and gaseous HCl/HNO3 concentrations with AIM. Atmos Environ 41:4242–4257
Zhuang H, Chan CK, Fang M et al (1999) Size distributions of particulate sulfate, nitrate, and ammonium at a coastal site in Hong Kong. Atmos Environ 33:843–853
Pitts JN Jr, Biermann HW, Winer AM et al (1984) Spectroscopic identification and measurement of gaseous nitrous acid in dilute auto exhaust. Atmos Environ 18:847–854
McHenry JN, Dennis RL (1994) The relative importance of oxidation pathways and clouds to atmospheric ambient sulfate production as predicted by the regional acid deposition model. J Appl Meteorol Clim 33:890–905
Finlayson-Pitts BJ, Pitts JN Jr (1999) Chemistry of the upper and lower atmosphere: theory, experiments, and applications. Academic Press, New York
Lefer BL, Talbot RW (2001) Summertime measurements of aerosol nitrate and ammonium at northeastern U.S. site. J Geophys Res 106:20365–20378
Yamasoe MA, Artaxo P, Miguel AH et al (2000) Chemical composition of aerosol particles from direct emissions of vegetation fires in the Amazon Basin: water soluble species and trace elements. Atmos Environ 34:1641–1653
Rogers CF, Hudson GJ, Zielinska B et al (1991) Global biomass burning: atmospheric, climatic and biospheric implications. MIT Press, Cambridge, MA
Novakov T, Corrigan CE (1996) Cloud condensation nucleus activity of the organic component of biomass smoke particles. Geophys Res Lett 23:2141–2144
Warneck P (1999) Chemistry of the natural atmosphere. Academic Press, London
Warneck P (2003) In-cloud chemistry opens pathway to the formation of oxalic acid in the marine atmosphere. Atmos Environ 37:2423–2427
Okada K, Ikegami M, Zaizen Y et al (2001) The mixture state of individual aerosol particles in the 1997 Indonesian haze episode. J Aerosol Sci 32:1269–1279
Chen LWA, Chow JC, Doddridge BG et al (2003) Analysis of a summertime PM2.5 and haze episode in the mid-Atlantic region. J Air Waste Manage Assoc 53:946–956
Yadav AK, Kumar K, Kasim A et al (2003) Visibility and incidence of respiratory diseases during the 1998 haze episode in Brunei Darussalam. Pure Appl Geophys 160:265–277
Sun YL, Zhuang GS, Tang AH et al (2006) Chemical characteristics of PM2.5 and PM10 in haze-fog episodes in Beijing. Environ Sci Technol 41:3148–3155
An JL, Li Y, Chen Y et al (2013) Enhancements of major aerosol components due to additional HONO sources in the North China Plain and implications for visibility and haze. Adv Atmos Sci 30:57–66
Decesari S, Facchini MC, Matta E et al (2001) Chemical features and seasonal variation of water soluble organic compounds in the Po valley fine aerosol. Atmos Environ 35:3691–3699
Decesari S, Fuzzi S, Facchini MC et al (2006) Characterization of the organic composition of aerosols from Rondonia, Brazil, during the LBA-SMOCC 2002 experiment and its representation through model compounds. Atmos Chem Phys 6:375–402
Lim HJ, Turpin BJ (2002) Origins of primary and secondary organic aerosol in Atlanta: results’ of time-resolved measurements during the Atlanta supersite experiment. Environ Sci Technol 36:4489–4496
Hennigan CJ, Bergin MH, Weber RJ (2008) Correlations between water-soluble organic aerosol and water vapor: a synergistic effect from biogenic emissions. Environ Sci Technol 42:9079–9085
Wang Y, Zhuang GS, Tang AH et al (2007) The evolution of chemical components of aerosols at five monitoring sites of China during dust storms. Atmos Environ 41:1091–1106
Chow JC, Watson JG, Doraiswamy P et al (2009) Aerosol light absorption, black carbon, and elemental carbon at the Fresno Supersite, California. Atmos Res 93:874–887
Zhang Q, Jimenez J (2007) Ubiquity and dominance of oxygenated species in organic aerosols in anthropogenically-influenced Northern Hemisphere midlatitudes. Geophys Res Lett 34:L13801. doi:10.1029/2007GL029979
Myhre CEL, Nielson CJ (2004) Optical properties in the UV and visible spectral region of organic acids relevant to tropospheric aerosols. Atmos Chem Phys 4:1759–1769
Garland RM, Ravishankara AR, Lovejoy ER et al (2007) Parameterization for the relative humidity dependence of light extinction: organic-ammonium sulfate aerosol. J Geophys Res 112:D19303. doi:10.1029/2006JD008179
Cheng Y, Wiedensohler A, Eichler H et al (2008) Aerosol optical properties and related chemical apportionment at Xinken in Pearl River Delta of China. Atmos Environ 42:6351–6372
Huang K (2010) The transformation of aerosol components during the long-range transport of Asian dust and the formation mechanism of haze in mega-city, China. Dissertation, Fudan University (in Chinese)
Zhang RY, Suh I, Zhao J et al (2004) Atmospheric new particle formation enhanced by organic acids. Science 304:1487–1490
Acknowledgments
This study was supported by the Great International Collaboration Project of MOST, China (2010DFA92230), the National Basic Research Program of China (2006CB403704), and the National Natural Science Foundation of China (20877020 and 20977017).
Author information
Authors and Affiliations
Corresponding author
About this article
Cite this article
Jiang, Y., Zhuang, G., Wang, Q. et al. Aerosol oxalate and its implication to haze pollution in Shanghai, China. Chin. Sci. Bull. 59, 227–238 (2014). https://doi.org/10.1007/s11434-013-0009-4
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s11434-013-0009-4