Abstract:The ammonium sulfate ((NH 4 ) 2 SO 4 ) seed aerosols commonly found in the Chinese urban atmosphere could affect the formation and aging of secondary organic aerosols (SOA). Aging of aromatic SOA is performed using UV-irradiation of 1,3,5-trimethylbenzene (135-TMB)/CH 3 ONO/NO/air mixtures with high concentrations (~100 μg/m 3 ) of (NH 4 ) 2 SO 4 seeds in the laboratory chamber in this study. The particulate products of SOA were measured using an aerosol laser time-of-flight mass spectrometer (ALTOFMS) in real… Show more
“…The reaction products were characterized by UV-visible spectroscopy, infrared spectroscopy and time-of-flight mass spectrometry. The series of characteristic mass spectral peaks C x H y N n + of imidazole nitrogen-containing organic compounds of aromatic SOA were obtained, and it was confirmed that imidazole nitrogen-containing compounds formed from the heterogeneous reaction of NH 3 and dicarbonyl components of aromatic SOA [22][23][24]. On this basis, this paper continues to study the effects of different ingredients, concentrations, humidity and acidity of seed aerosol on the formation of nitrogencontaining organic compounds formed from the reaction of NH 3 with the photooxidation products of toluene.…”
Section: Introductionmentioning
confidence: 61%
“…1. The mass spectrum peak with the highest peak intensity of m/z 41 (C 2 H 2 N + ), along with m/z 67 (C 3 H 3 N 2 + ) and 28 (CH 2 N + ) are the characteristic cracking peaks of the imidazole compounds, indicating that the nitrogen-containing imidazole organic compounds are the main reaction product [22][23][24]. In addition, in the mass spectrum, the fragment peak of m/z 18 corresponds to the ammonium ion (NH 4 + ), and m/z 44 is the fragment peak (COO + ) after the carboxyl group (-COOH) of the organic acid compound loses the hydrogen atom.…”
Section: Resultsmentioning
confidence: 99%
“…Since the formed NH 4 + is the weak acid, it cannot react with the condensed organic acid to form ammonium acid. According to the experimental results of Liu et al [7] and our group [23][24], the hydration of the dialdehyde compound and the reaction with NH 3 to form the tetraol and diimine products are important precursors for the formation of imidazole products. Since the reactivity of NH 4 + is less than that of NH 3 , the rate of NH 3 reaction with the condensed dialdehyde compound to form diimine is low, and the yield is small, resulting in the decrease of imidazole products.…”
Section: Effect Of Different Acidity Of Calcium Chloridementioning
confidence: 93%
“…The chemical composition of aerosol particles is gained from the ion peaks in the mass spectrum. Also, after the completion of the photoreaction, the products were collected with a 3% methanol solution for the UV-Vis spectrometric measurement as provided in our previous studies [23][24].…”
Ammonia (NH 3) is the most important alkaline pollution gas in the atmosphere, and the nitrogen-containing organic compounds formed by photooxidation with toluene is the main component of atmospheric brown carbon (BrC). Inorganic seed aerosols such as ammonium sulfate and calcium chloride can affect the formation and chemical composition of secondary organic aerosol (SOA), because of their large surface area. The effects of seed aerosols with different ingredients, concentrations, humidity and acidity on the formation of nitrogen-containing organic compounds were studied qualitatively by UV-Vis spectrometry in this study. The results showed that inorganic seed aerosols promoted the formation of nitrogen-containing organic compounds. The order of promotion is calcium chloride > sodium silicate > ammonium sulfate > sodium chloride > ammonium nitrate. The formation concentration of nitrogen-containing organic products gradually increases with the increase of calcium chloride seed aerosol concentration and acidity. When the seed aerosol is alkaline, it is not conducive to its formation. The increase of water molecules would reduce the concentration of nitrogen-containing organic products as the relative humidity increases. These would provide new experimental basis for the formation mechanism of brown carbon of aromatic SOA.
“…The reaction products were characterized by UV-visible spectroscopy, infrared spectroscopy and time-of-flight mass spectrometry. The series of characteristic mass spectral peaks C x H y N n + of imidazole nitrogen-containing organic compounds of aromatic SOA were obtained, and it was confirmed that imidazole nitrogen-containing compounds formed from the heterogeneous reaction of NH 3 and dicarbonyl components of aromatic SOA [22][23][24]. On this basis, this paper continues to study the effects of different ingredients, concentrations, humidity and acidity of seed aerosol on the formation of nitrogencontaining organic compounds formed from the reaction of NH 3 with the photooxidation products of toluene.…”
Section: Introductionmentioning
confidence: 61%
“…1. The mass spectrum peak with the highest peak intensity of m/z 41 (C 2 H 2 N + ), along with m/z 67 (C 3 H 3 N 2 + ) and 28 (CH 2 N + ) are the characteristic cracking peaks of the imidazole compounds, indicating that the nitrogen-containing imidazole organic compounds are the main reaction product [22][23][24]. In addition, in the mass spectrum, the fragment peak of m/z 18 corresponds to the ammonium ion (NH 4 + ), and m/z 44 is the fragment peak (COO + ) after the carboxyl group (-COOH) of the organic acid compound loses the hydrogen atom.…”
Section: Resultsmentioning
confidence: 99%
“…Since the formed NH 4 + is the weak acid, it cannot react with the condensed organic acid to form ammonium acid. According to the experimental results of Liu et al [7] and our group [23][24], the hydration of the dialdehyde compound and the reaction with NH 3 to form the tetraol and diimine products are important precursors for the formation of imidazole products. Since the reactivity of NH 4 + is less than that of NH 3 , the rate of NH 3 reaction with the condensed dialdehyde compound to form diimine is low, and the yield is small, resulting in the decrease of imidazole products.…”
Section: Effect Of Different Acidity Of Calcium Chloridementioning
confidence: 93%
“…The chemical composition of aerosol particles is gained from the ion peaks in the mass spectrum. Also, after the completion of the photoreaction, the products were collected with a 3% methanol solution for the UV-Vis spectrometric measurement as provided in our previous studies [23][24].…”
Ammonia (NH 3) is the most important alkaline pollution gas in the atmosphere, and the nitrogen-containing organic compounds formed by photooxidation with toluene is the main component of atmospheric brown carbon (BrC). Inorganic seed aerosols such as ammonium sulfate and calcium chloride can affect the formation and chemical composition of secondary organic aerosol (SOA), because of their large surface area. The effects of seed aerosols with different ingredients, concentrations, humidity and acidity on the formation of nitrogen-containing organic compounds were studied qualitatively by UV-Vis spectrometry in this study. The results showed that inorganic seed aerosols promoted the formation of nitrogen-containing organic compounds. The order of promotion is calcium chloride > sodium silicate > ammonium sulfate > sodium chloride > ammonium nitrate. The formation concentration of nitrogen-containing organic products gradually increases with the increase of calcium chloride seed aerosol concentration and acidity. When the seed aerosol is alkaline, it is not conducive to its formation. The increase of water molecules would reduce the concentration of nitrogen-containing organic products as the relative humidity increases. These would provide new experimental basis for the formation mechanism of brown carbon of aromatic SOA.
“…As an important contributor to SOA in urban areas, aromatic hydrocarbons are generally concerned about their kinetics (Atkinson and Arey, 2003;Calvert et al, 2002), reaction mechanisms (Tsiligiannis et al, 2019;J. Midey * et al, 2003;Huang et al, 2017c;Wang et al, 2020;Garmash et al, 2019), SOA yield (Cao and Jang, 2007;Kroll et al, 2007;Ng et al, 2007b;Huang et al, 2017b), ozone generation potential (Luo et al, 2019), and SOA physicochemical properties (optical properties, morphology, etc.) (Grosjean, 1981;Li et al, 2018;Li et al, 2017b;Phillips and Smith, 2014;Kim and Paulson, 2013;Huang et al, 2018).…”
Abstract. Motor vehicle exhaust is one of the important contribution sources of secondary organic aerosol (SOA) in urban areas. Long-chain alkanes and aromatic hydrocarbons are included in gaseous organic pollutants of vehicle emissions, representative for diesel and gasoline vehicles respectively. In this work, the SOA production from individual anthropogenic volatile organic compounds (AVOCs) (n-dodecane, 1,3,5-trimethylbenzene) and mixed AVOCs (n-dodecane + 1,3,5-trimethylbenzene) were studied with a large-scale outdoor smog chamber. Results showed that the SOA formation from the mixed AVOCs was enhanced compared to the predicted SOA mass concentration based on the SOA yield of individual AVOCs. According to the results of mass spectrometry analysis with electrospray ionization time-of-flight mass spectrometry (ESI-TOF-MS), interaction occurred between intermediate products from the two precursors, which could be the main reason for the enhanced SOA production from the mixed AVOCs reaction system. This study indicates that further studies on SOA chemistry from the mixed VOCs reaction system are needed, as the interactions between them and the effect on SOA formation can give us a further understanding of the SOA formed in the atmosphere.
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