2016
DOI: 10.5194/acp-16-12631-2016
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Photochemical organonitrate formation in wet aerosols

Abstract: Abstract. Water is the most abundant component of atmospheric fine aerosol. However, despite rapid progress, multiphase chemistry involving wet aerosols is still poorly understood. In this work, we report results from smog chamber photooxidation of glyoxal-and OH-containing ammonium sulfate or sulfuric acid particles in the presence of NO x and O 3 at high and low relative humidity. Particles were analyzed using ultra-performance liquid chromatography coupled to quadrupole time-of-flight mass spectrometry (UPL… Show more

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Cited by 30 publications
(31 citation statements)
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“…ON includes a wide variety of nitrogen-containing organic species that can be generally classified into three types, that is, reduced N (e.g., amines), oxidized N (e.g., organic nitrates), and ON from the biological or soil (e.g., humus) (Neff et al, 2002). Up to now, investigated components of particulate ON include amino acids (Zhang & Anastasio, 2003b), alkyl amines (Malloy et al, 2009;Murphy et al, 2007), organic nitrates (Ayres et al, 2015;Lim et al, 2016), nitrogen heterocycles (Ma & Hays, 2008), nitro-aromatics (Crimmins & Baker, 2006;Dimashki et al, 2000), and urea (Shi et al, 2010). ON compounds in the atmosphere have been shown to be important for the formation of particles and secondary organic aerosols (Lee et al, 2016).…”
Section: Introductionmentioning
confidence: 99%
“…ON includes a wide variety of nitrogen-containing organic species that can be generally classified into three types, that is, reduced N (e.g., amines), oxidized N (e.g., organic nitrates), and ON from the biological or soil (e.g., humus) (Neff et al, 2002). Up to now, investigated components of particulate ON include amino acids (Zhang & Anastasio, 2003b), alkyl amines (Malloy et al, 2009;Murphy et al, 2007), organic nitrates (Ayres et al, 2015;Lim et al, 2016), nitrogen heterocycles (Ma & Hays, 2008), nitro-aromatics (Crimmins & Baker, 2006;Dimashki et al, 2000), and urea (Shi et al, 2010). ON compounds in the atmosphere have been shown to be important for the formation of particles and secondary organic aerosols (Lee et al, 2016).…”
Section: Introductionmentioning
confidence: 99%
“…The high correlation of RH with nitrate (r = 0.53; Table 5) implies a role of aqueous chemistry in nitrate aerosol formation in Seoul. A recent thermodynamic model simulation with smog chamber experiments and measurement data reveals that NO x photochemistry under high RH conditions facilitates the hygroscopic growth of aerosols through water and HNO 3 uptake cycles with organonitrate formation in aerosol liquid water (Lim et al, 2016) and thus contributes to the high nitrate proportion to PM 2.5 in Seoul (Fig. 4a).…”
Section: Temporal Evolution Of the Multiday Hazementioning
confidence: 99%
“…Descriptions can be found elsewhere (Lim et al, 2016). In summary, 5 m 3 PTFE smog chamber at Korea Institute of Science and Technology (KIST), Seoul, Korea was used.…”
Section: Chamber Methodsmentioning
confidence: 99%
“…We have conducted smog chamber experiments of photochemistry of wet aerosols containing glyoxal, (NH 4 ) 2 SO 4 (or H 2 SO 4 ,), and H 2 O 2 in the presence of NO x and O 3 at high (> 70 % RH) and low (< 5 % RH) humid conditions (Lim et al, 2016). AS aerosols (the atomized aqueous solution of glyoxal, (NH 4 ) 2 SO 4 , and H 2 O 2 ) or SA aerosols (the atomized aqueous solution of glyoxal, H 2 SO 4 , and H 2 O 2 ) were introduced into a 5 m 3 PTFE smog chamber for photooxidation or dark reactions.…”
Section: Photochemical Aging Of Wet Aerosolsmentioning
confidence: 99%
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