2014
DOI: 10.1039/c3cp54859g
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Atmospheric aqueous phase radical chemistry of the isoprene oxidation products methacrolein, methyl vinyl ketone, methacrylic acid and acrylic acid – kinetics and product studies

Abstract: Kinetic and mechanistic studies were conducted on the isoprene oxidation products methacrolein, methyl vinyl ketone, methacrylic and acrylic acid reacting with hydroxyl and nitrate radicals and sulfate radical anions in aqueous solution by use of the laser flash photolysis technique and a reversed-rate method for kinetics. High-performance liquid chromatography/mass spectrometry was applied for product analysis. The kinetic investigations show the highest reactivity of the hydroxyl radical followed by sulfate … Show more

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Cited by 65 publications
(71 citation statements)
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“…One hour after the start of aqueous phase chemistry, O / C in the aqueous phase has remained around 1.0 and n C has decreased to 2.8 after a sharp initial increase to 2.9, thus showing that fragmentation is a major process. This result is in good agreement with other aqueous phase studies (Brégonzio-Rozier et al, 2016;Epstein and Nizkorodov, 2012;Epstein et al, 2013) and other models (Schrödner et al, 2014), but is in disagreement with field studies, probably due to a lack of descriptions of high molecular weight substances, and of their reactivity, as well as oligomerization processes. The higher O / C ratios obtained by Schrödner et al (2014) after the cloud event (1.8 for their rural case) can be due to important oxalic acid concentrations dissolved into the aqueous phase in their model, when the cloud is being formed.…”
Section: Gas Chemical Reactivitysupporting
confidence: 68%
“…One hour after the start of aqueous phase chemistry, O / C in the aqueous phase has remained around 1.0 and n C has decreased to 2.8 after a sharp initial increase to 2.9, thus showing that fragmentation is a major process. This result is in good agreement with other aqueous phase studies (Brégonzio-Rozier et al, 2016;Epstein and Nizkorodov, 2012;Epstein et al, 2013) and other models (Schrödner et al, 2014), but is in disagreement with field studies, probably due to a lack of descriptions of high molecular weight substances, and of their reactivity, as well as oligomerization processes. The higher O / C ratios obtained by Schrödner et al (2014) after the cloud event (1.8 for their rural case) can be due to important oxalic acid concentrations dissolved into the aqueous phase in their model, when the cloud is being formed.…”
Section: Gas Chemical Reactivitysupporting
confidence: 68%
“…The photooxidation of isoprene could produce isoprene epoxydiols (IEPOX C 5 H 10 O 3 ), methacrylic acid epoxide (MAE C 4 H 6 O 3 ) or hydroxymethyl‐methyl‐α‐lactone (HMML C 4 H 6 O 3 ), and MVK (C 4 H 6 O) or MACR (C 4 H 6 O) (Schoene et al, 2014; Worton et al, 2013). Among these oxidation products, IEPOX and MAE/HMML have been identified as two key gas‐phase intermediates to isoprene‐derived OSs formation under low‐NO x (i.e., hydroperoxyl (HO 2 ) channel) and high‐NO x (i.e., nitrogen oxides (NO/NO 2 ) channel) conditions, respectively (Lin et al, 2013; Paulot et al, 2009).…”
Section: Resultsmentioning
confidence: 99%
“…The predicted final isoprene mixing ratios account for losses due to gas‐phase reactions with simulated NO 3 , O 3 , and OH along the cyan trajectory. The model does not include aqueous‐phase chemistry of isoprene oxidation products with NO 3 radical (Schöne et al, 2014). Figure 14 shows the estimated SOA mass yields range from 0 to 0.55 as a function of newly formed SOA mass, calculated by dividing the observed SOA masses by the corresponding modeled amounts of isoprene mass reacted with NO 3 .…”
Section: Resultsmentioning
confidence: 99%