Abstract:Anthropogenic biomass burning is poorly represented in models due to a lack of observational data but represents a significant source of short‐lived toxic gases. Guy Fawkes Night (bonfire night) is a regular UK‐wide event where open fires are lit and fireworks are set off on 5 November. Previous gas phase studies of bonfire night focus on persistent organic pollutants primarily using off‐line techniques. Here the first simultaneous online gas phase measurements of several classes of compounds including isocyan… Show more
“…19 This result is consistent with measurements made during a nationwide bonre event in the UK where HNCO/CO ratios were observed to be 3 times higher during a period when emissions were thought to be dominated by aming combustion compared to smouldering. 58 In addition, this Guy Fawkes Night study found that plumes associated with bonres had maximum mixing ratios of 1.64 ppbv HNCO, a two-order of magnitude enhancement of the mean non-bonre mixing ratio of 0.012 ppbv. 58 Different parameters such as protein content and temperature determine how much HNCO is released during biomass burning.…”
Section: Biomass Burningmentioning
confidence: 91%
“…60 In the Fort Collins and Manchester data sets, there is an early morning minimum with increasing concentrations throughout the day to a late aernoon maximum. 26,58 One hypothesis for the late aernoon peak observed in some datasets is the production of HNCO through secondary photochemical sources. 26 Support for secondary production comes from two lines of evidence.…”
Isocyanic acid (HNCO) has recently been identified in ambient air at potentially concerning concentrations for human health. Since its first atmospheric detection, significant progress has been made in understanding its sources and sinks.
“…19 This result is consistent with measurements made during a nationwide bonre event in the UK where HNCO/CO ratios were observed to be 3 times higher during a period when emissions were thought to be dominated by aming combustion compared to smouldering. 58 In addition, this Guy Fawkes Night study found that plumes associated with bonres had maximum mixing ratios of 1.64 ppbv HNCO, a two-order of magnitude enhancement of the mean non-bonre mixing ratio of 0.012 ppbv. 58 Different parameters such as protein content and temperature determine how much HNCO is released during biomass burning.…”
Section: Biomass Burningmentioning
confidence: 91%
“…60 In the Fort Collins and Manchester data sets, there is an early morning minimum with increasing concentrations throughout the day to a late aernoon maximum. 26,58 One hypothesis for the late aernoon peak observed in some datasets is the production of HNCO through secondary photochemical sources. 26 Support for secondary production comes from two lines of evidence.…”
Isocyanic acid (HNCO) has recently been identified in ambient air at potentially concerning concentrations for human health. Since its first atmospheric detection, significant progress has been made in understanding its sources and sinks.
“…The I-CIMS is sensitive to acids and multifunctional oxygenates (Lee et al, 2014), which are likely to form as secondary NMOGs in biomass burning plumes. I-CIMS has been used to evaluate primary NMOG emissions (e.g., Priestley et al, 2018;Reyes-Villegas et al, 2018;Tomaz et al, 2018), biomass burning emissions aged by nocturnal processes (Ahern et al, 2018;Reyes-Villegas et al, 2018), and primary particle-phase components (Gaston et al, 2016). I-CIMS spectra of the NMOGs resulting from the OH oxidation of biomass burning smoke have yet to be reported.…”
Abstract. Chamber oxidation experiments conducted at the Fire Sciences Laboratory in 2016 are evaluated to identify important chemical processes contributing to the hydroxy radical (OH) chemistry of biomass burning non-methane organic gases (NMOGs). Based on the decay of primary carbon measured by proton transfer reaction time-of-flight mass spectrometry (PTR-ToF-MS), it is confirmed that furans and oxygenated aromatics are among the NMOGs emitted from western United States fuel types with the highest reactivities towards OH. The oxidation processes and formation of secondary NMOG masses measured by PTR-ToF-MS and iodide-clustering time-of-flight chemical ionization mass spectrometry (I-CIMS) is interpreted using a box model employing a modified version of the Master Chemical Mechanism (v. 3.3.1) that includes the OH oxidation of furan, 2-methylfuran, 2,5-dimethylfuran, furfural, 5-methylfurfural, and guaiacol. The model supports the assignment of major PTR-ToF-MS and I-CIMS signals to a series of anhydrides and hydroxy furanones formed primarily through furan chemistry. This mechanism is applied to a Lagrangian box model used previously to model a real biomass burning plume. The customized mechanism reproduces the decay of furans and oxygenated aromatics and the formation of secondary NMOGs, such as maleic anhydride. Based on model simulations conducted with and without furans, it is estimated that furans contributed up to 10 % of ozone and over 90 % of maleic anhydride formed within the first 4 h of oxidation. It is shown that maleic anhydride is present in a biomass burning plume transported over several days, which demonstrates the utility of anhydrides as markers for aged biomass burning plumes.
“…The UoM-CIMS setup has been described elsewhere (Priestley et al, 2018); a Filter Inlet for Gases and AEROsols (FI-GAERO; Lopez-Hilfiker et al, 2014) was additionally used in this study. The gas-phase inlet of UoM-CIMS consisted of 5 m 1/4 ID PFA tubing connected to a fast inlet pump with a total flow rate of 13 SLM from which the ToF-CIMS sub-sampled 2 SLM.…”
Abstract. The heterogeneous hydrolysis of dinitrogen pentoxide (N 2 O 5 ) has a significant impact on both nocturnal particulate nitrate formation and photochemistry on the following day through the photolysis of nitryl chloride (ClNO 2 ), yet these processes in highly polluted urban areas remain poorly understood. Here we present measurements of gas-phase Further analysis indicates that the fast N 2 O 5 loss in the nocturnal boundary layer in urban Beijing is mainly attributed to its indirect loss via NO 3 , for example through the reactions with volatile organic compounds and NO, while the contribution of the heterogeneous uptake of N 2 O 5 is comparably small (7-33 %). High ClNO 2 yields ranging from 0.10 to 0.35 were also observed, which might have important implications for air quality by affecting nitrate and ozone formation.
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