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Novel Analysis to Quantify Plume Crosswind Heterogeneity Applied to Biomass Burning Smoke
Environmental Science & Technology ( IF 11.4 ) Pub Date : 2021-11-24 , DOI: 10.1021/acs.est.1c03803
Zachary C J Decker 1, 2, 3 , Siyuan Wang 1, 2 , Ilann Bourgeois 1, 2 , Pedro Campuzano Jost 2, 3 , Matthew M Coggon 1, 2 , Joshua P DiGangi 4 , Glenn S Diskin 4 , Frank M Flocke 5 , Alessandro Franchin 1, 2, 5 , Carley D Fredrickson 6 , Georgios I Gkatzelis 1, 2 , Samuel R Hall 5 , Hannah Halliday 5 , Katherine Hayden 7 , Christopher D Holmes 8 , L Gregory Huey 9 , Jose L Jimenez 2, 3 , Young Ro Lee 9 , Jakob Lindaas 10 , Ann M Middlebrook 1 , Denise D Montzka 5 , J Andrew Neuman 1, 2 , John B Nowak 11 , Demetrios Pagonis 2, 3 , Brett B Palm 6 , Jeff Peischl 1, 2 , Felix Piel 12, 13 , Pamela S Rickly 1, 2 , Michael A Robinson 1, 2, 3 , Andrew W Rollins 1 , Thomas B Ryerson 1 , Kanako Sekimoto 14 , Joel A Thornton 6 , Geoff S Tyndall 5 , Kirk Ullmann 5 , Patrick R Veres 1 , Carsten Warneke 1, 2 , Rebecca A Washenfelder 1 , Andrew J Weinheimer 5 , Armin Wisthaler 12, 13 , Caroline Womack 1, 2 , Steven S Brown 1, 3
Affiliation  

We present a novel method, the Gaussian observational model for edge to center heterogeneity (GOMECH), to quantify the horizontal chemical structure of plumes. GOMECH fits observations of short-lived emissions or products against a long-lived tracer (e.g., CO) to provide relative metrics for the plume width (wi/wCO) and center (bi/wCO). To validate GOMECH, we investigate OH and NO3 oxidation processes in smoke plumes sampled during FIREX-AQ (Fire Influence on Regional to Global Environments and Air Quality, a 2019 wildfire smoke study). An analysis of 430 crosswind transects demonstrates that nitrous acid (HONO), a primary source of OH, is narrower than CO (wHONO/wCO = 0.73–0.84 ± 0.01) and maleic anhydride (an OH oxidation product) is enhanced on plume edges (wmaleicanhydride/wCO = 1.06–1.12 ± 0.01). By contrast, NO3 production [P(NO3)] occurs mainly at the plume center (wP(NO3)/wCO = 0.91–1.00 ± 0.01). Phenolic emissions, highly reactive to OH and NO3, are narrower than CO (wphenol/wCO = 0.96 ± 0.03, wcatechol/wCO = 0.91 ± 0.01, and wmethylcatechol/wCO = 0.84 ± 0.01), suggesting that plume edge phenolic losses are the greatest. Yet, nitrophenolic aerosol, their oxidation product, is the greatest at the plume center (wnitrophenolicaerosol/wCO = 0.95 ± 0.02). In a large plume case study, GOMECH suggests that nitrocatechol aerosol is most associated with P(NO3). Last, we corroborate GOMECH with a large eddy simulation model which suggests most (55%) of nitrocatechol is produced through NO3 in our case study.

中文翻译:

应用于生物质燃烧烟雾的羽状侧风异质性量化新分析

我们提出了一种新方法,即边缘到中心异质性的高斯观测模型 (GOMECH),以量化羽流的水平化学结构。GOMECH 将短期排放或产品的观察结果与长寿命示踪剂(例如 CO)进行拟合,以提供羽流宽度 ( w i / w CO ) 和中心 ( b i / w CO ) 的相关指标。为了验证 GOMECH,我们调查了 OH 和 NO 3在 FIREX-AQ(火灾对区域到全球环境和空气质量的影响,2019 年野火烟雾研究)期间采样的烟羽中的氧化过程。对 430 个侧风断面的分析表明,作为 OH 的主要来源亚硝酸 (HONO) 比 CO 窄 ( w HONO / w CO = 0.73–0.84 ± 0.01) 并且马来酸酐(一种 OH 氧化产物)在羽流中得到增强边缘(w马来酸酐/ w CO = 1.06–1.12 ± 0.01)。相比之下,NO 3 的产生 [P(NO 3 )] 主要发生在羽流中心 ( w P(NO 3 ) / w CO= 0.91–1.00 ± 0.01)。酚醛排放,OH和NO高度反应性的3,是窄于CO(瓦特苯酚/瓦特CO = 0.96±0.03,瓦特儿茶酚/瓦特CO = 0.91±0.01,和瓦特甲基儿茶酚/瓦特CO = 0.84±0.01),这表明羽流边缘酚类损失最大。然而,它们的氧化产物硝基酚气溶胶在羽流中心最大(w nitrophenolicaerosol / w CO = 0.95 ± 0.02)。在大型羽流案例研究中,GOMECH 表明硝基儿茶酚气溶胶与 P(NO 3)。最后,我们使用大型涡流模拟模型证实了 GOMECH,该模型表明在我们的案例研究中,大部分 (55%) 硝基儿茶酚是通过 NO 3产生的。
更新日期:2021-12-07
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