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首页> 外文期刊>Aerosol and Air Quality Research >Particulate Matter, Ozone, and Nitrogen Species in Aged Wildfire Plumes Observed at the Mount Bachelor Observatory
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Particulate Matter, Ozone, and Nitrogen Species in Aged Wildfire Plumes Observed at the Mount Bachelor Observatory

机译:在学士山天文台观测到的老野火羽中的颗粒物,臭氧和氮物质

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During the summer of 2012 and 2013, we measured carbon monoxide (CO), carbon dioxide (CO2), ozone (O3), nitrogen oxides (NOx), reactive nitrogen (NOy), peroxyacetyl nitrate (PAN), aerosol scattering (σsp) and absorption, elemental and organic carbon (EC and OC), and aerosol chemistry at the Mount Bachelor Observatory (2.8 km above sea level, Oregon, US). Here we analyze 23 of the individual plumes from regional wildfires to better understand production and loss of aerosols and gaseous species. We also developed a new method to calculate enhancement ratios and Modified Combustion Efficiency (MCE), which takes into account possible changes in background concentrations during transport. We compared this new method to existing methods for calculating enhancement ratios. The MCE values ranged from 0.79–0.98, ΔO3/ΔCO ranged from 0.01–0.07 ppbv ppbv–1, Δσsp/ΔCO ranged from 0.23–1.32 Mm–1 (at STP) ppbv–1, ΔNOy/ΔCO ranged from 2.89–12.82 pptv ppbv–1, and ΔPAN/ΔCO ranged from 1.46–6.25 pptv ppbv–1. A comparison of three different methods to calculate enhancement ratios (ER) showed that the methods generally resulted in similar Δσsp/ΔCO, ΔNOy/ΔCO, and ΔPAN/ΔCO; however, there was a significant bias between the methods when calculating ΔO3/ΔCO due to the small absolute enhancement of O3 in the plumes. The ΔO3/ΔCO ERs calculated using two common methods were biased low (~20–30%) when compared to the new proposed method. Two pieces of evidence suggest moderate secondary particulate formation in many of the plumes studied: 1) mean observed ΔOC/ΔCO2 was 0.028 g particulate-C gC–1 (as CO2)—27% higher than the midpoint of the biomass burning emission ratio range reported by a recent review—and 2) single scattering albedo (ω) was relatively constant at all MCE values, in contrast with results for fresh plumes. The observed NOx, PAN, and aerosol nitrate represented 6–48%, 25–57%, and 20–69% of the observed NOy in the aged plumes, respectively, and other species represented on average 11% of the observed NOy.
机译:在2012年和2013年夏季,我们测量了一氧化碳(CO),二氧化碳(CO2),臭氧(O3),氮氧化物(NOx),活性氮(NOy),过氧乙酰硝酸盐(PAN),气溶胶散射(σsp)以及学士山天文台(海拔2.8公里,美国俄勒冈)的元素吸收和吸收,元素和有机碳(EC和OC)以及气溶胶化学。在这里,我们分析了区域性野火中的23种单个羽状流,以更好地了解气溶胶和气态物种的产生和损失。我们还开发了一种计算增强比和修正燃烧效率(MCE)的新方法,该方法考虑了运输过程中背景浓度的可能变化。我们将该新方法与现有的计算增强率的方法进行了比较。 MCE值范围为0.79-0.98,ΔO3/ΔCO范围为0.01-0.07 ppbv ppbv-1,Δσsp/ΔCO范围为0.23-1.32 Mm-1(在STP时)ppbv-1,ΔNOy/ΔCO范围为2.89-12.82 pptv ppbv-1和ΔPAN/ΔCO范围为1.46-6.25 pptv ppbv-1。比较三种不同的计算增强比(ER)的方法表明,这些方法通常会产生相似的Δσsp/ΔCO,ΔNOy/ΔCO和ΔPAN/ΔCO。但是,由于羽流中O3的绝对增幅较小,因此在计算ΔO3/ΔCO时,方法之间存在很大偏差。与新提出的方法相比,使用两种常见方法计算出的ΔO3/ΔCOER偏低(〜20–30%)。有两个证据表明,在许多研究的羽流中形成中等程度的二次颗粒:1)观测到的平均ΔOC/ΔCO2为0.028 g颗粒-C gC-1(以CO2计)-比生物质燃烧排放率范围的中点高27%最近的一篇综述报道了这一点;以及2)在所有MCE值下,单散射反照率(ω)相对恒定,这与新鲜羽流的结果相反。在老羽中观察到的NOx,PAN和气溶胶硝酸盐分别占观察到的NOy的6–48%,25–57%和20–69%,其他物种平均占观察到的NOy的11%。

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