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Aqueous-phase mechanism for secondary organic aerosol formation from isoprene: application to the southeast United States and co-benefit of SO2 emission controls

机译:异戊二烯形成二次有机气溶胶的水相机理:在美国东南部的应用和SO2排放控制的共同效益

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摘要

Isoprene emitted by vegetation is an important precursor of secondary organicaerosol (SOA), but the mechanism and yields are uncertain. Aerosol isprevailingly aqueous under the humid conditions typical of isoprene-emittingregions. Here we develop an aqueous-phase mechanism for isoprene SOAformation coupled to a detailed gas-phase isoprene oxidation scheme. Themechanism is based on aerosol reactive uptake coefficients () forwater-soluble isoprene oxidation products, including sensitivity to aerosolacidity and nucleophile concentrations. We apply this mechanism to simulationof aircraft (SEACRS) and ground-based (SOAS) observations over thesoutheast US in summer 2013 using the GEOS-Chem chemical transport model.Emissions of nitrogen oxides (NO  ≡  NO + NO) overthe southeast US are such that the peroxy radicals produced from isopreneoxidation (ISOPO) react significantly with both NO (high-NOpathway) and HO (low-NO pathway), leading to different suites ofisoprene SOA precursors. We find a mean SOA mass yield of 3.3 % fromisoprene oxidation, consistent with the observed relationship of total fineorganic aerosol (OA) and formaldehyde (a product of isoprene oxidation).Isoprene SOA production is mainly contributed by two immediate gas-phaseprecursors, isoprene epoxydiols (IEPOX, 58 % of isoprene SOA) from thelow-NO pathway and glyoxal (28 %) from both low- and high-NOpathways. This speciation is consistent with observations of IEPOX SOA fromSOAS and SEACRS. Observations show a strong relationship between IEPOXSOA and sulfate aerosol that we explain as due to the effect of sulfate onaerosol acidity and volume. Isoprene SOA concentrations increase as NOemissions decrease (favoring the low-NO pathway for isopreneoxidation), but decrease more strongly as SO emissions decrease (due tothe effect of sulfate on aerosol acidity and volume). The US EnvironmentalProtection Agency (EPA) projects 2013–2025 decreases in anthropogenicemissions of 34 % for NO (leading to a 7 % increase in isopreneSOA) and 48 % for SO (35 % decrease in isoprene SOA). ReducingSO emissions decreases sulfate and isoprene SOA by a similar magnitude,representing a factor of 2 co-benefit for PM from SO emissioncontrols.
机译:植被释放的异戊二烯是次要有机气溶胶(SOA)的重要前体,但其机理和产量尚不确定。气溶胶在异戊二烯发射区典型的潮湿条件下普遍呈水性。在这里,我们开发了一种异戊二烯SOA形成的水相机理,并结合了详细的气相异戊二烯氧化方案。共生机制基于水溶性异戊二烯氧化产物的气溶胶反应性吸收系数(),包括对气溶胶酸度和亲核试剂浓度的敏感性。我们使用GEOS-Chem化学迁移模型将此机制应用于模拟美国东南部地区的飞机(SEACRS)和地面(SOAS)观测,2013年夏季,美国东南部氮氧化物(NO≡NO + NO)的排放使得异戊二烯氧化(ISOPO)产生的过氧自由基会与NO(高NO途径)和HO(低NO途径)发生显着反应,从而导致形成不同的异戊二烯SOA前体套件。我们发现异戊二烯氧化的平均SOA产率为3.3%,与观察到的总细有机气溶胶(OA)和甲醛(异戊二烯氧化的产物)之间的关系一致。异戊二烯SOA的生产主要由两个直接的气相前体异戊二烯环氧二醇贡献(IEPOX,异戊二烯SOA的58%)来自低NO途径,乙二醛(28 %%)来自低NO和高NO途径。这种形态与来自SOAS和SEACRS的IEPOX SOA的观察结果一致。观测结果表明,IEPOXSOA与硫酸盐气溶胶之间存在很强的关系,我们解释这是由于硫酸盐对气溶胶酸度和体积的影响。异戊二烯的SOA浓度随NO排放的减少而增加(有利于异戊二烯氧化的低NO途径),但随着SO排放的减少而更强烈地减少(由于硫酸盐对气溶胶酸度和体积的影响)。美国环境保护总署(EPA)预计,2013-2025年,人为排放的NO减少34%(导致异戊二烯SOA增加7%),SO减少48%(异戊二烯SOA减少35%)。减少SO的排放将硫酸盐和异戊二烯的SOA降低了类似的幅度,这代表了SO排放控制中PM的2倍效益。

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