Year-Round Analysis of Multiphase Sulfate Production in Aerosol Particles in East Asia

Katherine R. Travis*, Benjamin A. Nault, James H. Crawford, Hwajin Kim, Qi Chen, Yan Zheng, Tengyu Liu, Jose L. Jimenez, Pedro Campuzano-Jost, Paul O. Wennberg, John D. Crounse and L. Gregory Huey, 
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Abstract

Missing sulfate production pathways have been implicated as the cause of model underestimates of sulfate during haze events in East Asia. We add multiphase oxidation of SO2 in aerosol particles by H2O2, O3, NO2, HCHO, and O2, catalyzed by transition metal ions (TMIs), to the GEOS-Chem model and evaluate the model with (1) year-round ground-based observations in Seoul, South Korea, (2) airborne observations from the KORUS-AQ field campaign, and (3) fall and winter ground-based observations in Beijing, China. Multiphase chemistry contributes 14% to 90% to total sulfate production depending on the location and season and increases model daily average sulfate by 2 to 3 μg m–3, with maximum daily increases up to 12 μg m–3. From winter to summer, oxidation pathways shift, with the largest fraction of multiphase sulfate production occurring during spring and summer due to oxidation by H2O2. Multiphase oxidation of SO2 by the H2O2 pathway reduces gas-phase H2O2 concentrations by −40% in spring, which improves model agreement with H2O2 airborne observations. Oxidation pathways also shift between cities, in particular the contribution from the TMI and NO2 pathways, which are more important in Beijing than in Seoul. This is due to higher levels of transition metals, and a larger impact of an overly shallow mixed layer in Beijing compared to Seoul. The implementation of multiphase aerosol chemistry in GEOS-Chem here allows for the use of this chemistry in other models that can address boundary layer errors, including WRF-GC and CESM-GC. The analysis presented here shows that this chemistry is important to the simulation of sulfate year-round, not only during haze events, and is unique in showing coupled gas- and aerosol-phase impacts of multiphase chemistry.

Air quality models typically do not include production of sulfate in humidified particulate matter. This study shows the importance of including this process in models to improve understanding of particulate pollution levels year-round.

东亚气溶胶颗粒中多相硫酸盐生成的全年分析
缺失的硫酸盐生成途径被认为是东亚雾霾事件期间模式低估硫酸盐的原因。我们将H2O2、O3、NO2、HCHO和O2在过渡金属离子(tmi)催化下对气溶胶颗粒中SO2的多相氧化添加到GEOS-Chem模型中,并使用(1)韩国首尔全年地面观测数据,(2)KORUS-AQ野外运动的空中观测数据,以及(3)中国北京秋冬地面观测数据对该模型进行评估。多相化学对总硫酸盐产量的贡献为14%至90%,具体取决于地点和季节,并使模型日平均硫酸盐增加2至3 μg m-3,最大日增加可达12 μg m-3。从冬季到夏季,氧化途径发生变化,由于H2O2的氧化作用,春季和夏季多相硫酸盐生成的比例最大。在春季,H2O2途径对SO2的多相氧化使气相H2O2浓度降低了40%,这提高了模型与空气中H2O2观测值的一致性。氧化途径在不同城市之间也会发生变化,特别是TMI和NO2途径的贡献,这在北京比在首尔更重要。这是由于北京的过渡金属含量更高,以及与首尔相比,北京过浅的混合层的影响更大。在GEOS-Chem中实施多相气溶胶化学,允许在其他可以解决边界层误差的模型中使用这种化学,包括WRF-GC和CESM-GC。本文的分析表明,这种化学反应对硫酸盐全年的模拟很重要,而不仅仅是在雾霾事件期间,并且在显示多相化学反应的耦合气相和气溶胶相影响方面是独一无二的。空气质量模型通常不包括湿化颗粒物质中硫酸盐的产生。这项研究表明,将这一过程纳入模型,对于提高对全年颗粒物污染水平的了解非常重要。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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