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中国东部不同污染环境中气溶胶吸湿性的差异及其成因OA北大核心CSTPCD

Differences in aerosol hygroscopicity and influencing factors in various polluted environments in eastern China

中文摘要英文摘要

气溶胶吸湿性与其光学性质、活化能力和生命周期等密切相关.本研究基于华北和长三角地区6个典型站点的吸湿性-串联差分电迁移率分析仪观测数据,开展气溶胶吸湿性的对比分析.研究发现华北地区气溶胶吸湿性整体强于长三角地区,不同污染环境下粒子混合状态存在明显差别.人为一次排放产生的大量疏水性物质能够削弱气溶胶吸湿性,增强粒子外混程度;而二次生成过程(如光化学反应)产生的强吸湿性物质能够增强气溶胶吸湿性,同时增强粒子内混程度,造成两个地区不同站点间同一模态气溶胶吸湿性参数存在显著差异.一般情况下,积聚模态粒子吸湿性强于核模态粒子.特别地,受频繁的新粒子生成事件影响,邢台站点的核模态气溶胶也具有较强的吸湿性.以上结果表明,不同污染环境中气溶胶吸湿性存在明显差异,在进行气溶胶吸湿性的模拟实验及研究其对雾霾形成的影响时应注意区分.

Aerosol hygroscopicity is intricately linked to optical properties,activation potential,and lifespan.This study utilizes H-TDMA observational data from six sites across North China(Beijing,Xingtai,and Xinzhou)and the Yangtze River Delta(Baoshan,Dongtan in Shanghai,and Pukou in Nanjing)to investigate aerosol hygro-scopicity characteristics and influencing factors in diverse environments.Urban sites include Beijing and Baoshan(Shanghai),while Xingtai and Pukou(Nanjing)represent suburban areas heavily impacted by human pollution.In contrast,Xinzhou and Dongtan(Shanghai)are less-affected suburban locales.The findings reveal that particle hygroscopicity at North China sites generally exceeds that at Yangtze River Delta sites.Specifically,the average hygroscopicity parameter of 40 nm nucleation mode particles at North China sites is approxiamtely 0.1 higher,and 200 nm accumulation mode particles are about 0.06 higher,representing a 5.6%and 0.1%increase,repec-tively,compared to the same particle sizes at Yangtze River Delta sites.This disparity is attributed to the dense presence of heavy industries in North China,limited atmospheric dispersion,and significant emissions and accu-mulation of gaseous precursors,which foster the formation of highly hygroscopic secondary aerosols,such as sul-fates,under humid conditions.Overall,a significant divergence in aerosol hygroscopicity is observed across differ-ent emission backgrounds,with noticeable differences in hygroscopicity parameters between nucleation mode and accumulation mode particles across various North China sites.Urban site aerosols are heavily influenced by prima-ry emissions and predominantly comprise hydrophobic substances,resulting in weak hygroscopicity and pro-nounced external mixing characteristics.Suburban sites heavily impacted by human pollution exhibit stronger hy-groscopicity due to increased secondary aerosol formation.Conversely,less polluted suburban sites display inter-mediate hygroscopicity with a relatively higher internal mixing of particles.The marked variance in accumulation mode hygroscopicity at Yangtze River Delta sites is primarily attributed to the influence of marine aerosols,dis-tinct from those at North China sites.Excluding Xingtai,particle hygroscopicity generally increases with particle size across other sites,indicating that larger particles typically contain more hygroscopic substances.Frequent new particle formation events at the Xingtai site result in stronger hygroscopicity of nucleation mode particles,with 40 nm particle hygroscopicity values around 0.38,significantly higher than at the other two sites in the same region.Substantial emissions of primary aerosols during morning and evening peak hours generally diminish aerosol hy-groscopicity.Conversely,secondary aerosols generated by daytime photochemical reactions substantially enhance aerosol hygroscopicity,particularly evident at the three North China sites.These findings underscore the distinct differences in aerosol hygroscopicity across varying pollution environments,emphasizing the necessity for differ-entiation in simulations and studies addressing their impact on haze formation.The insights gleaned are of signifi-cant relevance for elucidating the mechanisms of air pollution formation and the radiative effects of aerosols.

崔晨;王玉莹;张睿;吴昊

南京信息工程大学大气物理学院/中国气象局气溶胶-云-降水重点开放实验室,江苏南京 210044南京信息工程大学大气物理学院/中国气象局气溶胶-云-降水重点开放实验室,江苏南京 210044||南京信息工程大学国家综合气象观测专项试验外场,江苏南京 210044成都信息工程大学电子工程学院,四川成都 610225

气溶胶吸湿性H-TDMA外场观测中国东部

aerosolhygroscopicityH-TDMAfield observationeastern China

《大气科学学报》 2024 (004)

592-603 / 12

国家自然科学基金资助项目(42005067;42030606)

10.13878/j.cnki.dqkxxb.20230719001

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