高级检索

北京春季高HONO事件源汇机制及其对臭氧生成敏感性研究

Budget analysis of high nitrous acid (HONO) events and its role on ozone formation during springtime of Beijing

  • 摘要: 气态亚硝酸(HONO)的源汇机制是当前大气化学研究中的难点和热点问题之一。本文于2021年春季对北京城区大气HONO及相关污染物进行了在线观测,并针对观测期间高HONO事件的源汇过程及其对O3生成的影响开展了模拟研究。结果显示:观测期间HONO的平均浓度为2.55±1.34ppb,出现两次高HONO事件(连续两天HONO小时浓度最高值大于4ppb)并伴随着较高PM2.5和O3浓度。基于光化学箱模型(F0AM)和观测数据,在详尽化学机制(MCM3.3.1)的基础上耦合更新的非均相化学机制探索了HONO 的主要来源和形成途径,结果表明昼间HONO的主要来源为硝酸盐的光解、NO与OH均相反应和NO2在气溶胶表面光增强非均相反应,其平均生成速率(贡献比例)分别为2.70(55.8%)、0.53(10.8%)和0.05(10.6%)ppb h-1;夜间非均相反应贡献逐渐升高,包括NO2在地表面和气溶胶表面的非均相反应以及与NH3增强气溶胶表面NO2摄取相关的非均相反应,其平均生成速率(贡献比例)分别为0.07(41.3%)、0.03(20.3%)和0.03(20.0%)ppb h-1;同时HONO昼间的汇以HONO光解为主,夜间则主要通过干沉降清除。进一步的模拟分析发现HONO新机制添加前后O3的生消速率显著提高,并且发现其生成敏感性由VOCs控制区向VOCs和NOX协同控制区转变。高浓度HONO及其源汇过程不仅可以促进O3的生成,并且通过影响O3前体物浓度改变O3的生成敏感性。因此,对于北京春季臭氧污染的防治应正确认识HONO化学对臭氧生成的反馈机制。

     

    Abstract: The budget analysis of nitrous acid (HONO) is one of the challenging and hot topics in atmospheric chemistry research. This study conducted observations of HONO and related pollutants in urban Beijing during the spring of 2021. A simulation study was carried out to investigate the source and loss processes of high HONO events and their impact on O3 formation during the observation period. The results showed that the average concentration of HONO during the observation period was 2.55 ± 1.34 ppb, with two high HONO events (defined as the hourly maximum concentration of HONO exceeded 4 ppb for two consecutive days) accompanied by high PM2.5 and O3 concentrations. Based on the photochemical box model (F0AM) and observational data, the main sources and formation pathways of HONO were explored by coupling an updated heterogeneous chemical mechanism on the basis of a chemical mechanism (MCM3.3.1). The results indicated that the main daytime sources of HONO were photolysis of nitrates, the homogeneous reaction between NO and OH, and the photochemically enhanced heterogeneous reaction of NO2 on aerosol surfaces, with average formation rates (contribution ratios) of 2.70(55.8%), 0.53(10.8%), and 0.05(10.6%) ppb h-1, respectively. During nighttime, the contribution of heterogeneous reactions gradually increased, including the heterogeneous reactions of NO2 on the ground surfaces and aerosol surfaces, as well as heterogeneous reactions related to the enhanced aerosol surface uptake of NO2 with NH3, with average formation rates (contribution ratios) of 0.07(41.3%), 0.03(20.3%), and 0.03(20.0%) ppb h-1. The primary removal pathway for HONO during the day was photolysis, while dry deposition was dominant at night. Further simulation analyses revealed that the incorporation of the new HONO mechanism significantly enhanced both the formation and loss rates of ozone (O3). The sensitivity of O3 generation was observed to transition from a VOC-dominated regime to a synergistic control regime involving both VOCs and NOx. Elevated HONO concentrations and their source-sink processes were found to not only accelerate O3 production but also modify its generation sensitivity through dynamic regulation of O3 precursor concentrations (VOCs/NOx). Therefore, for the prevention and control of springtime ozone pollution in Beijing, it is crucial to correctly understand the feedback mechanism of HONO chemistry on ozone formation.

     

/

返回文章
返回