State Key Joint Laboratory of Environment Simulation and Pollution Control, School of Environment, State Environmental Protection Key Laboratory of Sources and Control of Air Pollution Complex, Beijing Key Laboratory of Indoor Air Quality Evaluation and Control, Tsinghua University, Beijing 100084, China.
State Key Joint Laboratory of Environment Simulation and Pollution Control, School of Environment, State Environmental Protection Key Laboratory of Sources and Control of Air Pollution Complex, Beijing Key Laboratory of Indoor Air Quality Evaluation and Control, Tsinghua University, Beijing 100084, China.
Environ Pollut. 2018 Nov;242(Pt A):544-554. doi: 10.1016/j.envpol.2018.07.001. Epub 2018 Jul 6.
Continuous haze monitoring was conducted from 12:00 3 April to 12:00 8 April 2016 in Beijing, China to develop a more detailed understanding of spring haze characteristics. The PM concentration ranged from 6.30 to 165 μg m with an average of 63.8 μg m. Nitrate was the most abundant species, accounting for 36.4% of PM, followed by organic carbon (21.5%), NH (19.3%), SO (18.8%), and elemental carbon (4.10%), indicating the key role of nitrate in this haze event. Species contribution varied based on the phase of the haze event. For example, sulfate concentration was high during the haze formation phase, nitrate was high during the haze, and secondary organic carbon (SOC) had the highest contribution during the scavenging phase. The secondary transition of sulfate was influenced by SO, followed by relative humidity (RH) and O (O+NO). Nitrate formation occurred in two stages: through NO oxidation, which was vulnerable to O; and by the partitioning of N (+5) which was susceptible to RH and temperature. SOC tended to form when O and RH were balanced. According to hourly species behavior, sulfate and nitrate were enriched during haze formation when the mixed layer height decreased. However, SOC accumulated prior to the haze event and during formation, which demonstrated the strong contribution of secondary inorganic aerosols, and the limiting contribution of SOC to this haze case. Investigating backward trajectories showed that high speed northwestern air masses following a straight path corresponded to the clear periods, while southwesterly air masses which traversed heavily polluted regions brought abundant pollutants to Beijing and stimulated the occurrence of haze pollution. Results indicate that the control of NO needs to be addressed to reduce spring haze. Finally, the correlation between air mass trajectories and pollution conditions in Beijing reinforce the necessity of inter-regional cooperation and control.
从 2016 年 4 月 3 日 12 时到 4 月 8 日 12 时,在中国北京进行了持续的霾监测,以更详细地了解春季霾的特征。PM 浓度范围为 6.30 至 165μg/m³,平均值为 63.8μg/m³。硝酸盐是最丰富的物质,占 PM 的 36.4%,其次是有机碳(21.5%)、NH(19.3%)、SO(18.8%)和元素碳(4.10%),表明硝酸盐在此次霾事件中起关键作用。根据霾事件的阶段,物种的贡献会有所不同。例如,在霾形成阶段,硫酸盐浓度较高,在霾阶段,硝酸盐浓度较高,在清除阶段,二次有机碳(SOC)的贡献最高。硫酸盐的二次转化受 SO 的影响,其次是相对湿度(RH)和 O(O+NO)。硝酸盐的形成分两个阶段:通过 NO 氧化,NO 氧化易受 O 影响;通过 N(+5)的分配,N(+5)易受 RH 和温度影响。当 O 和 RH 平衡时,SOC 易于形成。根据每小时的物种行为,硫酸盐和硝酸盐在混合层高度降低时在霾形成过程中富集。然而,SOC 在霾事件之前和形成过程中积累,这表明二次无机气溶胶的贡献很大,而 SOC 对这次霾事件的贡献有限。后向轨迹分析表明,高速西北气流沿直线运动对应于晴朗期,而西南气流穿越污染严重的地区,将大量污染物输送到北京,并刺激霾污染的发生。结果表明,需要控制 NO 以减少春季霾。最后,空气团轨迹与北京污染状况之间的相关性加强了区域间合作和控制的必要性。