Department of Mechanical Engineering, Indian Institute of Technology (BHU), Varanasi, India.
Institute of Environment and Sustainable Development, Banaras Hindu University, Varanasi, 221005, India.
Environ Monit Assess. 2019 Aug 19;191(9):576. doi: 10.1007/s10661-019-7735-2.
Evolution of submicron particles in terms of particle number concentration and mobility-equivalent diameter was measured during Diwali festival-specific intensive pyrotechnic displays in Varanasi over central Indo-Gangetic Plain (IGP). A scanning mobility particle sizer coupled with an optical particle sizer was used to fit in an overlapping size range, and particle number concentration was analyzed to have an insight into the new particle formation and subsequent evolution of particles from nucleation to accumulation mode. Further, variation in black carbon (BC) concentration and aerosol ionic composition was measured simultaneously. Frequent fluctuation in particle number concentration in and around Diwali festival was evidenced, primarily influenced by local emission sources and meteorology, with three distinct peaks in number concentrations (dN/dlogD, 3.1-4.5 × 10 cm) coinciding well with peak firework emission period (18:00-23:00 h). Submicron particle size distribution revealed a single peak covering a size range of 80-130 nm, and for all instances, number concentration maximum coincided with geometric mean minimum, indicating the emission primarily in the ultrafine range (< 0.1 μm). Interestingly, during peak firework emissions, besides rise in accumulation mode, an event of new particle formation was identified with increase in nucleation and small Aitken mode, before being dispersed to background aerosols. On an integral scale, a clear distinction was noted between a normal and an episodic event, with a definite shift in the formation of ultrafine particles compared with the accumulation mode. The BC diurnal profile was typical, with a prominent nocturnal peak (12.0 ± 3.9 μg m) corresponding to a decrease in the boundary layer height. A slight variation in maximum BC concentration (16.8 μg m) was noted in the night of the event coinciding well with firework emissions. An increase in some specific ionic species was also noted in combination with an increase in the overall cation to anion ratio, which was explained in terms of heterogeneous transformation of NOx and catalytic conversion of SO. Graphical abstract Time-resolved evolution of particle size distribution during normal and episodic events.
在印度恒河平原中部的瓦拉纳西,针对排灯节特定的密集烟花表演,我们测量了亚微米颗粒在粒子数浓度和迁移率等效直径方面的演变。我们使用扫描迁移率颗粒粒径仪和光学颗粒粒径仪来拟合重叠的粒径范围,并分析粒子数浓度,以便深入了解新粒子的形成以及随后从成核到积聚态的粒子演变。此外,我们还同时测量了黑碳(BC)浓度和气溶胶离子成分的变化。结果表明,排灯节期间及前后,粒子数浓度频繁波动,主要受当地排放源和气象条件的影响,数浓度出现了三个明显峰值(dN/dlogD,3.1-4.5×10^4cm^-3),与烟花燃放高峰期(18:00-23:00 小时)吻合较好。亚微米颗粒粒径分布呈现出一个单一的峰值,涵盖了 80-130nm 的粒径范围,在所有情况下,数浓度最大值都与几何平均值最小值重合,表明排放主要集中在超细范围(<0.1μm)。有趣的是,在烟花燃放高峰期,除了积聚模态的增加,还发现了新粒子形成事件,伴随着成核和小艾肯模态的增加,然后被分散到背景气溶胶中。在整体尺度上,正常事件和突发事件之间有明显的区别,与积聚模态相比,超细颗粒的形成有明显的转变。BC 的日变化曲线呈典型特征,夜间峰值(12.0±3.9μg/m^3)明显,边界层高度降低。在事件发生的当晚,BC 浓度的最大值(16.8μg/m^3)略有变化,与烟花燃放情况相吻合。同时,一些特定离子种类的浓度也有所增加,与总阳离子与阴离子比值的增加相一致,这可以用 NOx 的非均相转化和 SO 的催化转化来解释。