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Effect of lightning activities on surface atmospheric NO, O3 and submicron particles based on artificially triggered lightning technology: A case study

机译:基于人工触发闪电技术的闪电活动对表面大气No,O3和亚微米粒子的影响 - 以案例研究

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Lightning can cause a variety of atmospheric chemical reactions because of its high temperature and high pressure. Known as a major natural source of atmospheric nitrogen oxides (NOx), lightning can also affect the abundance of ozone (O3) and result in the generation of new particles in the atmosphere. This study explores the effect of lightning activities on surface atmospheric nitric oxide (NO), O3 and submicron particles utilizing artificially triggered lightning experiments. Five lightning flashes were successfully triggered in Guangzhou on 19th August 2014. Concentrations of surface NO, O3 and submicron particles were observed together with lightning and meteorological parameters. Results show that NO concentration increased rapidly from 0.4?ppbv to 220.5?ppbv after a successful upwind artificially triggered lightning flash. Wind direction played an important role in the enhancement of NO concentration at different levels caused by each triggered lightning flash. O3 concentration increased from 15.8?ppbv to 28.7?ppbv before triggering lightning. After the first triggered lightning flash, O3 concentration decreased rapidly to the valley value of 16.9?ppbv because of titration effect. In addition, the number concentration of submicron particles also increased rapidly after successful triggered lightning experiments. The finds resulting from this study give a deeper insight into the impact of lightning on atmospheric chemistry.
机译:由于其高温和高压,闪电可能导致各种大气化学反应。被称为大气氮氧化物(NOx)的主要天然来源,闪电也可以影响臭氧(O3)的丰度并导致在大气中产生新的颗粒。本研究探讨了利用人工触发的闪电实验对表面大气一氧化氮(NO),O3和亚微米颗粒的闪电活动的影响。在2014年8月19日在广州成功触发了五次闪电。与雷电和气象参数一起观察到表面No,O3和亚微米颗粒的浓度。结果表明,在成功的逆风闪电闪现后,没有浓度从0.4〜220.5〜220.5?PPBV。风向在每个触发闪电闪现引起的不同水平的增强中发挥了重要作用。 O3浓度从15.8〜28.7℃增加到28.7℃,在触发闪电前PPBV。在第一触发闪电闪光之后,由于滴定效应,O3浓度迅速降低到16.9的谷值16.9?PPBV。此外,在成功触发闪电实验后,亚微米粒子的数量浓度也在迅速增加。本研究产生的发现深入了解闪电对大气化学的影响。

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