Elucidating the effect of HONO on O3 pollution by a case study in southwest China

• Published in: The Science of the total environment 2021-02, Vol.756, p.144127, Article 144127
• Main Authors: Yang, Yiming, Li, Xin, Zu, Kexin, Lian, Chaofan, Chen, Shiyi, Dong, Huabin, Feng, Miao, Liu, Hefan, Liu, Jingwei, Lu, Keding, Lu, Sihua, Ma, Xuefei, Song, Danlin, Wang, Weigang, Yang, Suding, Yang, Xinping, Yu, Xuena, Zhu, Yuan, Zeng, Limin, Tan, Qinwen, Zhang, Yuanhang
• Format: Article
• Language: English
• Subjects: Air quality; HONO; NO2 conversion; O3 pollution; Southwest China
• ISSN: 0048-9697
• DOI: 10.1016/j.scitotenv.2020.144127

Photolysis of nitrous acid (HONO) is one of the major sources for atmospheric hydroxyl radicals (OH), playing significant role in initiating tropospheric photochemical reactions for ozone (O3) production. However, scarce field investigations were conducted to elucidate this effect. In this study, a field campaign was conducted at a suburban site in southwest China. The whole observation was classified into three periods based on O3 levels and data coverage: the serious O3 pollution period (Aug 13–18 as P1), the O3 pollution period (Aug 22–28 as P2) and the clean period (Sep 3–12 as P3), with average O3 peak values of 96 ppb, 82 ppb and 44 ppb, respectively. There was no significant difference of the levels of O3 precursors (VOCs and NOx) between P1 and P2, and thus the evident elevation of OH peak values in P1 was suspected to be the most possible explanation for the higher O3 peak values. Considering the larger contribution of HONO photolysis to HOX primary production than photolysis of HCHO, O3 and ozonolysis of Alkenes, sensitivity tests of HONO reduction on O3 production rate in P1 are conducted by a 0-dimension model. Reduced HONO concentration effectively slows the O3 production in the morning, and such effect correlates with the calculated production rate of OH radicals from HONO photolysis. Higher HONO level supplying for OH radical initiation in the early morning might be the main reason for the higher O3 peak values in P1, which explained the correlation (R2 = 0.51) between average O3 value during daytime (10:00–19:00 LT) and average HONO value during early morning (00:00–05:00 LT). For nighttime accumulation, a suitable range of relative humidity that favored NO2 conversion within P1 was assumed to be the reason for the higher HONO concentration in the following early morning which promoted O3 peak values. This figure shows the effect of HONO on OH and O3 production (PO3) during the campaign in Xinjin, China. [Display omitted] •Higher HONO concentration coexisted with higher O3 level.•HONO photolysis contributed up to 60% of HOX primary production in the morning.•Reduction on HONO significantly slows morning O3 production in box model.•Nighttime RH favoring NO2 to HONO conversion might promote daytime O3 production.