Characteristics of HONO and its impact on O 3 formation in the Seoul Metropolitan Area during the Korea-US Air Quality Study

• Published in: Atmospheric environment (1994) 2021-02, Vol.247
• Main Authors: Gil, Junsu, Kim, Jeonghwan, Lee, Meehye, Lee, Gangwoong, An, Joonyeong, Lee, Dongsoo, Jung, Jinsang, Cho, Seogju, Whitehill, Andrew, Szykman, James, Lee, Jeonghoon
• Format: Article
• Language: English
• ISSN: 1352-2310
• DOI: 10.1016/j.atmosenv.2020.118182

Photolysis of nitrous acid (HONO) is recognized as an early-morning source of OH radicals in the urban air. During the Korea-US air quality (KORUS-AQ) campaign, HONO was measured using quantum cascade - tunable infrared laser differential absorption spectrometer (QC-TILDAS) at Olympic Park in Seoul from 17 May, 2016 to 14 June, 2016. The HONO concentration was in the range of 0.07-3.46 ppbv, with an average of 0.93 ppbv. Moreover, it remained high from 00:00-05:00 LST. During this time, the mean concentration was higher during the high-O episodes (1.82 ppbv) than the non-episodes (1.20 ppbv). In the morning, the OH radicals that were produced from HONO photolysis were 50% higher (0.95 pptv) during the high-O episodes than the non-episodes. Diurnal variations in HO and O concentrations were simulated by the F0AM model, which revealed a difference of ~20 ppbv in the daily maximum O concentrations between the high-O episodes and non-episodes. Furthermore, the HONO concentration increased with an increase in relative humidity (RH) up to 80%; the highest HONO was associated with the top 10% NO in each RH group, confirming that NO is one of the main precursors of HONO. At night, the conversion ratio of NO to HONO was estimated to be 0.88×10 h ; this ratio was found to increase with an increase in RH. The Aitken mode particles (30-120 nm), which act as catalyst surfaces, exhibited a similar tendency with a conversion ratio that increased along with RH, indicating the coupling of surfaces with HONO conversion. Using an artificial neural network (ANN) model, HONO concentrations were successfully simulated with measured variables (r = 0.66 as an average of five models). Among these variables, NO , aerosol surface area, and RH were found to be the main factors affecting the ambient HONO concentrations. The results reveal that RH facilitates the conversion of NO to HONO by constraining the availability of aerosol surfaces. This study demonstrates the coupling of HONO with the HO -O cycle in the Seoul Metropolitan Area (SMA) and provides practical evidence of the heterogeneous formation of HONO by employing the ANN model.