Abstract

Existing studies suggest various potential daytime sources of atmospheric nitrous acid (HONO), including photolysis surface reactions and photo-enhanced NO2 conversion on organic surfaces. However, the understanding of daytime HONO sources is still inadequate. In this study, we report the HONO formation on asphalt surfaces under various NO2, VOCs (toluene and hexane), and UV irradiance conditions using a continuous flow chamber. Although no HONO formation was found without light exposure, the light threshold for HONO formation on the asphalt surface was very low, with a total UV (TUV) of 0.7 W m−2. HONO formation on the asphalt surface was linearly dependent on NO2 up to 300 ppb in the presence of VOCs, but no HONO formation was observed with humified air and NO2. HONO production was saturated at high hydrocarbon concentrations and light intensities. The calculated first-order NO2 conversion rate to HONO on the asphalt surface was 1.2 × 10−4 s −1. The observed mean HONO emission flux was 1.3 × 109 molecules cm−2 s −1 with a similar range of those on other urban covered surfaces. The calculated vertical HONO profile using the measured HONO emission flux and 1-D steady state model revealed that the asphalt surface may account for 13% of daytime HONO in the elevated on-road pollutant concentrations in Seoul. However, we show that its HONO contribution could be much higher on real-life road surfaces directly exposed to much higher NO2 emissions from vehicle exhaust.

Highlights

  • Photolysis of nitrous acid (HONO) is a primary daytime source of hydroxyl radicals (OH), which are dominant atmospheric oxidants and play a significant role in the formation of ozone and secondary organic aerosol (SOA) [1,2]

  • The observed daytime levels were unusually high, from a few hundred ppt to a few ppb, especially in China [3,4,5,6]. These results indicate that unknown dominant daytime sources of HONO, which quantitively correspond to or exceed the photolysis rate of HONO and other loss mechanisms, are yet to be defined

  • HONO formation on the asphalt surface was linearly dependent on NO2 up to 300 ppbv

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Summary

Introduction

Photolysis of nitrous acid (HONO) is a primary daytime source of hydroxyl radicals (OH), which are dominant atmospheric oxidants and play a significant role in the formation of ozone and secondary organic aerosol (SOA) [1,2]. The observed daytime levels were unusually high, from a few hundred ppt to a few ppb, especially in China [3,4,5,6]. These results indicate that unknown dominant daytime sources of HONO, which quantitively correspond to or exceed the photolysis rate of HONO and other loss mechanisms, are yet to be defined. The NO2 dependence of heterogeneous HONO production has been well studied along with various potential formation paths, such as the reaction of NO2 with water (R1) or chemisorbed water via secondary heterogeneous conversion (R2), as well as excited NO2 * from adsorbed

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