Abstract

Abstract. Indole is a heterocyclic compound emitted by various plant species under stressed conditions or during flowering events. The formation, optical properties, and chemical composition of secondary organic aerosol (SOA) formed by low-NOx photooxidation of indole were investigated. The SOA yield (1. 3 ± 0. 3) was estimated from measuring the particle mass concentration with a scanning mobility particle sizer (SMPS) and correcting it for wall loss effects. The high value of the SOA mass yield suggests that most oxidized indole products eventually end up in the particle phase. The SOA particles were collected on filters and analysed offline with UV–vis spectrophotometry to measure the mass absorption coefficient (MAC) of the bulk sample. The samples were visibly brown and had MAC values of ∼ 2 m2 g−1 at λ = 300 nm and ∼ 0. 5 m2 g−1 at λ = 400 nm, comparable to strongly absorbing brown carbon emitted from biomass burning. The chemical composition of SOA was examined with several mass spectrometry methods. Direct analysis in real-time mass spectrometry (DART-MS) and nanospray desorption electrospray high-resolution mass spectrometry (nano-DESI-HRMS) were both used to provide information about the overall distribution of SOA compounds. High-performance liquid chromatography, coupled to photodiode array spectrophotometry and high-resolution mass spectrometry (HPLC-PDA-HRMS), was used to identify chromophoric compounds that are responsible for the brown colour of SOA. Indole derivatives, such as tryptanthrin, indirubin, indigo dye, and indoxyl red, were found to contribute significantly to the visible absorption spectrum of indole SOA. The potential effect of indole SOA on air quality was explored with an airshed model, which found elevated concentrations of indole SOA during the afternoon hours contributing considerably to the total organic aerosol under selected scenarios. Because of its high MAC values, indole SOA can contribute to decreased visibility and poor air quality.

Highlights

  • Atmospheric particulate matter (PM) absorbs and scatters solar radiation and is responsible for diminished visibility in urban areas and for global changes in climate

  • We show that indole can measurably contribute to secondary organic aerosol (SOA) loading even in urban environments, where anthropogenic emissions dominate over biogenic ones, such as the South Coast Air Basin of California (SoCAB)

  • The high mass absorption coefficient (MAC) values were due to well-known chromophoric products of indole oxidation, including tryptanthrin, indirubin, indigo dye, and indoxyl red, which were identified by their molecular formulas and characteristic peaks in their absorption spectra

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Summary

Introduction

Atmospheric particulate matter (PM) absorbs and scatters solar radiation and is responsible for diminished visibility in urban areas and for global changes in climate. A key component of PM is secondary organic aerosol (SOA). Discrepancies may result from incorrect or incomplete parameterizations of mechanisms for known SOA precursors, as well as from unaccounted precursors of SOA. Atmospheric researchers have investigated in detail the SOA generated from oxidation of basic anthropogenic and biogenic volatile organic compounds (VOCs), such as isoprene, monoterpenes, saturated hydrocarbons, and aromatic hydrocarbons. Much less is known about SOA from nitrogencontaining VOCs, even though such VOCs are common in the atmospheric environment and can potentially provide significant additional pathways for SOA formation.

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