Abstract

Abstract. Reactions of the key atmospheric nighttime oxidant NO3 with organic monolayers at the air–water interface are used as proxies for the ageing of organic-coated aqueous aerosols. The surfactant molecules chosen for this study are oleic acid (OA), palmitoleic acid (POA), methyl oleate (MO) and stearic acid (SA) to investigate the effects of chain length, head group and degree of unsaturation on the reaction kinetics and products formed. Fully and partially deuterated surfactants were studied using neutron reflectometry (NR) to determine the reaction kinetics of organic monolayers with NO3 at the air–water interface for the first time. Kinetic modelling allowed us to determine the rate coefficients for the oxidation of OA, POA and MO monolayers to be (2.8±0.7) × 10−8, (2.4±0.5) × 10−8and (3.3±0.6) × 10−8 cm2 molecule−1 s−1 for fitted initial desorption lifetimes of NO3 at the closely packed organic monolayers, τd, NO3, 1, of 8.1±4.0, 16±4.0 and 8.1±3.0 ns, respectively. The approximately doubled desorption lifetime found in the best fit for POA compared to OA and MO is consistent with a more accessible double bond associated with the shorter alkyl chain of POA facilitating initial NO3 attack at the double bond in a closely packed monolayer. The corresponding uptake coefficients for OA, POA and MO were found to be (2.1±0.5) × 10−3, (1.7±0.3) × 10−3 and (2.1±0.4) × 10−3, respectively. For the much slower NO3-initiated oxidation of the saturated surfactant SA we estimated a loss rate of approximately (5±1) × 10−12 cm2 molecule−1 s−1, which we consider to be an upper limit for the reactive loss, and estimated an uptake coefficient of ca. (5±1) × 10−7. Our investigations demonstrate that NO3 will contribute substantially to the processing of unsaturated surfactants at the air–water interface during nighttime given its reactivity is ca. 2 orders of magnitude higher than that of O3. Furthermore, the relative contributions of NO3 and O3 to the oxidative losses vary massively between species that are closely related in structure: NO3 reacts ca. 400 times faster than O3 with the common model surfactant oleic acid, but only ca. 60 times faster with its methyl ester MO. It is therefore necessary to perform a case-by-case assessment of the relative contributions of the different degradation routes for any specific surfactant. The overall impact of NO3 on the fate of saturated surfactants is slightly less clear given the lack of prior kinetic data for comparison, but NO3 is likely to contribute significantly to the loss of saturated species and dominate their loss during nighttime. The retention of the organic character at the air–water interface differs fundamentally between the different surfactant species: the fatty acids studied (OA and POA) form products with a yield of ∼ 20 % that are stable at the interface while NO3-initiated oxidation of the methyl ester MO rapidly and effectively removes the organic character ( ≤ 3 % surface-active products). The film-forming potential of reaction products in real aerosol is thus likely to depend on the relative proportions of saturated and unsaturated surfactants as well as the head group properties. Atmospheric lifetimes of unsaturated species are much longer than those determined with respect to their reactions at the air–water interface, so they must be protected from oxidative attack, for example, by incorporation into a complex aerosol matrix or in mixed surface films with yet unexplored kinetic behaviour.

Highlights

  • Over the last decades, aerosols have attracted increasing attention from the scientific community because their impact on the Earth’s radiative balance and on cloud formation is still largely unknown (Shindell et al, 2009; Stevens et al, 2009; Stocker et al, 2013)

  • Simultaneous neutron reflectometry and infrared reflection–absorption spectroscopy (IRRAS), a technique we have recently developed for study of related systems (Skoda et al, 2017), may be able to give some information on the chemical composition of one-molecule thin films during kinetic studies of oxidation reactions at the air–water interface in the future

  • Our present approach did not allow convenient variation in the surface excess due to the barrierless Langmuir trough in our miniature kinetic chamber optimised for kinetic measurements of fast reactions (Sebastiani et al, 2015), we believe that the best-fit parameters we report in the present study can predict the fate of an organic monolayer with a different compression, i.e. at a different initial surface excess

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Summary

Introduction

Aerosols have attracted increasing attention from the scientific community because their impact on the Earth’s radiative balance and on cloud formation is still largely unknown (Shindell et al, 2009; Stevens et al, 2009; Stocker et al, 2013). The composition and lifetime of aerosol particles in the atmosphere are largely determined by the ageing process due to exposure to trace gases, such as NO3, OH, O3 or other oxidants (e.g. Cl and Br; Estillore et al, 2016). To study the aerosol ageing it is crucial to investigate the heterogeneous reactions occurring between the particles and gas-phase oxidants. Field measurements suggest that heterogeneous reactions may change the chemical composition of particles and in particular of their surface films (Robinson et al, 2006). Most of the studies to date have investigated the heterogeneous reaction of organic aerosols by O3 and OH, which are the main oxidants during daytime. It has been shown that experimental studies of organic molecules self-assembled at the surface of water rather than purely organic aerosols alone are key to understanding atmospheric ageing of aerosols covered in organic material (Vesna et al, 2008)

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