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Title: Enhanced photodegradation of dimethoxybenzene isomers in/on ice compared to in aqueous solution
Abstract. Photochemical reactions of contaminants in snow and ice can be importantsinks for organic and inorganic compounds deposited onto snow from theatmosphere and sources for photoproducts released from snowpacks into theatmosphere. Snow contaminants can be found in the bulk ice matrix, ininternal liquid-like regions (LLRs), or in quasi-liquid layers (QLLs) at theair–ice interface, where they can readily exchange with the firn air. Somestudies have reported that direct photochemical reactions occur faster inLLRs and QLLs than in aqueous solution, while others have found similarrates. Here, we measure the photodegradation rate constants for loss of thethree dimethoxybenzene isomers under varying experimental conditions,including in aqueous solution, in LLRs, and at the air–ice interface ofnature-identical snow. Relative to aqueous solution, we find modestphotodegradation enhancements (3- and 6-fold) in LLRs for two of theisomers and larger enhancements (15- to 30-fold) at the air–ice interfacefor all three isomers. We use computational modeling to assess the impact oflight absorbance changes on photodegradation rate enhancements at theinterface. We find small (2–5 nm) bathochromic (red) absorbance shifts atthe interface relative to in solution, which increases light absorption, butthis factor only accounts for less than 50 % of the measured rate constantenhancements. The major factor responsible for photodegradation rateenhancements at the air–ice interface appears to be more efficientphotodecay: estimated dimethoxybenzene quantum yields are 6- to 24-foldlarger at the interface compared to in aqueous solution and account for themajority (51 %–96 %) of the observed enhancements. Using a hypotheticalmodel compound with an assumed Gaussian-shaped absorbance peak, we find thata shift in the peak to higher or lower wavelengths can have a minor tosubstantial impact on photodecay rate constants, depending on the originallocation of the peak and the magnitude of the shift. Changes in other peakproperties at the air–ice interface, such as peak width and height (i.e.,molar absorption coefficient), can also impact rates of light absorption anddirect photodecay. Our results suggest our current understanding ofphotodegradation processes underestimates the rate at which some compoundsare broken down, as well as the release of photoproducts into theatmosphere.  more » « less
Award ID(s):
1806210
PAR ID:
10328576
Author(s) / Creator(s):
; ; ; ; ; ;
Date Published:
Journal Name:
Atmospheric Chemistry and Physics
Volume:
22
Issue:
9
ISSN:
1680-7324
Page Range / eLocation ID:
5943 to 5959
Format(s):
Medium: X
Sponsoring Org:
National Science Foundation
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