Atmospheric photooxidation and ozonolysis of sabinene: reaction rate coefficients, product yields, and chemical budget of radicals
-
Published:2023-10-11
Issue:19
Volume:23
Page:12631-12649
-
ISSN:1680-7324
-
Container-title:Atmospheric Chemistry and Physics
-
language:en
-
Short-container-title:Atmos. Chem. Phys.
Author:
Pang Jacky Y. S.ORCID, Berg FlorianORCID, Novelli AnnaORCID, Bohn BirgerORCID, Färber Michelle, Carlsson Philip T. M.ORCID, Dubus René, Gkatzelis Georgios I.ORCID, Rohrer Franz, Wedel Sergej, Wahner AndreasORCID, Fuchs HendrikORCID
Abstract
Abstract. The oxidation of sabinene by the hydroxyl radical (OH)
and ozone (O3) was investigated under atmospherically relevant
conditions in the atmospheric simulation chamber SAPHIR (Simulation of
Atmospheric Photochemistry In a Large Reaction Chamber) at Forschungszentrum
Jülich, Germany. The rate coefficients of the reactions of sabinene with
OH and with O3 were determined. The temperature dependence between 284 to 340 K of the rate coefficient of the reaction of sabinene with OH,
kSAB+OH, was measured for the first time using an OH reactivity
instrument, resulting in an Arrhenius expression of (1.67 ± 0.16) × 10−11 × exp((575 ± 30)/T) cm3 s−1. The values agree with those determined in chamber experiments in
this work and reported in the literature for ∼ 298 K within
the uncertainties of measurements. The ozonolysis reaction rate coefficient
of sabinene (kSAB+O3) determined in chamber experiments at a temperature
of (278 ± 2) K is (3.4 ± 0.8) × 10−17 cm3 s−1, which is 58 % lower than the value reported in the literature
for room temperature. The measurement of products from the oxidation of
sabinene by OH resulted in an acetone yield of (21 ± 15) %, a
formaldehyde yield of (46 ± 25) %, and a sabinaketone yield of
(18 ± 16) %. All yields determined in the chamber experiments agree
well with values from previous laboratory studies within their
uncertainties. In addition, the formaldehyde yield determined in this study
is consistent with that predicted by the sabinene OH-oxidation mechanism
which was devised from quantum chemical calculations by Wang and Wang (2018), whereas the acetone yield is about 15 % higher than that
predicted by the mechanism. In the ozonolysis experiments, the analysis of
product measurements results in an acetone yield of (5 ± 2) %, a
formaldehyde yield of (48 ± 15) %, a sabinaketone yield of
(31 ± 15) %, and an OH radical yield of (26 ± 29) %. The OH
radical yield is lower than expected from the theoretical mechanism in Wang
and Wang (2017), but the value still agrees within the uncertainty. An
analysis of the chemical budget of OH radicals was performed for the chamber
experiments. The analysis reveals that the destruction rate of the OH radical
matches the production rate of OH, suggesting that there is no significant
missing OH source for example from isomerization reactions of peroxy
radicals for the experimental conditions in this work.
Publisher
Copernicus GmbH
Subject
Atmospheric Science
Reference77 articles.
1. Almatarneh, M. H., Elayan, I. A., Altarawneh, M., and Hollett, J. W.: A
computational study of the ozonolysis of sabinene, Theor. Chem. Acc., 138,
30, https://doi.org/10.1007/s00214-019-2420-7, 2019. 2. Alvarado, A., Arey, J., and Atkinson, R.: Kinetics of the Gas-Phase
Reactions of OH and NO3 Radicals and O3 with the Monoterpene Reaction
Products Pinonaldehyde, Caronaldehyde, and Sabinaketone, J. Atmos. Chem.,
31, 281–297, https://doi.org/10.1023/A:1006010915971, 1998. 3. Arey, J., Atkinson, R., and Aschmann, S. M.: Product study of the gas-phase
reactions of monoterpenes with the OH radical in the presence of NO x,
J. Geophys. Res.-Atmos., 95, 18539–18546,
https://doi.org/10.1029/JD095iD11p18539, 1990. 4. Aschmann, S. M., Arey, J., and Atkinson, R.: OH radical formation from the
gas-phase reactions of O3 with a series of terpenes, Atmos. Environ., 36,
4347–4355, https://doi.org/10.1016/S1352-2310(02)00355-2, 2002. 5. Atkinson, R. and Arey, J.: Gas-phase tropospheric chemistry of biogenic
volatile organic compounds: a review, Atmos. Environ., 37, 197–219,
https://doi.org/10.1016/S1352-2310(03)00391-1, 2003.
|
|