Comparison of temperature-dependent calibration methods of an instrument to measure OH and HO2 radicals using laser-induced fluorescence spectroscopy
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Published:2023-10-05
Issue:19
Volume:16
Page:4375-4390
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ISSN:1867-8548
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Container-title:Atmospheric Measurement Techniques
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language:en
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Short-container-title:Atmos. Meas. Tech.
Author:
Winiberg Frank A. F., Warman William J., Brumby Charlotte A., Boustead Graham, Bejan Iustinian G.ORCID, Speak Thomas H., Heard Dwayne E.ORCID, Stone DanielORCID, Seakins Paul W.ORCID
Abstract
Abstract. Laser-induced fluorescence (LIF) spectroscopy has been widely applied to
fieldwork measurements of OH radicals and HO2, following conversion
to OH, over a wide variety of conditions, on different platforms and in
simulation chambers. Conventional calibration of HOx (OH + HO2)
instruments has mainly relied on a single method, generating known
concentrations of HOx from H2O vapour photolysis in a flow of zero
air impinging just outside the sample inlet (SHOx=CHOx. [HOx],
where SHOx is the observed signal and CHOx is the calibration
factor). The fluorescence assay by gaseous expansion (FAGE) apparatus
designed for HOx measurements in the Highly Instrumented Reactor for
Atmospheric Chemistry (HIRAC) at the University of Leeds has been used to
examine the sensitivity of FAGE to external gas temperatures (266–348 K). The conventional calibration methods give the temperature dependence of
COH (relative to the value at 293 K) of (0.0059±0.0015) K−1
and CHO2 of (0.014±0.013) K−1. Errors are 2σ.
COH was also determined by observing the decay of hydrocarbons
(typically cyclohexane) caused by OH reactions giving COH (again,
relative to the value at 293 K) of (0.0038±0.0007) K−1.
Additionally, CHO2 was determined based on the second-order kinetics of
HO2 recombination with the temperature dependence of CHO2, relative
to 293 K being (0.0064±0.0034) K−1. The temperature dependence of CHOx depends on the HOx number density,
quenching, the relative population of the probed OH rotational level and HOx
transmission from the inlet to the detection axis. The first three terms can be
calculated and, in combination with the measured values of CHOx, show
that HOx transmission increases with temperature. Comparisons with other
instruments and the implications of this work are discussed.
Funder
Marie Curie Natural Environment Research Council
Publisher
Copernicus GmbH
Subject
Atmospheric Science
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