Ps. Stevens et al., MEASUREMENT OF TROPOSPHERIC OH AND HO2 BY LASER-INDUCED FLUORESCENCE AT LOW-PRESSURE, JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 99(D2), 1994, pp. 3543-3557
The hydroxyl radical (OH) is the primary oxidant in the atmosphere, re
sponsible for many photochemical reactions that affect both regional a
ir quality and global climate change. Because of its high reactivity,
abundances of OH in the troposphere are less than 1 part per trillion
by volume (pptv) and thus difficult to measure accurately. This paper
describes an instrument for the sensitive detection of OH in the tropo
sphere using low-pressure laser-induced fluorescence. Ambient air is e
xpanded into a low-pressure detection chamber, and OH is both excited
and detected using the A2SIGMA+(v' = 0) --> X2PI(v'' = 0) transition n
ear 308 nm. An injector upstream of the detection axis allows for the
addition of reagent NO to convert ambient HO2 to OH using the fast rea
ction HO2 + NO --> OH + NO2. Using recent advances in laser and detect
or technologies, this prototype instrument is able to detect less than
1 X 10(5) molecules cm-3 (0.004 pptv) of OH with an integration time
of 30 s with negligible interferences.