001     62344
005     20240712101029.0
024 7 _ |a pmid:19044365
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024 7 _ |a 10.1063/1.2968712
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024 7 _ |a WOS:000259374500036
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024 7 _ |a 2128/16761
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037 _ _ |a PreJuSER-62344
041 _ _ |a eng
082 _ _ |a 530
084 _ _ |2 WoS
|a Instruments & Instrumentation
084 _ _ |2 WoS
|a Physics, Applied
100 1 _ |a Fuchs, H.
|b 0
|u FZJ
|0 P:(DE-Juel1)7363
245 _ _ |a Measurement of tropospheric RO2 and HO2 radicals by a laser-induced fluorescence instrument (ROxLIF)
260 _ _ |a [S.l.]
|b American Institute of Physics
|c 2008
300 _ _ |a 084104-1 - 084104-12
336 7 _ |a Journal Article
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336 7 _ |a article
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440 _ 0 |a Review of Scientific Instruments
|x 0034-6748
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|v 79
500 _ _ |a Record converted from VDB: 12.11.2012
520 _ _ |a A new method (ROxLIF) for the measurement of atmospheric peroxy radicals (HO(2) and RO(2)) was developed using a two-step chemical conversion scheme and laser-induced fluorescence (LIF) for radical detection. Ambient air is sampled into a differentially pumped flow reactor, in which atmospheric RO(x) radicals (=RO(2)+RO+HO(2)+OH) are chemically converted to HO(2) by a large excess of NO and CO at reduced pressures (ROx mode). When only CO is added as a reagent, the sum of atmospheric HO(2)+OH is converted to HO(2) (HOx mode). At the reactor outlet, part of the air flow is transferred into a low-pressure detection chamber, where the HO(2) is further converted by reaction with NO to OH, which is then detected with high sensitivity by LIF at 308 nm. The ROxLIF technique has been implemented in an existing LIF instrument that is also capable of measuring atmospheric OH. From the concurrent measurements of RO(x), HO(x) and OH, concentrations of HO(2) and RO(2) can be determined. The system is calibrated using the quantitative photolysis of water vapor at 185 nm as a radical source. Addition of CO or hydrocarbons to the calibration gas yields well-defined concentrations of HO(2) or RO(2), respectively, providing an estimated accuracy for the calibration of about 20%. The ROxLIF technique is extremely sensitive and has detection limits (signal-to-noise ratio=2) of about 0.1 pptv of HO(2) or RO(2) at a time resolution of 1 min. The paper describes the technique and its calibration, discusses the chemistry in the conversion reactor and possible interferences, and gives an example of ambient air measurements to demonstrate the performance of the new technique.
536 _ _ |a Atmosphäre und Klima
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588 _ _ |a Dataset connected to Web of Science, Pubmed
650 _ 7 |a J
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700 1 _ |a Holland, F.
|b 1
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|0 P:(DE-Juel1)16342
700 1 _ |a Hofzumahaus, A.
|b 2
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|0 P:(DE-Juel1)16326
773 _ _ |a 10.1063/1.2968712
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|t Review of scientific instruments
|v 79
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856 7 _ |u http://dx.doi.org/10.1063/1.2968712
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920 1 _ |k ICG-2
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