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Atmospheric H2O2 measurement: comparison of cold trap method with impinger bubbling method.
1Institute of Geophysics and Planetary Physics, University of California at Los Angeles 90024, USA.
Summary
A new cold trap method accurately collects atmospheric hydrogen peroxide (H2O2), unlike impinger methods that overestimate levels due to ozone reactions. This finding is crucial for understanding atmospheric chemistry.
Area of Science:
- Atmospheric Chemistry
- Environmental Science
- Analytical Chemistry
Background:
- Accurate measurement of atmospheric hydrogen peroxide (H2O2) is vital for understanding atmospheric oxidation processes.
- Previous methods, like air impinger bubbling, may be subject to interferences.
- Ozone (O3) reactions with organic compounds can potentially generate peroxides in aqueous solutions.
Purpose of the Study:
- To develop and validate a reliable cold trap method for collecting atmospheric H2O2.
- To compare the cold trap method with the established air impinger bubbling method.
- To investigate the source of discrepancies observed between the two collection techniques.
Main Methods:
- Atmospheric air was drawn through a glass trap cooled with a dry ice-acetone slush at 2.5 L/min for 2 hours.
- Collection efficiency was assessed, and interferences from O3, SO2, and organic matter were evaluated.
- Results were compared with those obtained using the air impinger bubbling method.
Main Results:
- The cold trap method demonstrated collection efficiency > 99% with negligible interferences.
- Impinger method consistently yielded higher total peroxide (H2O2 + organic peroxide) values (0.06-3.7 ppb) compared to the cold trap method (0.02-1.2 ppb).
- Laboratory experiments indicated that ozone reactions with organic compounds in the impinger solution likely generated additional peroxides.
Conclusions:
- The cold trap method provides a more accurate measure of atmospheric H2O2 by avoiding artifactual peroxide formation.
- The air impinger method overestimates H2O2 due to ozone-induced reactions with atmospheric organics in the aqueous phase.
- Ozone-organic compound reactions in atmospheric water droplets may be a significant pathway for H2O2 generation in clouds and rainwater.