Journal of Geophysical Research Atmospheres · 2003 · 256 citations · 64 references
Radical EmissionEngineeringAtmospheric PhotochemistryPhotolysis FrequenciesAir QualityChemistryEnvironmental PhotochemistryAtmospheric ScienceOzone Layer DepletionPhotochemistryPhysicsMechanistic PhotochemistryRadical (Chemistry)Radiation MeasurementQuantum ChemistryOzoneDetection LimitAtmospheric RadiationNatural SciencesSpectroscopyAtmospheric ProcessAir PollutionRadical ConcentrationsChemical KineticsBerliner Ozone
This paper presents the measurements of OH and HO 2 radical concentrations as well as photolysis frequencies of different molecules during the Berliner Ozone (BERLIOZ) field experiment in July/August 1998 at the rural site Pabstthum about 50 km NW of Berlin. Radical concentrations were measured using laser‐induced fluorescence (LIF) spectroscopy, while filter radiometers and a scanning spectroradiometer were used to obtain photolysis frequencies. The radical data set covers the time period from 20 July to 6 August and consists of more than 6000 simultaneous measurements of OH and HO 2 with a typical time resolution of about 90 s. The maximum OH and HO 2 daytime concentrations were 8 × 10 6 and 8 × 10 8 cm −3 , respectively. While nighttime values of OH were usually below the detection limit of our instrument (3.5 × 10 5 cm −3 ), HO 2 did show significant concentrations throughout most of the nights (on average 3 × 10 7 cm −3 ). The OH concentration was mainly controlled by solar UV radiation and showed a high linear correlation with J(O 1 D). A deviation from this general behavior was observed around dawn and dusk, when OH concentrations well above the detection limit were observed, although J(O 1 D) was essentially zero. A comparison with data sets from previous campaigns revealed that even though the linear correlation is found in other environments as well the slope [OH]/J(O 1 D) differs significantly. The diurnal cycles of HO 2 were less dependent on the solar actinic flux but were predominantly influenced by NO. During episodes of high NO, HO 2 remained below the detection limit (1 × 10 7 cm −3 ) but started to rise rapidly as soon as NO started to decrease.
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Atmospheric chemistry of VOCs and NOx
Roger Atkinson · Atmospheric Environment · 2000 · 3.6K citations
Engineering, Atmospheric Photochemistry, Atmospheric Science +4
B. Alicke, U. Platt, J. Stutz · Journal of Geophysical Research Atmospheres · 2002 · 394 citations · Full text
Ozono Study, Advanced Oxidation Process, Radical Emission +21