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Evidence for large average concentrations of the nitrate radical (NO3) in Western Europe from the HANSA hydrocarbon database
Institution:1. School of Environmental Sciences, University of East Anglia, Norwich NR4 7TJ, UK;2. SEAES University of Manchester, Sackville Street Building, Sackville Street, Manchester M60 1QD, UK;3. Laboratoire Interuniversitaire des Systemes Atmospheriques (LISA), CMC—Université Paris 12 Val de Marne, 61 av du Général de Gaulle, 94 010 Créteil Cedex, France;4. Department of Meteorology, University of Bergen, Norway;5. IVL Swedish Environmental Research Institute Ltd, P.O. Box 5302, SE 400 14 Göteborg, Sweden;6. Norwegian Institute for Air Research (NILU), P.O. Box 100, N 2007 Kjeller, Norway;7. TNO Built Environment and Geosciences, P.O. Box 342, 7300 AH Apeldoorn, The Netherlands;8. RIVM, National Institute of Public Health, and Environmental Protection, P.O. Box 1, 3720 BA Bilthoven, The Netherlands;1. Instituto de Investigaciones en Fisicoquímica de Córdoba (INFIQC), Dpto. de Fisicoquímica, Facultad de Ciencias Químicas, Universidad Nacional de Córdoba, Ciudad Universitaria, 5000 Córdoba, Argentina;2. Facultad de Ciencias Exactas y Naturales, Universidad Nacional de Asunción, Campus Universitario, San Lorenzo, Paraguay;1. College of Geomatics, Xi’an University of Science and Technology, Xi’an 710054, China;2. State Key Laboratory of Geodesy and Earth’s Dynamics, Wuhan 430077, China;3. School of Geodesy and Geomatics, Wuhan University, Wuhan 430079, China;4. Key Laboratory of Geospace Environment and Geodesy, Ministry of Education, Wuhan University, Wuhan 430079, China;1. Departamento de Física, Universidade Federal do Espírito Santo, 29075-910 Vitória, Brazil;2. Centro de Química, and Departamento de Química, Universidade de Coimbra, 3004-535 Coimbra, Portugal;1. Department of Physical Chemistry, Indian Association for the Cultivation of Science, 2A & 2B Raja S. C. Mullick Road, Jadavpur, Kolkata 700032, West Bengal, India;2. Department of Chemistry, St. Xaviers’ College, Kolkata 700016, West Bengal, India;3. Departamento de Química and Centro de Química, Universidade de Coimbra, 3004-535 Coimbra, Portugal;1. Department of Physical and Organic Chemistry, Institute Jožef Stefan, Jamova c. 39, SI-1000 Ljubljana, Slovenia;2. Faculty of Chemistry and Chemical Technology, University of Ljubljana, Večna pot 113, SI-1000 Ljubljana, Slovenia
Abstract:The nitrate radical (NO3) was first measured in the atmosphere in the 1970s and suggestions were made that it could play a major role in oxidising many unsaturated hydrocarbons, such as those emitted from the biosphere. Analysis of the hydrocarbon mix over the North Atlantic Ocean suggested subsequently that the influence of NO3 radical chemistry at night was even more extensive, being on a par with hydroxyl radical chemistry at some times of the year.The paper presents a detailed analysis of an extensive database of many nonmethane hydrocarbons collected at various sites around the North Sea in the mid 1990s during the HANSA project. By comparing the relative rates of oxidation of iso and normal pentane with that of toluene and benzene it clearly shows that the efficiency of NO3 radical chemistry and hydroxyl radical chemistry over northwest Europe are similar in springtime and predicts an average nighttime NO3 concentration of the order of 350 pptv, assuming an annual average OH concentration of 0.6×106 cm−3. This value is very dependant on the average emission ratios of the different hydrocarbons and values between 200 and 600 pptv are possible. It is much larger than direct measurements made in Europe at the surface, but is of the same magnitude as concentrations measured recently from aircraft in the boundary layer over the northeast USA, and previously in vertical profiles by remote sounding over Europe.A simple analytical expression can be derived to calculate the NO3 concentration at night with the only variables being ozone and the loss rate of N2O5, either to the ground or to aerosol surfaces. The concentrations of NO3 calculated in this manner are similar to those derived from the analysis of the HANSA hydrocarbon database for typical conditions expected over Europe, but they are very dependant on the efficiency of the aerosol sink for N2O5.It is shown that NO3 oxidation of many unsaturated hydrocarbons can indeed be more efficient than OH oxidation, especially at times of the year outside the summer season. Direct evidence for hydrocarbon oxidation by NO3 radicals is shown by a series of peroxy radical measurements where the nighttime concentrations can be significantly higher than daytime concentrations in polluted air on occasion. Also the winter/summer (W/S) ratios of many unsaturated hydrocarbons are much lower than those expected from their removal purely by hydroxyl radical chemistry.The consequences of these findings are profound especially as satellite measurements of NO2, a major precursor to NO3, suggest that these high average concentrations of several hundred pptv could be widespread over most of the continents. This needs to be confirmed by direct in-situ measurement of nitrate radicals but it suggests a much larger role for NO3 chemistry in the oxidation capacity of the atmosphere than realised hitherto.
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