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Characterization of the winter atmospheric aerosols in Kyoto and Seoul using PIXE,EAS and IC
Institution:1. Graduate School of Energy Science, Kyoto University, Uji, Kyoto 611-0011, Japan;2. Department of Environmental Science, Dong-Nam Health College, Suwon 440-714, South Korea;1. Tokyo Institute of Technology, 4259 Nagatsuta, Midori-ku, Yokohama, Kanagawa 226-8503, Japan;2. The Institute of Advanced Energy, Kyoto University, Gokasho, Uji, Kyoto 611-0011, Japan;3. National Institute of Advanced Industrial Science and Technology, 1-2-1, Namiki, Tsukuba, Ibaraki 305-8564, Japan;4. Graduate School of Energy Science, Kyoto University, Yoshida Honmachi, Sakyo-ku, Kyoto 606-8501, Japan;5. Systems Research Center, Co. Ltd, KY Bldg., 3-16-7, Toranomon, Minato, Tokyo 105-0001, Japan;1. Frank Laboratory of Neutron Physics, Joint Institute for Nuclear Research, Dubna, Russia;2. Physics Department, Kyiv Taras Shevchenko National University, Kyiv, Ukraine;3. Institute for Safety Problems of Nuclear Power Plants, Chornobyl, Ukraine;4. Wigner Research Centre for Physics, Hungarian Academy of Sciences, Budapest, Hungary;5. Helmholtz-Zentrum Geesthach, Geesthacht, Germany;6. Faculty of Physics, St. Petersburg State University, Saint Petersburg, Russia;7. Center for Fundamental and Advanced Technical Research, Romanian Academy-Timisoara Branch, Timisoara, Romania;8. Institute of Experimental Physics, Slovak Academy of Sciences, Kosice, Slovakia;1. Institute of Experimental Physics, SAS, Watsonova 47, 040 01 Kosice, Slovakia;2. Joint Institute for Nuclear Research, Joliot-Curie 6, 141980 Dubna, Moscow region, Russia;3. Kyiv Taras Shevchenko National University, Volodymyrska Street 64, Kyiv, 01033 Ukraine;4. Helmholtz-Zentrum Geesthacht: Centre for Materials and Coastal Research, Max-Planck-Street 1, 21502 Geesthacht, Germany;5. Wigner Research Centre for Physics, HAS, H-1525 Budapest, POB 49, Hungary;1. Department of Earth System Science, Faculty of Science, Fukuoka University, Fukuoka, Japan;2. National Institute for Environmental Studies, Tsukuba, Japan;3. Fukuoka Institute for Atmospheric Environment and Health, Fukuoka University, Fukuoka, Japan;4. Hokkaido University, Sapporo, Japan;1. Departamento de Química, Universidade Federal do Paraná, 81531-990 Curitiba, PR, Brazil;2. Institut für Physikalische und Theoretische Chemie, Universität Tübingen, Auf der Morgenstelle 18, 72076 Tübingen, Germany;3. Instituto de Química, Universidade Federal do Rio de Janeiro, 21941-909 Rio de Janeiro, RJ, Brazil
Abstract:Characteristics of atmospheric aerosols in Kyoto, Japan and Seoul, Korea were investigated using particle-induced X-ray emission (PIXE), elemental analysis system (EAS) and ion chromatograph (IC). Atmospheric aerosols were collected into fine and coarse fractions using a two-stage filter pack sampler in Kyoto and Seoul in winter of 1998. PIXE was applied to analyze the middle and heavy elements with atomic number greater than 14 (Si), and EAS was applied to analyze the light elements such as H, C and N. The total mass concentration in Seoul was about two times higher than in Kyoto and the concentration of Ca, Si, and Ti that are mainly originated from soil were remarkably higher in Seoul. During an Asian dust storm event, the concentration of soil components increased dramatically and amounted to about 15 times higher than average concentration. The fine/coarse ratios of NH4+, NO3, and SO42− were extremely high in both sites. The fact that nearly 70% of fine particles in both Kyoto and Seoul consist of the light elements (N, C, and H) suggests the importance of light elements measurement. Good mass closure for fine particles with light element data was achieved.
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