Nature of Atmospheric Aerosols over the Desert Areas in the Asian Continent: Chemical State and Number Concentration of Particles Measured at Dunhuang,China |
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| Authors: | Iwasaka Y Shi G-Y Shen Z Kim Y S Trochkine D Matsuki A Zhang D Shibata T Nagatani M Nakata H |
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| Institution: | (1) Graduate School of Environmental Studies, Nagoya University, Chikusa-ku, Nagoya, Japan (author for correspondence;(2) Institute of Atmospheric Physics, Chinese Academy of Science, Beijing, China;(3) Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Science, Lanzhou, China;(4) Graduate School of Science, Nagoya University, Chikusa-ku, Nagoya, Japan;(5) Faculty of Environmental and Symbiotic Sciences, Prefectural University of Kumamoto, Kumamoto, Japan;(6) Solar-Terrestrial Environment Laboratory, Nagoya University, Toyokawa, Japan |
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| Abstract: | Measurements of aerosol were made in August and October 2001, and January 2002, at Dunhuang, China (40°00 N, 94°30E), to understand the nature of atmosphericparticles over the desert areas in the Asian continent. Balloon-borne measurements with an optical particle counter suggested that particle size and concentration had a noticeable peak in size range of super micron in not only the boundary mixing layer but also the free troposphere. Thickness of the boundary mixing layer, from distributions of particle concentration, was about 4 km in summer (17 August 2001), about2.5 km in fall (17 October 2001), and about 3 km in winter (11 January 2002), which suggest active mixing of particles near the boundary in summer. Number-size distribution of particleshowed a noticeable peak in the super micron particles size range inthe mixing boundary layer: 0.4–2 particles cm-3 at diameter>1.2  m in summer, 0.05–4 particles cm-3 at diameter >1.2 m in fall, and 0.1–5 particles cm-3 at diameter>1.2 m in winter. In winter strong inversion of atmospherictemperature was found in the height range from the boundary to about 3 km and vertical distribution of particle concentration well corresponded with the temperature distribution. Chemical elements of individual aerosols, which were collectedin the boundary layer atmosphere at Dunhuang (18 October 2001) were analyzed with an electron microscope equipped with EDX. Thosesingle particle analysis suggested that most of the particles with supermicron size were soil particles, and those particles had littlesulfate on its surface. This is a very important different point,comparing with the chemical state of soil particles, which weretransported from the desert area of China to Japan, and showed frequentlythe existence of sulfate on the particle surface. Therefore, it isstrongly suggested that dust particles can be chemically modifiedduring their long-range transport from desert areas to Japan. |
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| Keywords: | balloon-borne measurements KOSA particle number-size distribution |
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