The physical characteristics of sulfur aerosols |
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| Institution: | 1. Key Laboratory for Aerosol–Cloud–Precipitation of China Meteorological Administration, School of Atmospheric Physics, Nanjing University of Information Science and Technology, Nanjing, Jiangsu 210044, China;2. Weather Modification Office of Shanxi Province, Taiyuan, Shanxi 030032, China;3. Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Nanjing University of Information Science and Technology, Nanjing, Jiangsu 210044, China;4. College of Global Change and Earth System Science, Beijing Normal University, Beijing 100875, China;5. Department of Atmospheric and Oceanic Science and Earth System Science Interdisciplinary Center (ESSIC) University of Maryland, College Park, MD, USA;6. Meteorological Institute of Shaanxi Province, Xi''an, Shaanxi 710017, China;7. Meteorological Station in Anhui Province, Hefei, Anhui 230031, China;1. Jiangsu Key Laboratory of Atmospheric Environment Monitoring and Pollution Control (AEMPC), School of Environmental Sciences and Engineering, Nanjing University of Information Science & Technology, Nanjing 210044, China;2. Jiaxing Environmental Monitoring Station, Jiaxing 314000, China;3. Key Laboratory of Meteorological Disaster, Ministry of Education (KLME), Joint International Research Laboratory of Climate and Environment Change (ILCEC), Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Key Laboratory for Aerosol-Cloud-Precipitation of China Meteorological Administration, Nanjing University of Information Science & Technology, Nanjing 210044, China;4. Zhejiang Environmental Monitoring Center, Hangzhou 310000, China;1. College of City and Architecture Engineering, Zaozhuang University, Zaozhuang, Shandong 277160, China;2. Key Laboratory of Marine Ecology and Environmental Science, Institute of Oceanology, Chinese Academy of Sciences, Qingdao, Shandong 266071, China;3. College of Life Sciences, Zaozhuang University, Zaozhuang, Shandong 277160, China |
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| Abstract: | A review of the physical characteristics of sulfur-containing aerosols, with respect to size distribution of the physical distributions, sulfur distributions, distribution modal characteristics, nuclei formation rates, aerosol growth characteristics, and in situ measurement, has been made.Physical size distributions can be characterized well by a trimodal model consisting of three additive lognormal distributions.When atmospheric physical aerosol size distributions are characterized by the trimodal model, the following typical modal parameters are observed:1. Nuclei mode – geometric mean size by volume, DGVn, from 0.015 to 0.04 μm. σgn=1.6, nucler mode volumes from 0.0005 over the remote oceans to 9 μm3 cm?3 on an urban freeway.2. Accumulation mode – geometric mean size by volume, DGVa, from 0.15 to 0.5 μm, σga=1.6–2.2 and mode volume concentrations from 1 for very clean marine or continental backgrounds to as high as 300 μm3 cm?3 under very polluted conditions in urban areas.3. Coarse particle mode – geometric mean size by volume, DGVc, from 5 to 30 μm, σgn=2–3, and mode volume concentrations from 2 to 1000 μm3 cm?3.It has also been concluded that the fine particles (Dp<2 μm) are essentially independent in formation, transformation and removal from the coarse particles (Dp>2 μm).Modal characterization of impactor-measured sulfate size distributions from the literature shows that the sulfate is nearly all in the accumulation mode and has the same size distribution as the physical accumulation mode distribution.Average sulfate aerodynamic geometric mean dia. was found to be 0.48±0.1 μm (0.37±0.1 μm vol. dia.) and σg=2.00±0.29. Concentrations range from a low of about 0.04 μg m?3 over the remote oceans to over 8 μg m?3 under polluted conditions over the continents.Review of the data on nucleation in smog chambers and in the atmosphere suggests that when SO2, is present, SO2-to-aerosol conversion dominates the Aitken nuclei count and, indirectly, through coagulation and condensation, the accumulation mode size and concentration. There are indications that nucleation is ubiquitous in the atmosphere, ranging from values as low as 2 cm?3 h?1 over the clean remote oceans to a high of 6×106 cm?3 h?1 in a power plant plume under sunny conditions.There is considerable theoretical and experimental evidence that even if most of the mass for the condensational growth of the accumulation mode comes from hydrocarbon conversion, sulfur conversion provides most of the nuclei. |
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