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Laboratory measurement of the dry deposition of sulfur dioxide onto northern Chinese soil samples
Institution:1. Department of Environmental Science and Engineering, Xi''an Jiaotong University, Xi''an 710049, China;2. Key Lab of Aerosol Chemistry & Physics, Institute of Earth Environment, Chinese Academy of Sciences, China;3. Key Laboratory of Regional Climate-Environment Research for Temperate East Asia, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China;4. Air Quality Research Division, Science and Technology Branch, Environment Canada, Toronto, Canada;5. Laboratory of Atmospheric Chemistry, Paul Scherrer Institute (PSI), 5232 Villigen, Switzerland;6. Centre for Climate and Air Pollution Studies, Ryan Institute, National University of Ireland Galway, University Road, Galway, Ireland;1. State Key Laboratory of Organic Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, 510 640, China;2. Université Clermont Auvergne, CNRS, SIGMA Clermont, Institut de Chimie de Clermont-Ferrand, F-63000, Clermont–Ferrand, France;3. Dipartimento di Chimica, Università degli Studi di Torino, Via Pietro Giuria 5, 10125, Torino, Italy;1. State Key Joint Laboratory of Environment Simulation and Pollution Control, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China;2. Center for Excellence in Regional Atmospheric Environment, Institute of Urban Environment, Chinese Academy of Sciences, Xiamen 361021, China;3. University of Chinese Academy of Sciences, Beijing 100049, China;1. Division of Nuclear Technology and Applications, Institute of High Energy Physics, Chinese Academy of Sciences, Beijing 100049, People''s Republic of China;2. Beijing Engineering Research Center of Radiographic Techniques and Equipment, Beijing 100049, People''s Republic of China;3. Beijing Entry-Exit Inspection and Quarantine Bureau Technology Centre, Beijing 100026, People''s Republic of China;4. College of Chemistry, Sichuan University, Chengdu, 610064, People''s Republic of China;1. Research Institute for Applied Mechanics (RIAM), Kyushu University, Fukuoka, Japan;2. State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry (LAPC), Institute of Atmospheric Physics (IAP), Chinese Academy of Sciences (CAS), Beijing, China;3. University of Yamanashi, Yamanashi, Japan;4. National Institute for Environmental Studies (NIES), Tsukuba, Ibaraki, Japan;5. Fukuoka Institute of Health and Environmental Sciences, Fukuoka, Japan
Abstract:We investigated soil surface resistance Rc to dry deposition of sulfur dioxide (SO2) onto different types of soils in laboratory experiments, using samples collected from the arid loess plateau and deserts of northern China. We evaluated the factors that affect Rc, which depends on the physical and chemical interaction between a trace constituent and the deposition surface. We observed that the values of Rc for SO2 decreased with increase of soil weight and increased with SO2 concentration, although surface coverage had little effect on Rc. The SO2 uptake rate by all the northern Chinese soil samples seemed to be, on the whole, dependent on relative humidity (RH). In all of the northern Chinese soil samples, Rc was in the range 0.028–0.65 s mm−1, and was exponentially related to the effective surface area of each soil sample, regardless of RH. Wet chemical analysis of sulfur deposited onto the soil samples showed that oxidation ratio of sulfur(IV) to sulfur(VI) was related to RH, which might be related to complex interactions among the amount of water on the soil sample, the pH, and the metallic ions in the liquid phase.
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