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Dynamics of sulfur dioxide absorption in a raindrop falling at terminal velocity
Institution:1. College of Chemistry and Chemical Engineering, Central South University, Changsha 410083, China;2. Key Laboratory of Phytochemical R&D of Hunan Province, Hunan Normal University, Changsha 410081, China;1. Nuffield Department of Orthopaedics, Rheumatology and Musculoskeletal Sciences, University of Oxford, Oxford, United Kingdom;2. Department of Plastic Surgery, Stoke Mandeville Hospital, Buckinghamshire Healthcare NHS Trust, Aylesbury, United Kingdom;3. The Spires Cleft Centre, John Radcliffe Hospital, Oxford University Hospitals, Oxford, United Kingdom;4. Department of Pediatrics, McMaster University, Hamilton, Ontario, Canada;5. Division of Plastic and Reconstructive Surgery, Department of Surgery, Hospital for Sick Children, University of Toronto, Toronto, Ontario, Canada;6. MD Anderson Center for INSPiRED Cancer Care, the University of Texas, Houston, Texas, United States
Abstract:Sulfur dioxide absorption dynamics in a raindrop are studied numerically by means of a fully numerical simulation method (FNSM) in which a composite orthogonal grid system consisting of both gas- and liquid-phase is adopted. When a raindrop with fixed radius falls in association with terminal velocity, a recirculation bubble always accompanies the gas-phase flow field in the aft region of the drop. With regard to the drop internal flow structure it has a drastic variation with drop size. When the drop radius is small (e.g. rs=200 μm), only a single vortex motion is seen inside the drop. Under such a situation, sulfur dioxide absorbed from the interface is mainly transported from the area in front of the aft stagnation point. In contrast, as the drop is relatively large, say, rs=500 μm, it is of interest to find that a double-vortex motion, composed of a primary and a secondary vortexes, is clearly observed. As a result, the onset of SO2 transport process occurs at the drop’s surface near where the two vortexes meet. By defining a drop mass transport number, it indicates that the mass transported via internal circulation is always much faster than that by mass diffusion and the latter is highly relevant to the drop radius. Accordingly, the SO2 transport dynamics in a raindrop is essentially determined by drop size.
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