Methods of measurement and phenomena on dry deposition within acid deposition have not been understood, and not been established enough until lately. In this study, measurements by surrogate sampling method using bottle, which is one of the measuring methods of dry deposition, were performed, and discussed. The effect of water addition in sampling periods of dry deposition was significant, and the amounts of all species in collected dry deposition were higher than those at no addition of water and especially, easily water soluble components such as SO
42- and NO
3- were more collected by a factor of two or more. Another effect of water addition was that Ca
2+, which is the major component of atmospheric giant particle, was collected much more than other components in many cases. Regional distribution of dry deposition components showed that SO
42- and sea salt components such as Na
+ and Cl
- decreased inversely proportional to the distance from the sea coast. But, NO
3- and NH
4+, which were transformed secondary in atmospheric air, were highest in middle inland region such as Fussa. Comparing to the amounts of wet deposition components, dry deposition amount of Ca
2+ was about same with that in wet deposition, and dry deposition amounts of SO
42- and NO
3- were about half of those in wet deposition.
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