Rain samples were collected sequentially (each about 1mm) through rain events on 9-10 June, 27 August, and 19 October 1989 at Nagatsuta campus, Tokyo Institute of Technology. The concentrations of F
- and Br
- ions ranged from 0.20 to 53.8μg/l and from 0.74 to 19.0μg/l in three rain events, respectively. The ratios of F
-/Cl
- were high at the initial stage and gradually decreased. There was a high correlation between concentrations of Ca2
+ and F
- in three rain events, whose coefficient was 0.97, 0.89, 0.99 for rain events on 9-10 June, 27 August, and 19 October, respectively. On the other hand, the ratios of Br
-/Cl
- were approximately equal to the sea salt ratio (3.4×10
-3). However, in rain events on 9-10 June and 19 October, the ratios of Br/C1
- largely exceeded sea salt ratio at the middle or final stages of the events. There was a high correlation between N03
- and non-sea salt Br
- indicating that anthropogenic Br
- was loaded on precipitation.
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