Stable sulfur isotope ratios of SO
2 emitted from active volcanoes such as Mt. Sakurajima and SatsumaIwojima were determined in relation to the project clarify source of sulfur in acidic and oxidative compounds in East Asia. The δ
34S of SO
2 were +10.1 to + 13.5‰ and +3.2 to +8.4‰at Satsuma-Iwojima and Mt. Sakurajima, respectively. We reported the δ
34S values for Mt. Sakurajima for the first time, but it should be noted that the gas samples were collected at station about 3 km away from fumarole. Nevertheless the OS values of Mt. Sakurajima volcano were similar to those from Mt. Use, Mt. Tarumae, Mt. Kuju-Iwoyama and Mt. Aso for which gas samples directly collected from fumarole.
The δ
34S values of sulfate in wet deposition collected at Mt. Shibi and Yorita, located approximately 50 km northwest of Mt. Sakurajima volcano, varied with time, contribution of the different sources of sulfur to these two sampling localities. Wet deposition samples from Mt. Shibi were considered to be more influenced by Mt. Sakurajima emission than Yorita, which was rather affected by continental anthropogenic emission.
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