著者
呉 佳紅 西島 好美 佐竹 洋
出版者
日本地球化学会
雑誌
地球化学 (ISSN:03864073)
巻号頁・発行日
vol.42, no.1, pp.1-11, 2008
参考文献数
37
被引用文献数
1

Nitrogen isotope ratio of nitrate ion in precipitation at Toyama was traced from June 2003 to December 2005 to investigate the behavior of nitrate ion inassociation with precipitation. δ<sup>15</sup>N value varied from -7.8 to + 1.6%o and showed seasonal variation; i.e., it was higher in winter than in summer. δ<sup>15</sup>N value negatively correlated to solar radiation. Negative correlation was also observed between δ<sup>15</sup>N value and concentration of atmospheric oxidant, which converted NO<sub>2</sub> to HNO<sub>3</sub>. Such correlations suggest that the δ<sup>15</sup>N value of nitrate ion decreases with increasing conversion rate from atmospheric NO<sub>2</sub> to HNO<sub>3</sub>. Based on an equation obtained from the relationship between the conversion rate and δ<sup>15</sup>N value according to the Rayleigh distillation model, 78-98% (av. ±1σ, 90±5%) NO<sub>2</sub> exhausted into the atmosphere were estimated to be converted into HNO<sub>3</sub>. The similar seasonal variation was also observed at Nagoya, although the δ<sup>15</sup>N values are systematically higher than those of Toyama. The NO<sub>2</sub> concentration at Nagoya istwice as high as the concentration at Toyama, suggesting that the conversion rate from NO<sub>2</sub> to HNO<sub>3</sub> is lower in Nagoya (av. ±1σ, 86±6%) than in Toyama.