日本地球惑星科学連合2023年大会

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[J] 口頭発表

セッション記号 A (大気水圏科学) » A-AS 大気科学・気象学・大気環境

[A-AS07] 大気化学

2023年5月22日(月) 15:30 〜 16:45 展示場特設会場 (2) (幕張メッセ国際展示場)

コンビーナ:坂本 陽介(京都大学大学院地球環境学堂)、内田 里沙(一般財団法人 日本自動車研究所)、石戸谷 重之(産業技術総合研究所)、岩本 洋子(広島大学大学院統合生命科学研究科)、座長:猪俣 敏(国立研究開発法人国立環境研究所)、坂本 陽介(京都大学大学院地球環境学堂)、内田 里沙(一般財団法人 日本自動車研究所)

16:30 〜 16:45

[AAS07-19] 長崎における気相アンモニアの2年間連続測定:長距離輸送、ローカル発生源、火山活動の影響

*中山 智喜1、原田 龍1、上野 祐莉子1、前田 卓磨1,2池盛 文数3 (1.長崎大学、2.長崎県環境保健研究センター、3.名古屋市環境科学調査センター)

キーワード:アンモニア、フィールド観測、レーザー分光法、長距離輸送、火山、窒素循環

Gaseous ammonia (NH3) plays crucial roles in the atmosphere by neutralizing acidic compositions and leading secondary aerosol formation, and also acts as a key component in the nitrogen cycles of the Earth. Therefore, detailed understandings of behaviors and sources of NH3 are critically important for evaluating influence of acidic pollutants to atmospheric environment and human health. However, previous observations of NH3 have mainly conducted based on offline chemical analyses after collecting NH3 on filter pack or denuder tube, and reports on long-term continuous observation of NH3 are still very limited.

In this study, continuous observation of NH3 were conducted for more than two years from 2019 to 2021 using laser spectroscopic technique. By comparing the observed temporal variations of NH3 with meteorological data and gas- and particle-phase compositions, potential factors determining NH3 concentrations in different seasons have been analyzed. As results, high concentration events exceeding 10 ppbv were observed especially in late spring and autumn and with precipitations but NH3 concentrations were not positively correlated with particle-phase ammonium, suggesting the important contributions of local sources in Nagasaki in these seasons. From winter to early spring, increases in NH3 concentrations were often observed during the long-range transport events of air pollutants (e.g., sulfate, nitrate) from Asian continent, implying that gaseous NH3 are transported with particle-phase ammonium. In summer, whereas high concentration events were rarely observed, suppression of NH3 concentrations were observed when airmasses were considered to be affected by volcanic plumes containing sulfur dioxide (SO2) from southern Japan.