[H-TT35_1AM2] 地球人間圏科学研究のための加速器質量分析技術の革新と応用

[HTT35-09] 名古屋における14Cを用いたPM2.5中炭素の発生源解析

*池盛 文数¹、山神 真紀子²、本庄 浩司³、中村 俊夫⁴ (1.名古屋大学大学院環境学研究科、名古屋市環境科学調査センター、2.名古屋市環境科学調査センター、3.名古屋大学大学院環境学研究科、4.名古屋大学年代測定総合研究センター)

キーワード：大気エアロゾル, PM2.5, 放射性炭素

The measurement of radiocarbon (14C) has been used to estimate the relative contributions of fossil and contemporary carbon sources in particulate matter throughout the world. In this study, we use 14C to provide quantitative estimates of carbon origin sources in Nagoya in April 2003 to March 2004. pMC and OC/EC showed similar seasonal variations and high values (range 39.8 to 68.4, 1.0 to 2.0; average 53.4, 1.5, respectively) in May and early June, whereas the values of pMC stayed relatively low values (range 28.3 to 41.9, 0.7 to 1.2; average 34.2, 1.0, respectively) after middle June. To estimate the source region of high pMC values, backward air mass trajectories were calculated during the sampling period in April to June. The air mass appeared to have passed through eastern Siberia when the pMC values showed high values in May and early June which also showed high values of OC/EC ratio and OC concentrations. In 2003, many researchers reported the influence of large forest burning in Siberia. This large forest burning occurred in spring to summer. The smoke from this forest burning had reached to Korea, Japan, and North America. The influences from the Siberian forest fires had an important implication for air quality over East Asian region. We conclude that high pMC values measured in spring are originated from large forest fires in Siberia and transported long distance.