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Tracing the fate of atmospheric nitrate deposited onto a forest ecosystem in Eastern Asia using Δ17O

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タイトル: Tracing the fate of atmospheric nitrate deposited onto a forest ecosystem in Eastern Asia using Δ17O
著者: Tsunogai, U. 著作を一覧する
Komatsu, D. D. 著作を一覧する
Daita, S. 著作を一覧する
Kazemi, G. A. 著作を一覧する
Nakagawa, F. 著作を一覧する
Noguchi, I. 著作を一覧する
Zhang, J. 著作を一覧する
発行日: 2010年 2月16日
出版者: Copernicus Publications
誌名: Atmospheric Chemistry and Physics
巻: 10
号: 4
開始ページ: 1809
終了ページ: 1820
出版社 DOI: 10.5194/acp-10-1809-2010
抄録: The stable isotopic compositions of nitrate in precipitation (wet deposition) and groundwater (spring, lake, and stream water) were determined for the island of Rishiri, Japan, so as to use the 17O anomalies (Δ17O) to trace the fate of atmospheric nitrate that had deposited onto the island ecosystem, which is a representative background forest ecosystem for eastern Asia. The deposited nitrate had large 17O anomalies with Δ17O values ranging from +20.8‰ to +34.5‰ (n = 32) with +26.2‰ being the annual average. The maximum Δ17O value of +34.5‰, obtained for precipitation on the 23rd to 24th of February 2007, was an extraordinarily large value among values for all samples of precipitation in Rishiri. Most nitrate in the sample might have been produced via NO3 radical in a highly polluted air mass that had been supplied from megacities on the eastern coast of the Asian continent. On the other hand, nitrate in groundwater had small Δ17O values ranging from +0.9‰ to 3.2‰ (n = 19), which corresponds to an mixing ratio of atmospheric nitrate to total nitrate of (7.4±2.6)%. Comparing the inflow and outflow of atmospheric nitrate in groundwater within the island, we estimated that the direct drainage accounts for (8.8±4.6)% of atmospheric nitrate that has deposited on the island and that the residual portion has undergone biological processing before being exported from the forest ecosystem.
資料タイプ: article
URI: http://hdl.handle.net/2115/44834
出現コレクション:雑誌発表論文等 (Peer-reviewed Journal Articles, etc)

提供者: 角皆 潤

 

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