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  1. D300 大学院環境学研究科
  2. D300a 雑誌掲載論文
  3. 学術雑誌

Triple oxygen isotope evidence for the pathway of nitrous oxide production in a forested soil with increased emission on rainy days

http://hdl.handle.net/2237/0002013611
http://hdl.handle.net/2237/0002013611
0291f3f5-6280-4bb4-9463-39c987e0bf31
名前 / ファイル ライセンス アクション
bg-22-4333-2025.pdf bg-22-4333-2025.pdf (3.3 MB)
アイテムタイプ itemtype_ver1(1)
公開日 2025-11-25
タイトル
タイトル Triple oxygen isotope evidence for the pathway of nitrous oxide production in a forested soil with increased emission on rainy days
言語 en
著者 Ding, Weitian

× Ding, Weitian

en Ding, Weitian

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Tsunogai, Urumu

× Tsunogai, Urumu

en Tsunogai, Urumu

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Huang, Tianzheng

× Huang, Tianzheng

en Huang, Tianzheng

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Sambuichi, Takashi

× Sambuichi, Takashi

en Sambuichi, Takashi

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Ruan, Wenhua

× Ruan, Wenhua

en Ruan, Wenhua

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Ito, Masanori

× Ito, Masanori

en Ito, Masanori

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Xu, Hao

× Xu, Hao

en Xu, Hao

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Kim, Yongwon

× Kim, Yongwon

en Kim, Yongwon

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Nakagawa, Fumiko

× Nakagawa, Fumiko

en Nakagawa, Fumiko

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アクセス権
アクセス権 open access
アクセス権URI http://purl.org/coar/access_right/c_abf2
権利
権利情報 © Author(s) 2025. This work is distributed under the Creative Commons Attribution 4.0 License.
言語 en
内容記述
内容記述タイプ Abstract
内容記述 Continuous increases in atmospheric nitrous oxide (N2O) concentrations are a global concern. Both nitrification and denitrification are the major pathways of N2O production in soil, one of the most important sources of tropospheric N2O. The 17O excess (Δ17O) of N2O can be a promising signature for identifying the main pathway of N2O production in soil. However, reports on Δ17O are limited. Thus, we determined temporal variations in the Δ17O of N2O emitted from forested soil for more than one year and that of soil nitrite (NO2^-), which is a possible source of O atoms in N2O. We found that N2O emitted from the soil exhibited significantly higher Δ17O values on rainy days (+0.12 ± 0.13 ‰) than on fine days (−0.30 ± 0.09 ‰), and the emission flux of N2O was significantly higher on rainy days (38.8 ± 28.0 µg N m−2 h−1) than on fine days (3.8 ± 3.1 µg N m−2 h−1). Because the Δ17O values of N2O emitted on rainy and fine days were close to those of soil NO2^- (+0.23 ± 0.12 ‰) and O2 (−0.44 ‰), we concluded that although nitrification was the main pathway of N2O production in the soil on fine days, denitrification became active on rainy days, resulting in a significant increase in the emission flux of N2O. This study reveals that the main pathway of N2O production can be identified by precisely determining the Δ17O values of N2O emission from soil and by comparing the Δ17O values with those of NO2^-, O2, and H2O in the soil.
言語 en
出版者
出版者 European Geosciences Union
言語 en
言語
言語 eng
資源タイプ
資源タイプresource http://purl.org/coar/resource_type/c_6501
タイプ journal article
出版タイプ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
関連情報
関連タイプ isVersionOf
識別子タイプ DOI
関連識別子 https://doi.org/10.5194/bg-22-4333-2025
収録物識別子
収録物識別子タイプ EISSN
収録物識別子 1726-4189
書誌情報 en : Biogeosciences

巻 22, 号 17, p. 4333-4347, 発行日 2025-09-01
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