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Identification of atmospheric ozone generated from seismic activity during the occurrence of multiple earthquakes across Japan in 2022

https://hiroshima.repo.nii.ac.jp/records/2008786
https://hiroshima.repo.nii.ac.jp/records/2008786
baa055cd-c8f9-42d7-a15c-1ef1a7d4b4e9
名前 / ファイル ライセンス アクション
SciTotalEnv_924_171714.pdf SciTotalEnv_924_171714.pdf (5.4 MB)
 Download is available from 2026/3/14.
Item type デフォルトアイテムタイプ_(フル)(1)
公開日 2025-01-10
タイトル
タイトル Identification of atmospheric ozone generated from seismic activity during the occurrence of multiple earthquakes across Japan in 2022
言語 en
作成者 Sakugawa, Hiroshi

× Sakugawa, Hiroshi

en Sakugawa, Hiroshi

Search repository
アクセス権
アクセス権 embargoed access
アクセス権URI http://purl.org/coar/access_right/c_f1cf
権利情報
言語 en
権利情報 © 2024. This manuscript version is made available under the CC-BY-NC-ND 4.0 license https://creativecommons.org/licenses/by-nc-nd/4.0/
権利情報
言語 en
権利情報 This is not the published version. Please cite only the published version.
権利情報
言語 ja
権利情報 この論文は出版社版ではありません。引用の際には出版社版をご確認、ご利用ください。
主題
言語 en
主題Scheme Other
主題 Seismic activity ozone
主題
言語 en
主題Scheme Other
主題 Photochemical ozone
主題
言語 en
主題Scheme Other
主題 Photochemical air pollution
主題
言語 en
主題Scheme Other
主題 Earthquake generation
主題
言語 en
主題Scheme Other
主題 Earthquake prediction
内容記述
内容記述 Ground-level atmospheric ozone (tropospheric ozone) is a well-known indicator of photochemical air pollution. Atmospheric ozone may also be an indicator of earthquake generation. Ground-level observations of atmospheric ozone at multiple sites were conducted in this study at the time of multiple earthquake occurrences in Japan in 2022. As the result of this study, ozone peaks of unknown origin were detected during the occurrence of multiple earthquakes across Japan in 2022. The level of these ozone peaks began to increase from a few days to a few hours before each earthquake, reaching a maximum concentration coincident with the time of earthquake generation. ‘Unknown ozone’ were detected at near earthquake epicentres, except in the case of deep earthquakes. The ‘unknown ozone’ were also associated with earthquake seismic intensities, which were monitored at seismograph stations in various Japanese cities, towns, and villages. A laboratory experiment by Baragiola et al. (2011) indicated that ppm levels of ozone can be generated in air by the crushing and grinding of terrestrial crustal rocks, generated by exo-electrons emitted by high electric fields, resulting from charge separation during rock fracture. Baragiola et al. (2011) proposed a hypothesis whereby atmospheric ozone could be generated via rock fracturing during the occurrence of earthquakes. This hypothesis could explain the ozone peaks correlating with multiple Japanese earthquakes observed in this study. The significance of atmospheric ozone generated by seismic activity is discussed in terms of it being a possible indicator of earthquake generation and prediction.
言語 en
出版者
出版者 Elsevier
言語 en
言語
言語 eng
資源タイプ
資源タイプ識別子 http://purl.org/coar/resource_type/c_6501
資源タイプ journal article
出版タイプ
出版タイプ AM
出版タイプResource http://purl.org/coar/version/c_ab4af688f83e57aa
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/10.1016/j.scitotenv.2024.171714
開始ページ
開始ページ 171714
書誌情報 en : Science of The Total Environment

巻 924, p. 171714, 発行日 2024-03-14
旧ID 56095
備考 The full-text file will be made open to the public on 14 March 2026 in accordance with publisher's 'Terms and Conditions for Self-Archiving'
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