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Deep Groundwater Discharge and Ground Surface Phenomena
https://doi.org/10.15083/0000032527
4548918b-2602-4afb-b9d8-2bf780a1f6af
名前 / ファイル | ライセンス | アクション | |
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2007-04-23 | |||||
タイトル | ||||||
タイトル | Deep Groundwater Discharge and Ground Surface Phenomena | |||||
言語 | en | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
主題 | pore water | |||||
主題Scheme | Other | |||||
キーワード | ||||||
主題 | groundwater | |||||
主題Scheme | Other | |||||
キーワード | ||||||
主題 | water temperature | |||||
主題Scheme | Other | |||||
キーワード | ||||||
主題 | remote sensing | |||||
主題Scheme | Other | |||||
資源タイプ | ||||||
資源 | http://purl.org/coar/resource_type/c_6501 | |||||
タイプ | departmental bulletin paper | |||||
ID登録 | ||||||
ID登録 | 10.15083/0000032527 | |||||
ID登録タイプ | JaLC | |||||
その他のタイトル | ||||||
その他のタイトル | 深部地下水の放出と地表現象 | |||||
著者 |
Tsukuda, Tameshige
× Tsukuda, Tameshige× Gotoh, Keinosuke× Sa, Osamu |
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著者別名 | ||||||
識別子 | ||||||
識別子 | 125244 | |||||
識別子Scheme | WEKO | |||||
姓名 | ||||||
姓名 | 佃, 為成 | |||||
著者別名 | ||||||
識別子 | ||||||
識別子 | 125245 | |||||
識別子Scheme | WEKO | |||||
姓名 | ||||||
姓名 | 後藤, 恵之輔 | |||||
著者別名 | ||||||
識別子 | ||||||
識別子 | 125246 | |||||
識別子Scheme | WEKO | |||||
姓名 | ||||||
姓名 | 佐藤, 修 | |||||
著者所属 | ||||||
著者所属 | Earthquake Research Institute, University of Tokyo | |||||
著者所属 | ||||||
著者所属 | Division of Environmental System Science, Department of Systems Science, Graduate School of Science and Technology, Nagasaki University | |||||
著者所属 | ||||||
著者所属 | Research Center for Hazards in Snowy Areas, Niigata Univerisity | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | Stress changes associated with crustal deformations may induce migration of fluid within the crust. It is hypothetically expected that a volume of pore water, being suddenly pressured in response to an elevated stress level in some seismogenic zone, will tend to intrude up into a crack network, and incidentally emerge at the ground surface. Groundwater changes in temperature and concentrations of chemical constituents should be observed at the spot where the upwelling fluid comes out. This paper reports the following 4 transient events recently found in Japan as evidence of the near surface discharge of hot and pressured water of a deep origin: 1) Frequent rises in well water temperature were observed at Iwakuni,Yamaguchi Prefecture, southwest Japan. The largest rise occurred just before the 2001 Geiyo earthquake of M0.1, which indicated a possible precursor for the shock. A chemical analysis of ion concentrations of the hot water suggested that the temperature anomalies arise from contamination by intruding external deep water; 2) Gushing of groundwater at the sea bottom was considered to have occurred at the Akashi Strait 2 days before the 1335 Kobe earthquake of M1.3, based on an interpretation of the appearance of brownish-black seawater found by the captain of a passenger boat; 3) Upwelling of deep hot groundwater was occurred at Inagawa Town, Hyogo Prefecture, southwest Japan, which was associated with the 1335 Kobe earthquake. The well water temperature rose 3-4℃. at the time of the shock, and decayed with a time constant of 1-2 years; 4) Heating of ground rocks by upwelling hot water intruding into the fracture zone of an active fault, which is considered to be a precursor for the April 1, 1335 Niigata-ken Hokubu earthquake of M5.5, was confirmed by a LANDSAT infrared image in the northern Niigata area, central Japan, on a summer night in 133.. All of the above transient phenomena can be reasonably understood in the light of the hypothesis of pressured hot water upwelling from deep underground in response to crustal movements around seismically active regions. | |||||
書誌情報 |
東京大學地震研究所彙報 = Bulletin of the Earthquake Research Institute, University of Tokyo 巻 80, 号 3-4, p. 105-131, 発行日 2005 |
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ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 00408972 | |||||
書誌レコードID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN00162258 | |||||
フォーマット | ||||||
内容記述タイプ | Other | |||||
内容記述 | application/pdf | |||||
日本十進分類法 | ||||||
主題 | 51.1 | |||||
主題Scheme | NDC | |||||
出版者 | ||||||
出版者 | 東京大学地震研究所 | |||||
出版者別名 | ||||||
Earthquake Research Institute, University of Tokyo |