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Movement of the Ground due to Atmospheric Disturbance in a Sea Region
https://doi.org/10.15083/0000034941
https://doi.org/10.15083/0000034941752ddd78-9786-4362-9672-078004bc7951
名前 / ファイル | ライセンス | アクション |
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ji0093004.pdf (690.3 kB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2008-06-06 | |||||
タイトル | ||||||
タイトル | Movement of the Ground due to Atmospheric Disturbance in a Sea Region | |||||
言語 | en | |||||
言語 | ||||||
言語 | eng | |||||
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 | 10.15083/0000034941 | |||||
ID登録タイプ | JaLC | |||||
その他のタイトル | ||||||
その他のタイトル | 海面大氣壓の擾亂によつて起る地動に就て | |||||
著者 |
Sezawa, Katsutada
× Sezawa, Katsutada× Nishimura, Genrokuro |
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著者別名 | ||||||
識別子 | 134902 | |||||
識別子Scheme | WEKO | |||||
姓名 | 妹澤, 克雄 | |||||
著者別名 | ||||||
識別子 | 134903 | |||||
識別子Scheme | WEKO | |||||
姓名 | 西村, 源六郎 | |||||
著者所属 | ||||||
著者所属 | 地震研究所 | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | We may now complete this paper with a brief summary. 1. The movement of the ground is composed of four kinds of displacements ; namely the displacement due to the transmission of shallow water waves, that due to Bayleigh-waves, that due to distortional waves and that due to dilatational waves. 2. The velocity of the transmission of the displacement of the body due to shallow water waves is equal to that of shallow water waves, while the transmission of the displacements of other kinds have their own velocities peculiar to the respective waves. 3. The amplitudes of the deformation of the solid body due to Rayleigh-waves and also to shallow water waves change as inverse square root of the epicentral distance, while those due to the dilatational and distortional waves diminish as inverse square of the epicentral distance. 4. Microseisms due to a disturbed weather occurring in a different region are chiefly due to long water waves, including breakers at the coast, advancing near the observing station, but not the seismic waves directly transmitted from the region of the disturbed weather. The action of the long water waves is, however, relatively small compared with that of breakers. 5. The amplitude of the ground due to pulsatory original disturbance of long periods is smaller than that due to short periods, even though the amplitude of the disturbing pressure is kept constant. | |||||
書誌情報 |
東京帝國大學地震研究所彙報 = Bulletin of the Earthquake Research Institute, Tokyo Imperial University 巻 9, 号 3, p. 291-309, 発行日 1931-09-22 |
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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 | AN00029699 | |||||
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 | 453 | |||||
主題Scheme | NDC | |||||
出版者 | ||||||
出版者 | 東京帝国大学地震研究所 | |||||
出版者別名 | ||||||
Earthquake Research Institute, Tokyo Imperial University |