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秋田県能代市における地盤の振動特性(2)-1983年日本海中部地震で液状化を生じた地盤の微動特性-
https://iwate-u.repo.nii.ac.jp/records/9859
https://iwate-u.repo.nii.ac.jp/records/985992bb63c8-d53f-42e0-8080-237b3281b36c
名前 / ファイル | ライセンス | アクション |
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bt-v41n1p64-75.pdf (1.2 MB)
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Item type | 学術雑誌論文 / Journal Article(1) | |||||
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公開日 | 2009-11-12 | |||||
タイトル | ||||||
タイトル | 秋田県能代市における地盤の振動特性(2)-1983年日本海中部地震で液状化を生じた地盤の微動特性- | |||||
言語 | ||||||
言語 | jpn | |||||
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 | |||||
著者 |
斎藤, 徳美
× 斎藤, 徳美× 阿部, 司× 小林, 直太× 中島, 直吉× 中村, 操× 野越, 三雄× 毎熊, 輝記 |
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著者別名 | ||||||
姓名 | SAITO, Tokumi | |||||
著者別名 | ||||||
姓名 | ABE, Mamoru | |||||
著者別名 | ||||||
姓名 | KOBAYASHI, Naota | |||||
著者別名 | ||||||
姓名 | NAKAJIMA, Naoyoshi | |||||
著者別名 | ||||||
姓名 | NAMAKURA, Misao | |||||
著者別名 | ||||||
姓名 | NOGOSHI, Mitsuo | |||||
著者別名 | ||||||
姓名 | MAIGUMA, Teruki | |||||
著者(機関) | ||||||
岩手大学工学部 | ||||||
著者(機関) | ||||||
東北大学工学部 | ||||||
著者(機関) | ||||||
中央大学理工学部 | ||||||
著者(機関) | ||||||
(株)東京ソイルリサーチ | ||||||
著者(機関) | ||||||
日本物理探鉱(株) | ||||||
著者(機関) | ||||||
秋田大学教育学部 | ||||||
著者(機関) | ||||||
埼玉大学工学部 | ||||||
登録日 | ||||||
日付 | 2009-11-12 | |||||
書誌情報 |
物理探査 巻 41, 号 1, p. 64-75, 発行日 1988-01-01 |
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ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 0912-7984 | |||||
Abstract | ||||||
内容記述タイプ | Other | |||||
内容記述 | The previous study (Research group for short-and long-period microtremors: 1988), proved that the damage due to soil liquefaction in earthquakes could be estimated by measurements of short-period microtremors. As a series of the previous study, intensive measurements of microtremors and S-wave velocities were made on and around the most heavily damaged areas, Shonan-cho, Hamadori-cho, and Aobacho,in Noshiro City in 1985. Results of this investigation areas follows: 1) Most of the sites undamaged by soil liquefaction have S-wave velocities above 130m/sec and the ground water level deeper than 3m below the ground surface. 2) Most of the sites damaged by soil liquefaction have S-wave velocities below 130m/sec and the ground water level within 3m below the ground surface. These sites have type a of microtremor spectra, which have peaks above 4Hz, with high probability. 3) It is found that type a of microtremor spectrum corresponds well to the liquefied sites with very shallow level of ground water below the ground surface and very small subsurface S-wave velocities. Therefore, the measurements of short-period microtremors give a high probability prediction of damage from soil liquefaction. |
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出版者 | ||||||
出版者 | 社団法人物理探査学会 | |||||
権利 | ||||||
権利情報 | copyright (c) 1988 SEGJ | |||||
著者版フラグ | ||||||
出版タイプ | VoR | |||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 |