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噴砂現象の規則性とその成因 : 日本海中部地震による秋田県若美町, 秋田港における噴砂災害
http://hdl.handle.net/10191/39025
502958e3-ba68-4d42-84e2-7906f29a915f
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 | 2016-03-03 | |||||
タイトル | ||||||
タイトル | 噴砂現象の規則性とその成因 : 日本海中部地震による秋田県若美町, 秋田港における噴砂災害 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | 噴砂現象の規則性とその成因 : 日本海中部地震による秋田県若美町, 秋田港における噴砂災害 | |||||
言語 | ||||||
言語 | jpn | |||||
資源タイプ | ||||||
資源 | http://purl.org/coar/resource_type/c_6501 | |||||
タイプ | departmental bulletin paper | |||||
その他のタイトル | ||||||
その他のタイトル | On the regularity and origin of sand crater caused by the earthquake : Disaster by sand crater at Wakami一machi and Akita harbour, Akita prefecture | |||||
著者 |
藤田, 至則
× 藤田, 至則 |
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著者別名 | ||||||
識別子 | ||||||
識別子 | 162009 | |||||
識別子Scheme | WEKO | |||||
姓名 | ||||||
姓名 | Fujita, Yukinori | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | The author concluded the origin of sand crater caused by the earthquake of the middle part of Japan Sea (May, 26, 1983) as follows: 1. Sand mass of crater erupted from the tension cracks formed the artificial soil parts of paddy fields at Wakami-machi, and from the cracks in the reclaimed soil at Akita Harbor (Fig. 8-3 and Fig. 9-3), 2. The tension cracks resulted from the sideslip along the sand dune (Fig. 8-2 and Fig. 9-2) 3. The sideslips were caused by the gravity of the paddy soil on the liquefacted sand mass (Fig. 8-1 and Fig. 9-1). Therefore, the occurrence of sand craters essentially attributed the cause to the existence of the inclined water level in sand mass on the inclined basement (Fig. 8 and 9). | |||||
書誌情報 |
新潟大学積雪地域災害研究センター研究年報 en : 新潟大学積雪地域災害研究センター研究年報 巻 5, p. 53-69, 発行日 1984-01 |
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出版者 | ||||||
出版者 | 新潟大学積雪地域災害研究センター | |||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 03877892 | |||||
書誌レコードID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN00183327 | |||||
著者版フラグ | ||||||
値 | publisher |