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  1. 0 資料タイプ別
  2. 03 紀要論文
  1. 360 災害・復興科学研究所
  2. 20 紀要
  3. 90 新潟大学積雪地域災害研究センター研究年報
  4. 第5号

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
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
5_53-69.pdf 5_53-69.pdf (1.5 MB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
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

WEKO 162008

藤田, 至則

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著者別名
識別子 162009
識別子Scheme WEKO
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
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
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