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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11号

富士山の雪代に関する基礎的研究 (故大草重康教授追悼号)

http://hdl.handle.net/10191/39106
http://hdl.handle.net/10191/39106
0b28775f-77a5-4ace-ae48-a42b0aa8d53c
名前 / ファイル ライセンス アクション
11_17-23.pdf 11_17-23.pdf (280.9 kB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2016-03-04
タイトル
タイトル 富士山の雪代に関する基礎的研究 (故大草重康教授追悼号)
タイトル
言語 en
タイトル 富士山の雪代に関する基礎的研究 (故大草重康教授追悼号)
言語
言語 jpn
キーワード
主題Scheme Other
主題 Slush avalanche
キーワード
主題Scheme Other
主題 Mt. Fuji
キーワード
主題Scheme Other
主題 Seepage force
キーワード
主題Scheme Other
主題 Thawed soil
キーワード
主題Scheme Other
主題 Frozen soil
キーワード
主題Scheme Other
主題 Permeability
キーワード
主題Scheme Other
主題 雪代(土・雪混合流)
キーワード
主題Scheme Other
主題 富士山
キーワード
主題Scheme Other
主題 浸透水圧
キーワード
主題Scheme Other
主題 融解土
キーワード
主題Scheme Other
主題 凍結土
キーワード
主題Scheme Other
主題 透水係数
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 Fundamental Study on Slush Avalanche on the Slope of Mt. Fuji
著者 土肥, 直喜

× 土肥, 直喜

WEKO 161502

土肥, 直喜

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福江, 正治

× 福江, 正治

WEKO 161503

福江, 正治

Search repository
安間, 荘

× 安間, 荘

WEKO 161504

安間, 荘

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著者別名
識別子 161505
識別子Scheme WEKO
姓名 Dohi, Naoki
著者別名
識別子 161506
識別子Scheme WEKO
姓名 Fukue, Masaharu
著者別名
識別子 161507
識別子Scheme WEKO
姓名 Anma, So
抄録
内容記述タイプ Abstract
内容記述 Slush avalanches and debris flows often occur on the slope of Mt. Fuji. It is common that the shear plane exists in the upper thawed soil layer on the frozen soil layer. As the permeability of the frozen soil layer is extremely low in comparison to the upper thawed layer, ground seepage can easily develop during rain fall. Therefore, the instability condition of the slope is obtained mainly due to the seepage force developed in the thawed soil layer. This report describes the summary and results of a model experiment in relation to the mass flow, using soil samples obtained from the slope of Mt. Fuji. The result show that the slope stability problem of Mt. Fuji can be solved with the conventional analysis being used in geotechnical engineering, if the seepage forces are properly estimated. For the prediction of slush avalanches, the following factors are at least needed: (1) thickness of thawed soil layer and depth of frozen soil layer, (2) thickness of snow deposits, (3) water level in thawed layer, and (4) slope angle.
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 11, p. 17-23, 発行日 1989-12
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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