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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/10191/391060b28775f-77a5-4ace-ae48-a42b0aa8d53c
名前 / ファイル | ライセンス | アクション |
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11_17-23.pdf (280.9 kB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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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× 福江, 正治× 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 |
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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 |