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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7号

姫川水系浦川流域における斜面崩壊と土石流について : その4 (中俣三郎教授退官記念号)

http://hdl.handle.net/10191/39060
http://hdl.handle.net/10191/39060
a60da8da-22e9-49fb-8e68-aa936860cbd4
名前 / ファイル ライセンス アクション
7_115-155.pdf 7_115-155.pdf (2.2 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 姫川水系浦川流域における斜面崩壊と土石流について : その4 (中俣三郎教授退官記念号)
タイトル
言語 en
タイトル 姫川水系浦川流域における斜面崩壊と土石流について : その4 (中俣三郎教授退官記念号)
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 Geological and geochemcical studies on the slope failures and observation of debris flows in the Ura river basin, Nagano Prefecture : part 4
著者 青木, 滋

× 青木, 滋

WEKO 161846

青木, 滋

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佐藤, 修

× 佐藤, 修

WEKO 161847

佐藤, 修

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霜鳥, 重雄

× 霜鳥, 重雄

WEKO 161848

霜鳥, 重雄

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藤田, 至則

× 藤田, 至則

WEKO 161849

藤田, 至則

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茅原, 一也

× 茅原, 一也

WEKO 161850

茅原, 一也

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早川, 嘉一

× 早川, 嘉一

WEKO 161851

早川, 嘉一

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鈴木, 幸治

× 鈴木, 幸治

WEKO 161852

鈴木, 幸治

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五日市, 好則

× 五日市, 好則

WEKO 161853

五日市, 好則

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北出, 一郎

× 北出, 一郎

WEKO 161854

北出, 一郎

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加藤, 陽一

× 加藤, 陽一

WEKO 161855

加藤, 陽一

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森田, 信介

× 森田, 信介

WEKO 161856

森田, 信介

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著者別名
識別子 161857
識別子Scheme WEKO
姓名 Aoki, Shigeru
著者別名
識別子 161858
識別子Scheme WEKO
姓名 Sato, Osamu
著者別名
識別子 161859
識別子Scheme WEKO
姓名 Shimotori, Shigeo
著者別名
識別子 161860
識別子Scheme WEKO
姓名 Fujita, Yukinori
著者別名
識別子 161861
識別子Scheme WEKO
姓名 Chihara, Kazuya
著者別名
識別子 161862
識別子Scheme WEKO
姓名 Hayakawa, Kaichi
著者別名
識別子 161863
識別子Scheme WEKO
姓名 Suzuki, Koji
著者別名
識別子 161864
識別子Scheme WEKO
姓名 Itsukaichi, Yoshinori
著者別名
識別子 161865
識別子Scheme WEKO
姓名 Kitade, Ichiro
著者別名
識別子 161866
識別子Scheme WEKO
姓名 Kato, Yoichi
著者別名
識別子 161867
識別子Scheme WEKO
姓名 Morita, Nobusuke
抄録
内容記述タイプ Abstract
内容記述 This is the fourth of a series of papers on the Ura River basin (AOKI et al 1981, 1982 and 1983) and deals with the results of the research carried out in 1983. The results can be summarized as follows: 1. In order to analyze the possibility of landslide, a boring test with 80m depth was carried out in the hazardous slope as shown in Fig. 1. 2. In the area of the lower stream of the Ura river, we found the distribution of pyroclastic flow derived from the Kazabuki volcano. 3. From July to October in 1983, we observed 21 debris flows in the Kanayama river by using T.V. cameras (Table 2). Observation data are shown in Table 3 and Table 4. The results of soil tests for debris flow deposit are shown in Tables 5 to 8 and Fig. 3. 4. From the multivariate analysis on the relationships between the rainfall and the occurrence of debris flows, the results suggest that the occurrence of debris flows was related to not only the rainfall but also to other factors (Fig. 9 and Table 12). 5. A change in the electrical conductivity of river water by recorder suggests the occurrence of flowing water with high electrical conductivity before the occurrence of debris flow as shown in Fig. 11.
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 7, p. 115-155, 発行日 1986-01
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
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