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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23号

結晶片岩地域の山地における土石流源頭部の地下水流の推定

http://hdl.handle.net/10191/39231
http://hdl.handle.net/10191/39231
2b807264-27a0-4840-9121-404bee3aade0
名前 / ファイル ライセンス アクション
23_35-44.pdf 23_35-44.pdf (720.0 kB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2016-03-08
タイトル
タイトル 結晶片岩地域の山地における土石流源頭部の地下水流の推定
タイトル
言語 en
タイトル 結晶片岩地域の山地における土石流源頭部の地下水流の推定
言語
言語 jpn
キーワード
主題Scheme Other
主題 Slope failure
キーワード
主題Scheme Other
主題 Debris flow
キーワード
主題Scheme Other
主題 Groundwater temperature
キーワード
主題Scheme Other
主題 Electric conductivity
キーワード
主題Scheme Other
主題 Underflow
キーワード
主題Scheme Other
主題 Groundwater in deep layer
キーワード
主題Scheme Other
主題 斜面崩壊
キーワード
主題Scheme Other
主題 土石流
キーワード
主題Scheme Other
主題 地下水温
キーワード
主題Scheme Other
主題 電気伝導度
キーワード
主題Scheme Other
主題 伏流水
キーワード
主題Scheme Other
主題 深層地下水
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 Detecting of groundwater flow at source area of debris flow in crystalline schist mountains
著者 古谷, 元

× 古谷, 元

WEKO 160907

古谷, 元

Search repository
末峯, 章

× 末峯, 章

WEKO 160908

末峯, 章

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小山内, 信智

× 小山内, 信智

WEKO 160909

小山内, 信智

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原, 龍一

× 原, 龍一

WEKO 160910

原, 龍一

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佐藤, 修

× 佐藤, 修

WEKO 160911

佐藤, 修

Search repository
小松原, 岳史

× 小松原, 岳史

WEKO 160912

小松原, 岳史

Search repository
著者別名
識別子 160913
識別子Scheme WEKO
姓名 Furuya, Gen
著者別名
識別子 160914
識別子Scheme WEKO
姓名 Suemine, Akira
著者別名
識別子 160915
識別子Scheme WEKO
姓名 Osanai, Nobutomo
著者別名
識別子 160916
識別子Scheme WEKO
姓名 Hara, Ryuichi
著者別名
識別子 160917
識別子Scheme WEKO
姓名 Sato, Osamu
著者別名
識別子 160918
識別子Scheme WEKO
姓名 Komatsubara, Takeshi
抄録
内容記述タイプ Abstract
内容記述 Many debris flows caused by heavy rainfall have occurred at mountains in crystalline schist area, Shikoku Island, Southwestern Japan. The typical movement form of debris flow caused by heavy rainfall in mountainous area is fluidizing of soil mass from source area of debris flow to down slope (Stream). The debris flow at Tobinosu-dani stream in Zentoku, Nishiiyayama village on 29 June 1999 is this type of movement form. Therefore, it is important to make clear about occurrence mechanism of slope failures at source area of debris flow. Then, we carried out investigations of soil temperature at one-meter depth, water temperature and electric conductivity of springs and boreholes at the source area in the Tobinosu-dani stream and the Zentoku landslide. The results of our investigations are as follow. 1) There are two types of groundwater flows at the source areas of debris flows in the Tobinosu-dani stream that cause slope failure. One type is underflow changed by groundwater flow in deep layers with low value of electric conductivity. The other type is fissure water like groundwater vein-streams from deep layer with one digit higher value of electric conductivity than the underflow. 2) It is presumed that different of value of electric conductivity between underflow and fissure water is based on the different storage time (groundwater pass). Depth of the fissure water supply, especially, is corresponding to the approximate depth of the sliding surface (or bed rock) in the Zentoku landslide.
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 23, p. 35-44, 発行日 2001-12
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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