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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22号

平成11年6月29日の豪雨によって善徳地すべり地・大師堂周辺で発生した斜面崩壊と水みちの分布

http://hdl.handle.net/10191/39220
http://hdl.handle.net/10191/39220
4690f272-36fa-40e1-8dbc-84b10af1c648
名前 / ファイル ライセンス アクション
22_44-60.pdf 22_44-60.pdf (874.2 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 平成11年6月29日の豪雨によって善徳地すべり地・大師堂周辺で発生した斜面崩壊と水みちの分布
タイトル
言語 en
タイトル 平成11年6月29日の豪雨によって善徳地すべり地・大師堂周辺で発生した斜面崩壊と水みちの分布
言語
言語 jpn
キーワード
主題Scheme Other
主題 Zentoku landslide
キーワード
主題Scheme Other
主題 slope failure
キーワード
主題Scheme Other
主題 investigation of one-meter depth temperature
キーワード
主題Scheme Other
主題 groundwater vein-stream
キーワード
主題Scheme Other
主題 borehole water temperature
キーワード
主題Scheme Other
主題 善徳地すべり
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 1m深地温探査
キーワード
主題Scheme Other
主題 地下水脈
キーワード
主題Scheme Other
主題 孔内水温
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 Distribution of slope failures caused by heavy rain on 29 June 1999 and groundwater vain-streams in Taishido, Zentoku landslide, Shikoku Island, Japan.
著者 古谷, 元

× 古谷, 元

WEKO 160970

古谷, 元

Search repository
末峯, 章

× 末峯, 章

WEKO 160971

末峯, 章

Search repository
小山内, 信智

× 小山内, 信智

WEKO 160972

小山内, 信智

Search repository
原, 龍一

× 原, 龍一

WEKO 160973

原, 龍一

Search repository
著者別名
識別子 160974
識別子Scheme WEKO
姓名 Furuya, Gen
著者別名
識別子 160975
識別子Scheme WEKO
姓名 Suemine, Akira
著者別名
識別子 160976
識別子Scheme WEKO
姓名 Osanai, Nobutomo
著者別名
識別子 160977
識別子Scheme WEKO
姓名 Hara, Ryuichi
抄録
内容記述タイプ Abstract
内容記述 Many slope failures were occurred by a heavy rainfall 476mm/day on 29 June 1999 at the Zentoku landslide area in the central Shikoku Island, Japan. It is necessary to investigate the distribution and behavior of groundwater in the slopes, because the occurrences of slope failures and landslides are caused by increase of pore water pressure on the sliding surface. We determined soil temperatures in one-meter depth at Taishido and water temperatures in non-strainer boreholes along the line of extensometers at the Z6 block in the Zentoku landslide, in order to find groundwater vein-Streams. Here we give a summary of our investigation as follows. 1) Two types of groundwater vein-streams are distinguished by the distribution of soil and water temperatures and are respectively derived from shallow and deep layers in the landslide mass. 2) The largest vein-stream of groundwater from deep layers is found from the north to east part of the study area, and probably flows toward the southeast direction. The lowest soil temperature in one-meter depth along the vein-stream shows 12.32℃ and is close to water temperature at the bottom of boreholes in the upper slope. There are also two or three local groundwater vein-streams from deep layers in the study area. 3) Another large groundwater vein-stream is distributed from the west part of the study area to a large slope failure nearby Taishido and probably flows toward the east direction. The soil temperatures in one-meter depth along this vein-stream and the water temperature at a spring in the head scarp of the large slope failure are significantly higher than the soil temperatures along the above largest vein-stream from deep layers. This vein-stream flowing toward the east direction, therefore, is the shallow groundwater in origin. 4) The large slope failure nearby Taishido and a surface subsidence might be caused by groundwater from shallow layers, on the basis of the distribution of the vein-streams and slope failures. The slope failures located in the northeast part of the study area were influenced by groundwater from deep layers.
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 22, p. 44-60, 発行日 2000-03
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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