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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

福島県滝坂地すべり地の地下水の水質とその変動

http://hdl.handle.net/10191/39221
http://hdl.handle.net/10191/39221
89a53bab-ad90-4748-b909-e37d9b8b438e
名前 / ファイル ライセンス アクション
22_61-77.pdf 22_61-77.pdf (815.9 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 福島県滝坂地すべり地の地下水の水質とその変動
タイトル
言語 en
タイトル 福島県滝坂地すべり地の地下水の水質とその変動
言語
言語 jpn
キーワード
主題Scheme Other
主題 origin of groundwater
キーワード
主題Scheme Other
主題 chloride ion concentration
キーワード
主題Scheme Other
主題 seasonal change
キーワード
主題Scheme Other
主題 drainage wells
キーワード
主題Scheme Other
主題 地下水の起源
キーワード
主題Scheme Other
主題 塩化物イオン濃度
キーワード
主題Scheme Other
主題 季節変化
キーワード
主題Scheme Other
主題 集水井
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 Chemical variation of groundwater in the Takisaka landslide area, Fukushima Prefecture
著者 鈴木, 将之

× 鈴木, 将之

WEKO 160978

鈴木, 将之

Search repository
佐藤, 修

× 佐藤, 修

WEKO 160979

佐藤, 修

Search repository
著者別名
識別子 160980
識別子Scheme WEKO
姓名 Suzuki, Masayuki
著者別名
識別子 160981
識別子Scheme WEKO
姓名 Sato, Osamu
抄録
内容記述タイプ Abstract
内容記述 Groundwater samples were collected from a spring and drainage system such as drainage wells and boreholes in the Takisaka landslide area, Fukushima Prefecture. Major ion concentrations of the drainage were analyzed to investigate the effectiveness of existing measures on the landslide. Wells mainly drain shallow groundwater because drainage boreholes of wells are shallower than the slip surface. However, the higher chloride ion concentrations in the drainage suggest that deep groundwater is partially drained by drainage wells in Yudenosawa and Shimosawanome. The wells drain the deep groundwater that ascends along a fault several times every year, and contribute to reduce excess pore pressure. Discharge rate of Matsuzaka spring water increases remarkably during snowmelting, heavy rain and rainy season. However, its increase does not balance with increase of water supply into the catchment area. Groundwater should originate from outside of Matsuzaka watershed since the discharge is larger than recharge in the watershed. The rate of flow from Matsuzaka into Numata remains constant throughout the year. Numata drainage wells are effective in draining the water from Matsuzaka. Sodenosawa drainage tunnel mainly drains water from mud stone debris in Shimosawanome subsidence zone and contributes to stabilize the whole 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 22, p. 61-77, 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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