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沖見地すべりの水文観測(予報)
http://hdl.handle.net/10191/39165
e02d8075-cfac-4f85-b36a-91afe5cf2233
名前 / ファイル | ライセンス | アクション | |
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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 | 沖見地すべりの水文観測(予報) | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | 沖見地すべりの水文観測(予報) | |||||
言語 | ||||||
言語 | jpn | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Okimi landslide | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Hydrology | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Groundwater | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Geochemistry | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Drain | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | :沖見地すべり | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 水文学 | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 地下水 | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 地球化学 | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 排水 | |||||
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 | Preriminary report of Hydrological Investigation in Okimi Landslide, Niigata Prefecture | |||||
著者 |
佐藤, 修
× 佐藤, 修× 丸井, 英明× 渡部, 直喜× 羅, 暁林 |
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著者別名 | ||||||
識別子 | ||||||
識別子 | 161250 | |||||
識別子Scheme | WEKO | |||||
姓名 | ||||||
姓名 | Sato, Osamu | |||||
著者別名 | ||||||
識別子 | ||||||
識別子 | 161251 | |||||
識別子Scheme | WEKO | |||||
姓名 | ||||||
姓名 | Marui, Hideaki | |||||
著者別名 | ||||||
識別子 | ||||||
識別子 | 161252 | |||||
識別子Scheme | WEKO | |||||
姓名 | ||||||
姓名 | Watanabe, Naoki | |||||
著者別名 | ||||||
識別子 | ||||||
識別子 | 161253 | |||||
識別子Scheme | WEKO | |||||
姓名 | ||||||
姓名 | Luo, Xiao Lin | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | The Okimi landslide was divided into A valley (about 12.52 hectares) which included an active A block and B valley (11.35 hectares) which included comparatively steady B block. The amount of drain was measured in each valley and the chemical element included in the drain was analyzed. The amount of drain of A valley was three times B valley though the areas was almost the same as the A valley and the B valley. The outflow of all ions has increased in A valley when the amount of drain increases. There is no change at all ion outflow rate even if the drain increases in B valley. The groundwater which has a constant water quality always springs out in the B valley except miner ions like chloride ions. Increase of amount of drain is caused by adding of thawing water which contains negligible small amount of ions. | |||||
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 18, p. 33-42, 発行日 1997-03 |
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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 |