WEKO3
アイテム
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長岡地区地下水の流動状況の地球化学的研究
http://hdl.handle.net/10191/39125
http://hdl.handle.net/10191/3912550e96e14-e955-4d49-b08c-b0600fd6b30e
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 | 長岡地区地下水の流動状況の地球化学的研究 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | 長岡地区地下水の流動状況の地球化学的研究 | |||||
言語 | ||||||
言語 | jpn | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | ground water | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | geochemistry | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | recharge | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Nagaoka | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | tritium | |||||
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 | 涵養 | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 長岡 | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | トリチウム | |||||
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 | Geochemical study of Ground Water Recharge and Movement in Nagaoka Area. | |||||
著者 |
佐藤, 修
× 佐藤, 修× 鈴木, 幸治× 青木, 滋 |
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著者別名 | ||||||
識別子 | 161471 | |||||
識別子Scheme | WEKO | |||||
姓名 | Sato, Osamu | |||||
著者別名 | ||||||
識別子 | 161472 | |||||
識別子Scheme | WEKO | |||||
姓名 | Suzuki, Koji | |||||
著者別名 | ||||||
識別子 | 161473 | |||||
識別子Scheme | WEKO | |||||
姓名 | Aoki, Shigeru | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | Ground waters are sampled from observation wells bored to measure ground water levels in Nagaoka and its outskirts. The water samples are analized for major ions and tritium concentrations. The analysis indicates 4 main aquifers (I, II, Ⅲ, IV) in an investigation area. Age of ground water in the aquifer I estimated from tritium concentration is youngest and ages of other aquifers become older with depth. The ground water in aquifer Ⅲ is recharged from rainfalls containing a large amount of tritium supplied since 1952 by the detonation of thermonuclear devices explosion in the atmosphere. The aquifer Ⅱ from which water using for snow melt is mainly pumped up is recharged from upperstream and infiltration in eastern mountain foot and partly recharged from river water of the Shinano river. | |||||
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 12, p. 45-55, 発行日 1991-03 |
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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 |