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六郷扇状地における地下水人工滴養の実施と成果
http://hdl.handle.net/10295/1145
http://hdl.handle.net/10295/1145a00a99a1-b246-4b38-bbc7-272051519a60
名前 / ファイル | ライセンス | アクション |
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Item type | 学術雑誌論文 / Journal Article(1) | |||||||||
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公開日 | 2008-09-22 | |||||||||
タイトル | ||||||||||
タイトル | 六郷扇状地における地下水人工滴養の実施と成果 | |||||||||
言語 | ja | |||||||||
タイトル | ||||||||||
タイトル | Experience of Artificial Recharge of Ground Water in the Rokugo Alluvial Fan, Akita Prefecture | |||||||||
言語 | en | |||||||||
言語 | ||||||||||
言語 | jpn | |||||||||
主題 | ||||||||||
言語 | ja | |||||||||
主題Scheme | Other | |||||||||
主題 | 六郷扇状地 | |||||||||
主題 | ||||||||||
言語 | ja | |||||||||
主題Scheme | Other | |||||||||
主題 | 地下水人工滴養 | |||||||||
主題 | ||||||||||
言語 | ja | |||||||||
主題Scheme | Other | |||||||||
主題 | 帯水層 | |||||||||
主題 | ||||||||||
言語 | ja | |||||||||
主題Scheme | Other | |||||||||
主題 | 水理水頭 | |||||||||
主題 | ||||||||||
言語 | ja | |||||||||
主題Scheme | Other | |||||||||
主題 | 地下水温 | |||||||||
資源タイプ | ||||||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||||||
資源タイプ | journal article | |||||||||
アクセス権 | ||||||||||
アクセス権 | open access | |||||||||
アクセス権URI | http://purl.org/coar/access_right/c_abf2 | |||||||||
作成者 |
肥田, 登
× 肥田, 登
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内容記述 | ||||||||||
内容記述タイプ | Abstract | |||||||||
内容記述 | The Rokugo alluvial fan lies around 39' 25' Nand 140' 34' E in northern Japan. The distance between the proximal fan at 90 meters above sea level and the distal fan at 45 meters is about four kilometers. The unconfined aquifer of the fan consists mainly of gravel and sand. Four artificial recharge basins were constructed on the central part of the fan. Observation instruments are wells and piezometers installed in depths of 20 m and 50 m. In this paper, the author discusses the effects of artificial recharge using the basin No.2 at the center of the fan. The recharge experience was done during the period when ground water level was affected by melting snow, from April 8 to May 2, 1998. Results obtained are as follows: first, artificial recharging caused a rise in the hydraulic head, which was related to the Rokugo town area situated on the distal fan, and second, because the author supplied the basin No.2 with water with a low water temperature after snow melted, the characteristic phenomenon of ground water temperature was recorded by piezometers in a depth of 20 m at both sites of central and distal fan. Consideration of this point is a theme for future studies. As a synthetic judgment, the artificial recharge of ground water contributes to sustainable aquifer management in the alluvial fan. | |||||||||
言語 | en | |||||||||
内容記述 | ||||||||||
内容記述タイプ | Other | |||||||||
出版タイプ | ||||||||||
出版タイプ | VoR | |||||||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||||||
書誌情報 |
ja : 地学雑誌 巻 116, 号 1, p. 23-30, 発行日 2007-01-01 |
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収録物識別子 | ||||||||||
収録物識別子タイプ | ISSN | |||||||||
収録物識別子 | 0022135X | |||||||||
収録物識別子 | ||||||||||
収録物識別子タイプ | NCID | |||||||||
収録物識別子 | AN00322536 | |||||||||
出版者 | ||||||||||
出版者 | 東京地学協会 | |||||||||
言語 | ja |