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Surfacewater-groundwater interaction in the Heihe River basin, Northwestern China
http://hdl.handle.net/2261/54883
http://hdl.handle.net/2261/5488345a6ed46-8625-4198-866b-84a914df9a1c
| Item type | 学術雑誌論文 / Journal Article(1) | |||||
|---|---|---|---|---|---|---|
| 公開日 | 2013-06-14 | |||||
| タイトル | ||||||
| タイトル | Surfacewater-groundwater interaction in the Heihe River basin, Northwestern China | |||||
| 言語 | ||||||
| 言語 | eng | |||||
| 資源タイプ | ||||||
| 資源 | http://purl.org/coar/resource_type/c_6501 | |||||
| タイプ | journal article | |||||
| アクセス権 | ||||||
| アクセス権 | metadata only access | |||||
| アクセス権URI | http://purl.org/coar/access_right/c_14cb | |||||
| 著者 |
Akiyama, Tomohiro
× Akiyama, Tomohiro× Sakai, Akiko× Yamazaki, Yusuke× Wang, Genxu× Fujita, Koji× Nakawo, Masayoshi× Kubota, Jumpei× Konagaya, Yuki |
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| 著者所属 | ||||||
| 著者所属 | Graduate School of Environmental Studies, Nagoya University | |||||
| 著者所属 | ||||||
| 著者所属 | Research Institute for Humanity and Nature | |||||
| 著者所属 | ||||||
| 著者所属 | Institute of Agriculture, Kyoto University | |||||
| 著者所属 | ||||||
| 著者所属 | Cold and Arid Regions Environmental and Engineering Research Institute | |||||
| 著者所属 | ||||||
| 著者所属 | College of Earth and Environment Sciences, Lanzhou University | |||||
| 著者所属 | ||||||
| 著者所属 | National Museum of Ethnology | |||||
| 抄録 | ||||||
| 内容記述タイプ | Abstract | |||||
| 内容記述 | River discharge and groundwater level data were collected in the Heihe River basin, which is the second largest inland river in Northwestern China. The surfacewater-groundwater interaction, particularly in the lower desert reaches, was analyzed with the help of isotope data of water collected from the river. In the non-irrigation period, river water, which originated from the groundwater in the middle oasis reaches, was present throughout the period in the lower desert reaches. During this period, the river water recharged the groundwater not only in the riparian forest region located near the river but also in the desert-riparian fringe region located farther away from the river. In the irrigation period, the river was usually dried up in the lower desert reaches. The river water in the lower reaches appeared just after short-term releases from the middle reaches; the groundwater level in the riparian forest region rose rapidly, but it declined again just after the short-term releases finished. Since the mixing ratio of the short-term released discharge to the groundwater in the desert-riparian fringe region was smaller than that in the riparian forest region, the short-term released discharge did not contribute to the groundwater recharge in the desert-riparian fringe region. | |||||
| 内容記述 | ||||||
| 内容記述タイプ | Other | |||||
| 内容記述 | 本文フィルはリンク先を参照のこと | |||||
| 書誌情報 |
Bulletin of Glaciological Research 巻 24, p. 87-94, 発行日 2007 |
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| ISSN | ||||||
| 収録物識別子タイプ | ISSN | |||||
| 収録物識別子 | 1345-3807 | |||||
| ISSN | ||||||
| 収録物識別子タイプ | ISSN | |||||
| 収録物識別子 | 1884-8044 | |||||
| 権利 | ||||||
| 権利情報 | (c) Japanese Society of Snow and Ice | |||||
| 著者版フラグ | ||||||
| 値 | author | |||||
| 出版者 | ||||||
| 出版者 | Japanese Society of Snow and Ice | |||||
| 関係URI | ||||||
| 識別子タイプ | URI | |||||
| 関連識別子 | http://www.seppyo.org/bgr/vol24 | |||||
| 関係URI | ||||||
| 識別子タイプ | URI | |||||
| 関連識別子 | http://www.seppyo.org/bgr/pdf/24/BGR24p87.pdf | |||||
