WEKO3
アイテム
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低温室にできた氷柱の結晶構造
http://hdl.handle.net/10191/39202
http://hdl.handle.net/10191/392022bc61ae2-c99e-40fb-b047-3a52a26c5eae
名前 / ファイル | ライセンス | アクション |
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20_137-142.pdf (797.3 kB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2016-03-08 | |||||
タイトル | ||||||
タイトル | 低温室にできた氷柱の結晶構造 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | 低温室にできた氷柱の結晶構造 | |||||
言語 | ||||||
言語 | jpn | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | ice pillar | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | ice stalagmite | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | icicle | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Structure of ice crystals | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | growth processes | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 氷柱 | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 水筍 | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | つらら | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 結晶構造 | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 成長過程 | |||||
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 | Structure of the ice pillar in the cold room | |||||
著者 |
竹内, 由香里
× 竹内, 由香里× 前田, 直哉× 永崎, 智晴× 山田, 英樹× 王, 昕× 佐藤, 真理子 |
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著者別名 | ||||||
識別子 | 161164 | |||||
識別子Scheme | WEKO | |||||
姓名 | Takeuchi, Yukari | |||||
著者別名 | ||||||
識別子 | 161165 | |||||
識別子Scheme | WEKO | |||||
姓名 | Maeda, Naoya | |||||
著者別名 | ||||||
識別子 | 161166 | |||||
識別子Scheme | WEKO | |||||
姓名 | Nagasaki, Tomoharu | |||||
著者別名 | ||||||
識別子 | 161167 | |||||
識別子Scheme | WEKO | |||||
姓名 | Yamada, Hideki | |||||
著者別名 | ||||||
識別子 | 161168 | |||||
識別子Scheme | WEKO | |||||
姓名 | Wang, Xin | |||||
著者別名 | ||||||
識別子 | 161169 | |||||
識別子Scheme | WEKO | |||||
姓名 | Sato, Mariko | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | Ice pillar, which means ice stalagmite linked to icicle in this paper, was formed in the cold room and the height of it was 185 cm. The growth processes of the ice pillar were estimated from the ice structures in the horizontal and vertical cross sections. The whole ice pillar consists of many ice crystals. Judging from the discontinuity of the ice structure, it can be presumed that the lower part of the ice pillar which had grown upward were linked to the upper part which had grown downward at around 170cm high. Either parts has different ice structure from the natural ice stalagmite or icicle, because too much water dropped intermittently and the air temperature in the cold room was too low during the ice pillar grew. | |||||
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 20, p. 137-142, 発行日 1999-03 |
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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 |