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  1. 学術雑誌掲載済論文
  2. 和雑誌

寒冷地河川における 取水堰上流の晶氷変動現象に関する研究

https://kitami-it.repo.nii.ac.jp/records/8646
cdf095fd-7a52-4e72-a795-8ca932941906
名前 / ファイル ライセンス アクション
2017-03 寒冷地河川における 取水堰上流の晶氷変動現象に関する研究 (778.9 kB)
Item type 学術雑誌論文 / Journal Article(1)
公開日 2018-04-23
タイトル
言語 ja
タイトル 寒冷地河川における 取水堰上流の晶氷変動現象に関する研究
タイトル
言語 en
タイトル FRAZIL SLUSH VARIATION IN TAKE FACILITIES ON ICE-COVERED RIVERS
言語
言語 jpn
キーワード
言語 en
主題Scheme Other
主題 Ice-covered river
キーワード
言語 en
主題Scheme Other
主題 Frazil slush
キーワード
言語 en
主題Scheme Other
主題 Calculation model
キーワード
言語 en
主題Scheme Other
主題 Field observation
キーワード
言語 en
主題Scheme Other
主題 Water Intake facilities
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 open access
アクセス権URI http://purl.org/coar/access_right/c_abf2
その他のタイトル
その他のタイトル FRAZIL SLUSH VARIATION IN TAKE FACILITIES ON ICE-COVERED RIVERS
言語 en
著者 吉川, 泰弘

× 吉川, 泰弘

WEKO 89971
e-Rad 50414149

ja 吉川, 泰弘

Search repository
岡部, 博一

× 岡部, 博一

WEKO 89972

ja 岡部, 博一

Search repository
橋場, 雅弘

× 橋場, 雅弘

WEKO 89973

ja 橋場, 雅弘

Search repository
森田, 共胤

× 森田, 共胤

WEKO 89974

ja 森田, 共胤

Search repository
著者別名
姓名
姓名 Yoshikawa, Yasuhiro
言語 en
著者別名
姓名
姓名 Okabe, Hirokazu
言語 en
著者別名
姓名
姓名 Hashiba, Masahiro
言語 en
著者別名
姓名
姓名 Morita, Tomotsugu
言語 en
抄録
内容記述タイプ Abstract
内容記述 本研究の目的は,取水堰上流における河川縦断方向の晶氷変動現象の解明である.晶氷の発生・輸送・堆積
を考慮した計算モデルを構築した.過去に冬期の取水障害が発生した実河川において,晶氷輸送量および氷板・
晶氷断面積の現地観測を実施した.観測値および計算値に基づき,晶氷変動現象を推定した.結氷は取水堰か
ら始まり,時間の経過とともに上流へと進む.水面で発生および輸送される晶氷は,下流の氷板下に堆積する.
結氷の先端地点の上流に近いほど,晶氷面積は早い段階で急激に増加する.その後,上流の晶氷が下流へと流
れて,下流において晶氷面積が急激に増加する.冬期の取水障害の危険性が高い時期は,結氷の始まりの時期
と,結氷後に上流から晶氷が輸送される時期であることが推察された.
抄録
内容記述タイプ Abstract
内容記述 This study aims to clarify the frazil slush variation mechanisms associated with the water intake facilities of ice-covered rivers. A river ice calculation model was developed to determine the dynamics of frazil slush
generation, transport, and accumulation. Field observations of frazil slush transport, ice sheet and frazil slush cross sections were performed. In the results, The phenomenon in which a river freezes begins from
intake facilities, and it progresses to upstream direction. Frazil slush that is generated upstream accumulates under downstream ice sheets. Frazil slush accumulates more quickly in upstream than downstream. Then, as
upstream frazil slush accumulation begins to flow downstream, it accumulates more quickly in downstream.
書誌情報 ja : 土木学会論文集B1(水工学)

巻 73, 号 4, p. I_1321-I_1326, 発行日 2017
権利
権利情報 c 2017 土木学会
出版者
出版者 土木学会
著者版フラグ
値 publisher
出版タイプ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
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