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山地小流域の濁度と濁度発生量に関する数値解析
https://kitami-it.repo.nii.ac.jp/records/6806
https://kitami-it.repo.nii.ac.jp/records/680607335a2a-dcb0-432f-a2bd-6433c3925e54
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
4734.pdf (3.5 MB)
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| Item type | 学術雑誌論文 / Journal Article(1) | |||||||||
|---|---|---|---|---|---|---|---|---|---|---|
| 公開日 | 2007-04-17 | |||||||||
| タイトル | ||||||||||
| タイトル | 山地小流域の濁度と濁度発生量に関する数値解析 | |||||||||
| 言語 | ja | |||||||||
| タイトル | ||||||||||
| タイトル | NUMERICAL ANALYSIS OF TURBIDITY AND ITS OCCURANCE IN SMALL MOUNTAINOUS BASIN | |||||||||
| 言語 | en | |||||||||
| 言語 | ||||||||||
| 言語 | jpn | |||||||||
| 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 | |||||||||
| 著者 |
山梨, 光訓
× 山梨, 光訓
× 佐渡, 公明
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| 著者別名 | ||||||||||
| 識別子Scheme | WEKO | |||||||||
| 識別子 | 34350 | |||||||||
| 姓名 | YAMANASHI, Mitsunori | |||||||||
| 言語 | en | |||||||||
| 著者別名 | ||||||||||
| 識別子Scheme | WEKO | |||||||||
| 識別子 | 34351 | |||||||||
| 姓名 | SADO, Kimiteru | |||||||||
| 言語 | en | |||||||||
| 抄録 | ||||||||||
| 内容記述タイプ | Abstract | |||||||||
| 内容記述 | lt is well known that turbidity increases during snowmelt season and storm rainfall of summer season in river flow. Although the reason for the highest degree level of turbidity during snowmelt season is not clear. M. Yamanashi et al. (1995) suggested that the high degree level of turbidity during snowmelt season depends on surface flow on amountainous basin and the turbidity during summer season is mainly caused by a shearing force between river bed and river flow. There is a possibility to analyze runoff mechanism through the observation of turbidity according his suggestion. The maximum snowmelt which is equivalent to rainfall intensity is about 3 to 4 mm/hr. 0n the other hand，such rainfall intensity, 3 to 4 mm/hr during summer season does not cause so high turbidity in river flow. This paper studies the mechanisms of the turbidity increase in mountainous river flow through field observations and theoretical analysis. The conditions of turbidity variation by using turbidity occurrence and also inverse estimation method of turbidity occurrence are clarified under the assumption that soil-water content plays an important role. | |||||||||
| 書誌情報 |
水工学論文集 巻 50, p. 919-924, 発行日 2006-02 |
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| 権利 | ||||||||||
| 権利情報 | 社団法人 土木学会, 山梨光訓, 佐渡公明, 水工学論文集, 50, 2006, 919-924. | |||||||||
| フォーマット | ||||||||||
| 内容記述タイプ | Other | |||||||||
| 内容記述 | application/pdf | |||||||||
| 出版者 | ||||||||||
| 出版者 | 社団法人 土木学会 | |||||||||
| 言語 | ja | |||||||||
| 著者版フラグ | ||||||||||
| 言語 | en | |||||||||
| 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 | |||||||||
