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| ファイル | 記述 | サイズ | フォーマット | |
|---|---|---|---|---|
| cgk01400_001.pdf | 445.74 kB | Adobe PDF | 見る/開く |
完全メタデータレコード
| DCフィールド | 値 | 言語 |
|---|---|---|
| dc.contributor.author | YANAGI, Tetsuo | en |
| dc.date.accessioned | 2013-09-02T04:42:15Z | - |
| dc.date.available | 2013-09-02T04:42:15Z | - |
| dc.date.issued | 1974-12 | - |
| dc.identifier.uri | http://hdl.handle.net/2433/178651 | - |
| dc.description.abstract | The dispersion phenomena due to the tidal current are studied in a hydraulic model. A semidiurnal tide is provided for the model of Mikawa Bay, with horizontal and vertical scales of 1/2000 and 1/160, respectively. Effects of density stratification and wind are not considered. The diffusion of dyed water discharged continuously from a point source is investigated by a dye concentration analysis. Patterns of dye spreading are highly affected by the tidal residual flow. The one-dimensional diffusivity calculated from the distribution of the dye concentration is about 2.7 x 10^5 cm2/sec in Mikawa Bay. It is in the same order as that of the dispersion coefficient due to the tidal residual flow. | en |
| dc.format.mimetype | application/pdf | - |
| dc.language.iso | eng | - |
| dc.publisher | Geophysical Institute, Kyoto University | en |
| dc.subject.ndc | 450 | - |
| dc.title | DISPERSION DUE TO THE RESIDUAL FLOW IN THE HYDRAULIC MODEL | en |
| dc.type | departmental bulletin paper | - |
| dc.type.niitype | Departmental Bulletin Paper | - |
| dc.identifier.ncid | AA00617516 | - |
| dc.identifier.jtitle | Contributions of the Geophysical Institute, Kyoto University | en |
| dc.identifier.volume | 14 | - |
| dc.identifier.spage | 1 | - |
| dc.identifier.epage | 10 | - |
| dc.textversion | publisher | - |
| dc.sortkey | 02 | - |
| dcterms.accessRights | open access | - |
| 出現コレクション: | No.14 | |
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