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このアイテムのファイル:
| ファイル | 記述 | サイズ | フォーマット | |
|---|---|---|---|---|
| sgk00600_107.pdf | 279.75 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 | HIRANO, Toshiyuki | en |
| dc.date.accessioned | 2013-08-30T06:36:17Z | - |
| dc.date.available | 2013-08-30T06:36:17Z | - |
| dc.date.issued | 1966-12 | - |
| dc.identifier.issn | 0454-7837 | - |
| dc.identifier.uri | http://hdl.handle.net/2433/178513 | - |
| dc.description.abstract | The dilution area of effluent is sometimes identified by its colored water spread on the sea surface. On the basis of the number of observations, the relationship between the volume of effluent and its dilution area had been introduced as the empirical formula (Nitta (1963)). The author discussed the formation of dilution area of effluent from the viewpoint of the entry mixing. Consequently, a formula explaining the relationship between the volume of effluent and its dilution area, was obtained and compared with the empirical one. | en |
| dc.format.mimetype | application/pdf | - |
| dc.language.iso | eng | - |
| dc.publisher | Geophysical Institute, Kyoto University | en |
| dc.subject.ndc | 450 | - |
| dc.title | ON THE DILUTION AREA OF EFFLUENT IN THE SEA | en |
| dc.type | departmental bulletin paper | - |
| dc.type.niitype | Departmental Bulletin Paper | - |
| dc.identifier.ncid | AA00423961 | - |
| dc.identifier.jtitle | Special Contributions of the Geophysical Institute, Kyoto University | en |
| dc.identifier.volume | 6 | - |
| dc.identifier.spage | 107 | - |
| dc.identifier.epage | 112 | - |
| dc.textversion | publisher | - |
| dc.sortkey | 14 | - |
| dcterms.accessRights | open access | - |
| dc.identifier.pissn | 0454-7837 | - |
| 出現コレクション: | No.6 | |
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