WEKO3
アイテム
16. 櫻島噴火に伴ふ鳴動及び噴煙
https://doi.org/10.15083/0000034306
https://doi.org/10.15083/0000034306c3998181-ddf0-4e98-aeff-6103cc004efc
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
ji0241016.pdf (514.3 kB)
|
|
| Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
|---|---|---|---|---|---|---|
| 公開日 | 2008-06-06 | |||||
| タイトル | ||||||
| タイトル | 16. 櫻島噴火に伴ふ鳴動及び噴煙 | |||||
| 言語 | ja | |||||
| 言語 | ||||||
| 言語 | jpn | |||||
| 資源タイプ | ||||||
| 資源 | http://purl.org/coar/resource_type/c_6501 | |||||
| タイプ | departmental bulletin paper | |||||
| ID登録 | ||||||
| ID登録 | 10.15083/0000034306 | |||||
| ID登録タイプ | JaLC | |||||
| その他のタイトル | ||||||
| その他のタイトル | 16. Detonation and Smoke that Accompanied the Eruption of Sakura-jima | |||||
| 著者 |
永田, 武
× 永田, 武× 川野, 實× 大林, 辰藏 |
|||||
| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 133384 | |||||
| 姓名 | Nagata, Takesi | |||||
| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 133385 | |||||
| 姓名 | Kawano, Minoru | |||||
| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 133386 | |||||
| 姓名 | Obayashi, Tatuzo | |||||
| 著者所属 | ||||||
| 著者所属 | 地震研究所 | |||||
| 著者所属 | ||||||
| 著者所属 | 地球物理學敎室 | |||||
| 抄録 | ||||||
| 内容記述タイプ | Abstract | |||||
| 内容記述 | In March 1946, Sakura-jima erupted with a large detonation, and smoke shooted up in the sky. Detonation in the end of March was the most intense ones, it became feeble gradually. The change in volume ejected smoke was nearly equal to the intensity of detonation. There was a distinct shortperiod of variation, 4～6 minutes in average period. Comparing the result of observation of tilting motion of ground by means of the spirit level with the strength of detonation, we found that there were some correlation between those two quantities. On the other hand, we observe 1 that the ejected smoke consistes with two斌inds of vortex. One of them is the horizontal vortex caused by the .Corioll's force of the earth, while the other is the vertical one which is hydrodynamically caused. From the observed values of vorticities of the latter type, we estimate the initial velocity of ejection of smoke from the crater, the result being that it was about 55m/sec. On the other hand, the initial velocity of ejection of volcanic bombs was also estimated from its flying pathes, the result just agreeing with that estimate from the vorticites. Then, the pressure of gas at the time of ejection was estimated to be about 18 atm., under the assumption ""momentum conservation"" in the case of ejection, of bombs. While from the pressure equation of compressible fluid, we can observe relation between the gas pressure into the above-mentioned equation and its density. Putting P 18 atm., we get that the density of volcanic smoke at the crater is about 0.05. | |||||
| 書誌情報 |
東京大學地震研究所彙報 = Bulletin of the Earthquake Research Institute, University of Tokyo 巻 24, 号 1-4, p. 201-206, 発行日 1948-06-30 |
|||||
| ISSN | ||||||
| 収録物識別子タイプ | ISSN | |||||
| 収録物識別子 | 00408972 | |||||
| 書誌レコードID | ||||||
| 収録物識別子タイプ | NCID | |||||
| 収録物識別子 | AN00162258 | |||||
| フォーマット | ||||||
| 内容記述タイプ | Other | |||||
| 内容記述 | application/pdf | |||||
| 日本十進分類法 | ||||||
| 主題Scheme | NDC | |||||
| 主題 | 453 | |||||
| 出版者 | ||||||
| 出版者 | 東京大学地震研究所 | |||||
| 出版者別名 | ||||||
| Earthquake Research Institute, University of Tokyo | ||||||
