WEKO3
アイテム
EFFECTS OF UPLIFT ON THE DEVELOPMENT OF EXPERIMENTAL EROSION LANDFORM STARTED WITH A FLAT-TOPPED SQUARE SAND MOUND
https://doi.org/10.24789/00001235
https://doi.org/10.24789/00001235e1a78853-d33d-4af2-8b44-9d88f9b804fb
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
本文を見る(PDFファイル) (716.2 kB)
|
|
| Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||||
|---|---|---|---|---|---|---|---|---|
| 公開日 | 2012-10-01 | |||||||
| タイトル | ||||||||
| タイトル | EFFECTS OF UPLIFT ON THE DEVELOPMENT OF EXPERIMENTAL EROSION LANDFORM STARTED WITH A FLAT-TOPPED SQUARE SAND MOUND | |||||||
| 言語 | en | |||||||
| 言語 | ||||||||
| 言語 | eng | |||||||
| 資源タイプ | ||||||||
| 資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||||
| 資源タイプ | departmental bulletin paper | |||||||
| ID登録 | ||||||||
| ID登録 | 10.24789/00001235 | |||||||
| ID登録タイプ | JaLC | |||||||
| 著者 |
OUCHI, Shunji
× OUCHI, Shunji
|
|||||||
| 著者別名 | ||||||||
| 識別子Scheme | WEKO | |||||||
| 識別子 | 23452 | |||||||
| 姓名 | 大内, 俊二 | |||||||
| 抄録 | ||||||||
| 内容記述タイプ | Abstract | |||||||
| 内容記述 | Two runs of rainfall erosion experiment (one with and another without uplift) are conducted to see the effect of uplift on the development of experimental erosion landform started with a flat-topped square mound. In the first stage of erosion, valley incision and the development of a valley system proceed rapidly regardless of the uplift. The uplift then works to increase the surface relief, while the accelerated erosion keeps the average height at nearly the same level against the uplift. This suggests that the flux steady-state can be achieved while mountains are growing. The ridge tops, where the erosion is not accelerated by the uplift, move up with the uplift, while the accelerated erosion on main valley floors keeps the lowest elevation despite the uplift. As a result, overall relief increased with uplift. The increased sediment supply with uplift encourages the development of alluvial fans, which controls the local base levels, and causes some rise of lower valley floors. The residuals of the increased relief and raised lower valley floors remain longafter the end of uplift. The identical changes of H’ in both runs indicate the lack of significant effect of the uplift on the relief characteristics. The uplift does not change the manner of landform development with time, but it increases the magnitude of surface relief throughout the process. | |||||||
| 内容記述 | ||||||||
| 内容記述タイプ | Other | |||||||
| 内容記述 | 【査読有】 | |||||||
| 書誌情報 |
中央大学理工学研究所論文集 巻 10, p. 85-97, 発行日 2005-03-31 |
|||||||
| 出版者 | ||||||||
| 出版者 | 中央大学理工学研究所 | |||||||
| ISSN | ||||||||
| 収録物識別子タイプ | ISSN | |||||||
| 収録物識別子 | 1343-0068 | |||||||
| 権利 | ||||||||
| 権利情報 | この資料の著作権は、資料の著作者または学校法人中央大学に帰属します。著作権法が定める私的利用・引用を超える使用を希望される場合には、掲載誌発行部局へお問い合わせください。 | |||||||
| フォーマット | ||||||||
| 内容記述タイプ | Other | |||||||
| 内容記述 | application/pdf | |||||||
| 著者版フラグ | ||||||||
| 出版タイプ | VoR | |||||||
| 出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||||
