KMS Institute of Mountain Hazards and Environment,CAS
| 半成岩地层库岸变形破坏过程 | |
| Alternative Title | THE PROCESS OF THE-RESERVOIR-BANK DEFORMATION DESTRUCTION IN SEMI-SOLID ROCK |
| Language | 中文 |
| 王成华; 黄大庭 | |
| 1991-05 | |
| Source Publication | 国际滑坡与岩土工程学术会议论文集 Ⅱ |
| Author of Source | 朱瑞赓等主编 |
| Pages | 1-7 |
| meeting | 国际滑坡与岩土工程学术会议论文集 |
| Conference Date | 1991-5-21～23 |
| Conference Place | 武汉 |
| Country | 中国 |
| Publication Place | 武汉 |
| Publisher | 华中理工大学出版社 |
| Contribution Rank | 1 |
| Abstract | 本文以黄河上游某水库为例，从半成岩库岸特征介绍入手，以水库运行初期库岸变形破坏现状为依据，分析论述了在水库运行初期，库岸的破坏方式以崩塌为主，次为中小型滑坡；库水位上升到正常高水位以后，库岸破坏的方式将转为中小型滑坡为主，偶有大型滑坡发生。库水位上升过程中，库岸变形破坏加剧，并塑造水下阶状岸坡雏形，水位下降过程中，库岸变形破坏过程的地质模型。 |
| Other Abstract | Taking some riservoir at the upper reaches of the Huang River as example, this paper denlt with the deformation destruction of the reservoir-bank in the starting running of the reservoir based on the characteristics of semi-solid rock, deformation data and ground-water observation of the reservoir-bank. The forms deformation desiruction are maimly collapse, secondly median and small scale landslides, without large and massive scale landslides. While the Water level rising to the normal level, the forms of deformation destruction Would turn into sedinn-small scale landslides, and the large or massive scale landslides occur by accidend. In the rising process of the water level, the deformation destruction of the reservoir-bank was aggravated and formed the subaqueous reservoir-bank embryo like ladder; and in the dropping process of the water level, the deformation destruction was weakened. The action of hydrodynamic pressure caused water sliding of the subaqueous reservoir bank so as to form subaqueous reservoir-bank like ladder. As a result, the geologic pattern of the evolution process for reservoir-bank deformation destruction in the starting running of the reservoir is built. |
| Keyword | 半成岩地层 库岸变形 滑坡 黄河上游 |
| ISBN | 7-5609-0597-8 |
| Indexed By | 其他 |
| Document Type | 会议论文 |
| Identifier | http://ir.imde.ac.cn/handle/131551/26455 |
| Collection | 成都山地所知识仓储（2009年以前） |
| Corresponding Author | 王成华 |
| Affiliation | 中国科学院水利部成都山地灾害与环境研究所 |
| First Author Affilication | 中国科学院水利部成都山地灾害与环境研究所 |
| Corresponding Author Affilication | 中国科学院水利部成都山地灾害与环境研究所 |
| Recommended Citation GB/T 7714 | 王成华,黄大庭. 半成岩地层库岸变形破坏过程[C]//朱瑞赓等主编. 武汉:华中理工大学出版社,1991:1-7. |
| Files in This Item: | ||||||
| File Name/Size | DocType | Version | Access | License | ||
| 半成岩地层库岸变形破坏过程 1-7.p（1167KB） | 会议论文 | 开放获取 | CC BY-NC-SA | View Application Full Text | ||
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