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Analysis on Dam-Breaking Mode of Tangjiashan Barrier Dam in Beichuan County
  • ISSN号:1672-6316
  • 期刊名称:Journal of Mountain Science
  • 时间:2011.4.15
  • 页码:354-362
  • 分类:P315.727[天文地球—地震学;天文地球—固体地球物理学;天文地球—地球物理学] TV698.1[水利工程—水利水电工程]
  • 作者机构:[1]Faculty of Geosciences and Environmental Engineering, Southwest Jiaotong University, Chengdu 610031, China, [2]State Key Laboratory of Geohazard Prevention and Geoenvironment Protection, Chengdu University of Technology, Chengdu 610059, China, [3]Aseismic Engineering Technology Key Laboratory of Sichuan Province,Southwest Jiaotong University,Chengdu 610031, China, [4]Chengdu Hydroelectric Investigation and Design Institute, China Hydropower Consulting Group, Chengdu 610072, China
  • 相关基金:funding from the National Natural Science Foundation Project (Grant No. 40772175 40972175); the Scientific research fund of Southwest Jiaotong University (Grant No.2008-A01); the Opening Fund of State Key Laboratory of Geohazard Prevention and Geoenvironment Protection (Chengdu University of Technology) (Grant No. DZKJ–08012); the National Natural Science Foundation Project-mutual fund of Yunnan Province (Grant No.U1033601)
  • 相关项目:植被发育斜坡对强降雨过程的地下水响应机制及其灾害效应
中文摘要:

Tangjiashan 山崩是典型 highspeed 媒介陡峭的剧降角度的作为结果的山崩。地震触发的这山崩发生了在关于半分钟。相对滑动排水量是 900 米,因此平均滑动速度每秒是大约 30 米。被高速度的山崩沿着河形成的障碍水坝的纵的长度是 803.4 米;并且最大的宽度十字路口河是 611.8 米。并且它的体积被估计大约 2037 万立方米。通过障碍水坝的详细地质的调查,和在地震前的早地质的信息,当水水平处于状况到达不同举起时,障碍水坝和它在上游、下游的斜坡的稳定性的地质的结构被学习在有 7 或 8 Richter 规模的地震紧张的震动以后不断。在这个基础上,障碍水坝的打破水坝的模式深深地被讨论。从而,分析结果提供重要指导,到 Tangjiashan 障碍的前面总部的忠告建水坝,以便一些合适的工程措施能被实现并且泛滥分泌物能被执行很好。

英文摘要:

Tangjiashan landslide is a typical high-speed consequent landslide of medium-steep dip angle. This landslide triggered by earthquake took place in about semi-minute. The relative sliding displacement is 900 meters, so average sliding speed is about 30 meters per second. The longitudinal length of barrier dam which is formed by high-speed landslide along river is 803.4 meters; and maximum width crossing river is 611.8 meters. And its volume is estimated about 20.37 million steres. Through detailed geological investigation of the barrier dam, together with early geological information before earthquake, geological structures of the barrier dam and its stability of upstream and downstream slopes are studied when water level reaches different elevations in condition of continual after shocks with seismic intensity of 7 or 8 Richter scale. On this basis, dam-breaking mode of barrier dam is discussed deeply. Thereby, analytic results provide significant guidance and advices to front headquarters of Tangjiashan barrier dam, so that some proper engineering measures can be implemented and flood discharge can be carried out well.

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期刊信息
  • 《山地科学学报:英文版》
  • 主管单位:
  • 主办单位:中国科学院山地灾害与环境研究所
  • 主编:
  • 地址:四川成都一环路南二段16号
  • 邮编:610041
  • 邮箱:yudf@imde.ac.cn
  • 电话:028-85252110 85252044
  • 国际标准刊号:ISSN:1672-6316
  • 国内统一刊号:ISSN:51-1668/P
  • 邮发代号:
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  • 英国农业与生物科学研究中心文摘,荷兰文摘与引文数据库,美国地质文献预评数据库,美国剑桥科学文摘,美国科学引文索引(扩展库)
  • 被引量:84