›› 2018, Vol. 39 ›› Issue (7): 2424-2432.doi: 10.16285/j.rsm.2017.2330

• 基础理论与实验研究 • 上一篇    下一篇

跨越走滑断层黏土地层动力响应离心机试验研究

蔡奇鹏1,吴宏伟2,胡 平3,陈星欣1,李升才1   

  1. 1. 华侨大学 土木工程学院,福建 厦门 361021;2. 香港科技大学 土木与环境工程系,香港;3. 北京市地震局,北京 100080
  • 收稿日期:2017-11-27 出版日期:2018-07-10 发布日期:2018-08-05
  • 作者简介:蔡奇鹏,男,1982年生,博士,副教授,主要从事岩土与地下工程的研究工作。
  • 基金资助:

    国家自然科学基金资助项目(No. 51778249);华侨大学中青年教师科研提升资助计划(No. ZQN-PY216);厦门市科技计划项目 (No. 3502Z20172011)。

Centrifuge experimental study of of dynamic responses of clay stratum overlying a strike-slip fault

CAI Qi-peng1, CHARLES W W Ng 2, HU Ping3, CHEN Xing-xin1, LI Sheng-cai1   

  1. 1. College of Civil Engineering, Huaqiao University, Xiamen, Fujian 361021, China; 2. Department of Civil and Environmental Engineering, Hong Kong University of Science and Technology, Hong Kong, China; 3. Earthquake Administration of Beijing Municipality, Beijing 100080, China
  • Received:2017-11-27 Online:2018-07-10 Published:2018-08-05
  • Supported by:

    This work was supported by the National Natural Science Foundation of China (51778249), the Promotion Program for Young and Middle-aged Teacher in Science and Technology Research of Huaqiao University (ZQN-PY216), the Scientific and Technological Planning Project of Xiamen City (3502Z20172011).

摘要: 地震中基岩走滑断层活动引起跨断层地下结构物破坏,上覆土层的非一致响应机制尚不明确,隐伏裂缝影响规律认识不足。基于可模拟走滑断层活动的层状剪切箱,针对黏土地层展开两个离心机振动台试验,对比上覆土体中隐伏裂缝的影响。试验结果表明,当地层中不存在隐伏裂缝时,基岩走滑断层错动对两盘地层的非一致振动的影响不显著。当地层中存在隐伏裂缝,错动盘一侧土体的振动加速度幅值随振动循环次数的增加逐渐减小,固定盘和错动盘两侧土体出现非一致振动响应,固定盘一侧土体产生的超静孔压大于错动盘一侧。隐伏裂缝对土体非一致振动响应的影响范围受限于其在地层中的分布范围,探明隐伏裂缝上断点的埋深具有重要工程意义。

关键词: 土工离心机, 振动台试验, 走滑断层, 隐伏裂缝, 动力响应

Abstract: Underground structures are severely damaged when subjected to strike-slip faulting during an earthquake. Mechanism behind inconsistent dynamic responses in soil stratum is not yet fully understood. The influence of pre-existing fracture in soil stratum on the dynamic response of the soil is still not clear. Based on a newly designed laminar box with simulation of strike-slip fault, two dynamic centrifuge tests were conducted on clay stratum to investigate the influences of the pre-existing fracture. Centrifuge test results show that inconsistent dynamic responses for the soil crossing bedrock fault is not obvious when there is no pre-existing fracture. With a pre-existing fracture, however, the magnitude of seismic wave at the moving block decreases with time during shaking. Inconsistent dynamic responses between the stationary and moving blocks are then observed. In addition, the excess pore water pressures developed at the stationary block are larger than what are observed at the moving block. The effects of distribution of the pre-existing fracture on the inconsistent dynamic responses in the soil stratum are also demonstrated. It is of significant importance to identify the tip depth of the pre-existing fracture in soil stratum.

Key words: geotechnical centrifuge, shaking table test, strike-slip fault, preexisting fracture, dynamic response

中图分类号: 

  • TU 45

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