上海交通大学学报(自然版) ›› 2011, Vol. 45 ›› Issue (05): 696-700.

• 建筑科学 • 上一篇    下一篇

地脉动法在黄土地区S波速度构造探测中的应用

吴志坚1,2,曾立峰1,王兰民1,2,于凯3,陈拓1   

  1. (1.中国地震局兰州地震研究所 黄土地震工程开放实验室, 兰州 730000;2.中国地震局地震预测研究所 兰州创新基地, 兰州 730000;3.上海交通大学 船舶海洋与建筑工程学院, 上海 200030)
  • 收稿日期:2010-10-17 出版日期:2011-05-30 发布日期:2011-05-30
  • 基金资助:

    中国地震局地震预测研究所基本科研业务费资助项目(2010A76),国家自然科学基金项目(40902094,40974070)

Application of Microtremor Method in Shear Wave Velocity  Structure Survey at Loess Regions

 WU  Zhi-Jian-1, 2 , ZENG  Li-Feng-1, WANG  Lan-Min-1, 2 , YU  Kai-3, CHEN  Tuo-1   

  1. 1. Open Laboratory of Loess Earthquake Engineering, Lanzhou Institute of Seismology, China Earthquake Administration, Lanzhou 730000, China; 2. Lanzhou Innovation Base of Institute of  Earthquake Science, China Earthquake Administration, Lanzhou 730000, China; 3. School of Naval Architecture, Ocean and Civil Engineering, Shanghai Jiaotong University, Shanghai 200030, China)
  • Received:2010-10-17 Online:2011-05-30 Published:2011-05-30

摘要: 在我国西部典型黄土地区分别进行连续和高密度(25 m×25 m)的地脉动观测,并分析所采集的信号,探讨了地脉动信号的时间稳定性及空间分布规律,利用地脉动水平和垂直方向(H/V)频谱反演地下黄土层的剪切波速度剖面,并与已有的钻孔波速资料进行对比.结果表明:内陆地区的地脉动信号具有良好的时间稳定性;在黄土覆盖场地,利用地脉动测试以获取地下剪切波速度构造的方法具有较好的适应性.

关键词: 地脉动, 黄土, 剪切波速度剖面, 水平和垂直方向(H/V)频谱分析

Abstract: Based on continuous microtremor survey and highdensity microtremor survey respectively at the typical loess areas in the west of China, the time stability and space distribution of microtremor data were studied. The shear wave velocity profile of underground loess layer was obtained using the inversion method of H/V frequency spectrum of microtremor, and contrasting the existing wave velocity data of borehole at this region as well. The results show that the microtremor signal is stable in time range at inland areas of China, and microtremor survey is available and effective for obtaining underground shear wave velocity profile at deep loess sediment ground.

Key words: microtremor, loess, shear wave velocity profile, H/V frequency spectrum analysis

中图分类号: