Journal of Shanghai Jiaotong University ›› 2011, Vol. 45 ›› Issue (05): 696-700.

• Architechural Science • Previous Articles     Next Articles

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

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

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