论文部分内容阅读
The great Wenchuan earthquake(Ms = 8.0) in 2008 caused severe damage in the western part of the Chengdu Plain.Soil liquefaction was one of the major causes of damage in the plain areas,and proper evaluation of liquefaction potential is important in the defi nition of the seismic hazard facing a given region and post-earthquake reconstruction.In this paper,a simplifi ed procedure is proposed for liquefaction assessment of sandy deposits using shear wave velocity(Vs),and soil liquefaction from the Banqiao School site was preliminarily investigated after the earthquake.Boreholes were made at the site and shear wave velocities were measured both by SASW and down-hole methods.Based on the in-situ soil information and Vs profi les,the liquefaction potential of this site was evaluated.The results are reasonably consistent with the actual fi eld behavior observed after the earthquake,indicating that the proposed procedure is effective.The possible effects of gravel and fi nes contents on liquefaction of sandy soils were also brie? y discussed.
The great Wenchuan earthquake (Ms = 8.0) in 2008 caused severe damage in the western part of the Chengdu Plain.Soil liquefaction was one of the major causes of damage in the plain areas, and proper evaluation of liquefaction potential is important in the definition of the seismic hazard facing a given region and post-earthquake reconstruction.In this paper, a simplifi ed procedure is proposed for liquefaction assessment of sandy deposits using shear wave velocity (Vs), and soil liquefaction from the Banqiao School site was preliminarily investigated after the earthquake.Boreholes were made at the site and shear wave velocities were measured both by SASW and down-hole methods. Based on the in-situ soil information and Vs profi les, the liquefaction potential of this site was was. The results are reasonably consistent with the actual fi eld behavior observed after the earthquake, indicating that the proposed procedure is effective. possible effects of gravel and fi nes contents on lique faction of sandy soils were also brie? y discussed.