川藏铁路风沙动力响应特征

K. Han, Chun-xiao Xue
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引用次数: 0

摘要

为了减少川藏铁路沿线风沙液化的危害,采用振动台试验对研究区饱和风沙的动力响应特性进行了研究。结果表明:研究区饱和风积砂的宏观特征为沉降、水流和断裂;位移时程表明,地表位移随输入地震动加速度的增大而增大。当加速度较小时(0.1g),土层振动有明显的自下而上连续放大的趋势。随着加速度的增大(0.2g),放大趋势基本消失。当加速度增加到0.3g时,地震动先增大后减小。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Dynamic Response Characteristics of Aeolian Sediment along Sichuan-Tibet Railway
In order to reduce the damage of liquefaction of aeolian sand along the Sichuan-Tibet railway, the dynamic response characteristics of saturated aeolian sand in the study area were discussed by using shaking table test. The results show that the macroscopic characteristics of saturated aeolian sand in the study area are subsidence, water flow and fracture. The displacement time history shows that the surface displacement increases with increasing the input ground motion acceleration. When the acceleration is small (0.1g), the vibration in the soil layer has an obvious tendency to enlarge continuously from bottom to top. With the increase of the acceleration (0.2g), the amplification trend basically disappeared. When the acceleration increases to 0.3g, the ground motion increases first and then decreases.
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