深圳大学学报(理工版)
深圳大學學報(理工版)
심수대학학보(리공판)
JOURNAL OF SHENZHEN UNIVERSITY (SCIENCE & ENGINEERING)
2007年
4期
339-344
,共6页
场地响应%砂土%超静孔压%地震%放大系数%固有频率
場地響應%砂土%超靜孔壓%地震%放大繫數%固有頻率
장지향응%사토%초정공압%지진%방대계수%고유빈솔
ground response%sand%pore pressure%earthquakes%amplification factor%natural frequencies
水平场地地震响应分析是岩土地震工程实践中最重要的问题之一.深圳近年多次经历外围地震引起的小振动,因而研究场地在小震作用下的响应有特殊意义.利用香港科技大学离心机及双向振动台,进行饱和砂土场地的动力模型试验.观测模型在原型峰值加速度为0.07 g 的小震作用下,加速度、侧向位移、竖向沉降及超静孔压等方面的响应.发现在地震过程中,土体变形较小,超静孔压比也小于0.5,但超静孔压的变化使场地固有频率靠近输入地震波的频率,加速度的放大系数最大可达到3.67.分析结果表明,小震作用下场地虽不大可能发生液化,但在特定情况下,仍可能对上部结构造成破坏.
水平場地地震響應分析是巖土地震工程實踐中最重要的問題之一.深圳近年多次經歷外圍地震引起的小振動,因而研究場地在小震作用下的響應有特殊意義.利用香港科技大學離心機及雙嚮振動檯,進行飽和砂土場地的動力模型試驗.觀測模型在原型峰值加速度為0.07 g 的小震作用下,加速度、側嚮位移、豎嚮沉降及超靜孔壓等方麵的響應.髮現在地震過程中,土體變形較小,超靜孔壓比也小于0.5,但超靜孔壓的變化使場地固有頻率靠近輸入地震波的頻率,加速度的放大繫數最大可達到3.67.分析結果錶明,小震作用下場地雖不大可能髮生液化,但在特定情況下,仍可能對上部結構造成破壞.
수평장지지진향응분석시암토지진공정실천중최중요적문제지일.심수근년다차경력외위지진인기적소진동,인이연구장지재소진작용하적향응유특수의의.이용향항과기대학리심궤급쌍향진동태,진행포화사토장지적동력모형시험.관측모형재원형봉치가속도위0.07 g 적소진작용하,가속도、측향위이、수향침강급초정공압등방면적향응.발현재지진과정중,토체변형교소,초정공압비야소우0.5,단초정공압적변화사장지고유빈솔고근수입지진파적빈솔,가속도적방대계수최대가체도3.67.분석결과표명,소진작용하장지수불대가능발생액화,단재특정정황하,잉가능대상부결구조성파배.
Analysis of response of level ground subjected to earthquake is one of the most important problems in geotechnical engineering practice.Since Shenzhen has been subjected to small vibration several times in recent years,the studies on response of level ground under small earthquakes are of particular interest.In this study,a centrifuge dynamic test was performed on a uniform saturated sand ground model under a small earthquake loading with a peak acceleration of about 0.07 g in the prototype scale.Acceleration,lateral displacement,vertical settlement as well as excess pore pressure were measured during the shaking event.It was observed that the deformation of soil body was small,and the excess pore pressure ratios were less than 0.5.However,the input acceleration was amplified by a factor as large as 3.67 at the ground surface.The phenomenon is associated with a shift of the natural frequency of the sand ground induced by the buildup of excess pore pressure during the earthquake.This study indicates that small earthquake may bring detrimental effect to superstructures,although liquefaction is unlikely to occur.