北京建筑大学学报
北京建築大學學報
북경건축대학학보
Journal of Beijing Institute of Civil Engineering and Architecture
2014年
3期
35-39,49
,共6页
孙健%戚承志%刘旭%陈国兴
孫健%慼承誌%劉旭%陳國興
손건%척승지%류욱%진국흥
含水率%加速度%Mises 应力%平面应力
含水率%加速度%Mises 應力%平麵應力
함수솔%가속도%Mises 응력%평면응력
moisture%acceleration%Mises stress%biaxial stress
含水率对土体的弹性模量、黏聚力、内摩擦角以及土体密度都会产生影响。密实度一定的情况下,黏性土的多种力学参数会随着最佳含水率的出现而出现“峰值”效应。利用 FLAC3D 差分软件对不饱和土在地震作用下的动力响应进行了模拟和分析,探讨了土中含水率对于地下结构地震动力响应的影响规律。结果表明,在最佳含水率附近,土层的性质对于地下结构的作用来说是最良好的,此时结构的内力可取得最小值;顶板和底板的相对水平位移变化不大,并且位移的数值随着含水率的增加而逐渐减小;土体和结构的加速度峰值都随着含水率的增加而呈减小的趋势。
含水率對土體的彈性模量、黏聚力、內摩抆角以及土體密度都會產生影響。密實度一定的情況下,黏性土的多種力學參數會隨著最佳含水率的齣現而齣現“峰值”效應。利用 FLAC3D 差分軟件對不飽和土在地震作用下的動力響應進行瞭模擬和分析,探討瞭土中含水率對于地下結構地震動力響應的影響規律。結果錶明,在最佳含水率附近,土層的性質對于地下結構的作用來說是最良好的,此時結構的內力可取得最小值;頂闆和底闆的相對水平位移變化不大,併且位移的數值隨著含水率的增加而逐漸減小;土體和結構的加速度峰值都隨著含水率的增加而呈減小的趨勢。
함수솔대토체적탄성모량、점취력、내마찰각이급토체밀도도회산생영향。밀실도일정적정황하,점성토적다충역학삼수회수착최가함수솔적출현이출현“봉치”효응。이용 FLAC3D 차분연건대불포화토재지진작용하적동력향응진행료모의화분석,탐토료토중함수솔대우지하결구지진동력향응적영향규률。결과표명,재최가함수솔부근,토층적성질대우지하결구적작용래설시최량호적,차시결구적내력가취득최소치;정판화저판적상대수평위이변화불대,병차위이적수치수착함수솔적증가이축점감소;토체화결구적가속도봉치도수착함수솔적증가이정감소적추세。
Moisture content of soil has definite effects on elasticity modulus, cohesion, internal friction angle and density of soil. Given compactness of soil, several mechanical parameters of soil will have“peak value” effect at the optimum moisture content. In this paper simulation and analysis on dynamic responses of unsaturated soil under seismic excitations are carried out by using Flac3D finite difference software, and the effect of moisture content on dynamic responses of underground structure under seismic excitations is investigated. Analysis results show that properties of soil at the optimum water content are optimal for the seismic responses of underground structures, because in this case the internal forces achieve the minimum values; the relative horizontal displacement of top and bottom slabs has not significant change, and the values of displacement are gradually decreasing with the increase of water content; and so does the maximum accelerations of soil and structure with the increase of water content.