反平面冲击荷载作用下圆柱形洞室的动力响应
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  • 英文篇名:Dynamic response of a cylindrical cavity to an anti-plane impact load
  • 作者:翟朝娇 ; 夏唐代 ; 王宁 ; 杜国庆
  • 英文作者:ZHAI Chao-jiao1,2,XIA Tang-dai1,2,WANG Ning1,2,DU Guo-qing3(1.MOE Key Laboratory of Soft Soils and Geoenvironmental Engineering,Zhejiang University,Hangzhou 310058,China; 2.Institute of Geotechnical Engineering,Zhejiang University,Hangzhou 310058,China; 3.Anhui Electric Power Design Institute,Hefei 230601,China)
  • 关键词:圆柱形孔洞 ; 反平面 ; 拉普拉斯变换 ; 冲击荷载 ; 动力响应
  • 英文关键词:cylindrical cavity;anti-plane;Laplace transformation;impact load;dynamic responses
  • 中文刊名:ZDCJ
  • 英文刊名:Journal of Vibration and Shock
  • 机构:浙江大学软弱土与环境土工教育部重点实验室;浙江大学岩土工程研究所;安徽省电力设计院;
  • 出版日期:2013-01-28
  • 出版单位:振动与冲击
  • 年:2013
  • 期:v.32;No.190
  • 语种:中文;
  • 页:ZDCJ201302029
  • 页数:6
  • CN:02
  • ISSN:31-1316/TU
  • 分类号:158-162+175
摘要
对无限弹性土体内圆柱形洞室在反平面冲击荷载的作用下的瞬态响应进行了探讨。用残余变量的方法结合拉普拉斯变换及其逆变换,在频域内的得到土体位移和应力一般表达式,并采用拉普拉斯逆变换的数值方法,给出了问题的数值解。在时域内分析了无限弹性土体内圆柱形孔洞在沿轴向方向的冲击荷载作用下的土体动力响应的变化规律,并将计算结果与静力情况下的计算值作了比较:反平面荷载作用后,波向外发散传播,并沿半径方向衰减,衰减速度较静力情况下的衰减要慢,且距离波源越远二者差别越大;波到达后,该点土体的应力和位移均发生与外荷载相同的三角形变化:先增大,随后减小最后保持为零不变。
        The transient response to an anti-plane impact load of an infinite elastic soil body containing a cylindrical cavity was studied.Using the residual variable method combined with Laplace transformation and its inverse transformation,the general expressions of the displacement and stress of the soil were obtained in frequency domain,respectively.And the numerical solutions were calculated by using the numerical method of inverse Laplace transformation.In time domain,the dynamic responses of a cylindrical cavity in the infinite elastic soil were analyzed under axial impact load,and the calculation results were compared with those in the static case.It was shown that after an anti-plane impact load is exerted on,the wave spreads outward,and dissipates along the radial direction;the attenuation rate is smaller than that under static conditions;and the farther the wave from its source,the greater the difference between the two rates;after wave arrivals,the stress and displacement of the soil at this point reveal triangular changes,the same as the external load,they increase at first and then decrease,and remain zero finally.
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