The elastic plate vibration model is studied under the external force. The size of the source term by the given mode of the source and some observations from the body of the plate is determined over a time interval, w...The elastic plate vibration model is studied under the external force. The size of the source term by the given mode of the source and some observations from the body of the plate is determined over a time interval, which is referred to be an inverse source problem of a plate equation. The uniqueness theorem for this problem is stated, and the fundamental solution to the plate equation is derived. In the case that the plate is driven by the harmonic load, the fundamental solution method （FSM） and the Tikhonov regularization technique axe used to calculate the source term. Numerical experiments of the Euler-Bernoulli beam and the Kirchhoff-Love plate show that the FSM can work well for practical use, no matter the source term is smooth or piecewise.展开更多
We treat even-order tensors with Einstein product as linear operators from tensor space to tensor space, define the mill spaces and the ranges of tensors, and study their relationship. We extend the fundamental theore...We treat even-order tensors with Einstein product as linear operators from tensor space to tensor space, define the mill spaces and the ranges of tensors, and study their relationship. We extend the fundamental theorem of linear algebra for matrix spaces to tensor spaces. Using the new relationship, we characterize the least-squares （M） solutions to a multilineax system and establish the relationship between the minimum-norm （N） leastsquares （M）solution of a multilinear system and the weighted Moore-Penrose inverse of its coefficient tensor. We also investigate a class of even-order tensors induced by matrices and obtain some interesting properties.展开更多
针对柯西声学反问题,即部分边界信息未知的声学问题,本文采用局部基本解法,对基于局部基本解法的声学反问题模拟及Matlab实现进行研究。采用新型半解析无网格配点法,将中心节点处的声压表示成局部支撑域内支撑节点处声压的线性组合,再...针对柯西声学反问题,即部分边界信息未知的声学问题,本文采用局部基本解法,对基于局部基本解法的声学反问题模拟及Matlab实现进行研究。采用新型半解析无网格配点法,将中心节点处的声压表示成局部支撑域内支撑节点处声压的线性组合,再通过可测边界节点的已知物理量,使内部节点和不可测边界节点的声压值满足控制方程,建立一个大型稀疏线性方程,获得不可测边界的声压值。同时,给出局部基本解法的计算模型及其数值离散格式,并以Matlab为软件平台,设计了声学反问题仿真计算程序,开发了图形用户界面(graphics user interface,GUI)。仿真结果表明,该方法计算精度高,数值稳定,对含有噪声的边界数据可得到较好的反演结果。该研究为声学反问题的数值模拟提供了一种新的思路。展开更多
研究了六层层状介质模型瑞利波基阶和高模式波相速度对横波速度、深度的敏感性,结果表明：基阶波较高模式波对7m以内浅部地层的横波速度更敏感,敏感性频带在10-25Hz范围内,峰值频带集中在18Hz左右;高模式波较基阶波对深部地层的横波速...研究了六层层状介质模型瑞利波基阶和高模式波相速度对横波速度、深度的敏感性,结果表明：基阶波较高模式波对7m以内浅部地层的横波速度更敏感,敏感性频带在10-25Hz范围内,峰值频带集中在18Hz左右;高模式波较基阶波对深部地层的横波速度更敏感,敏感性频带宽,峰值分散.基阶波对浅层的敏感性和高模式波穿透深度更深的特点为近地表岩土层二维横波速度结构的联合反演提供了前提条件.利用阻尼最小二乘SVD（Singular Value Decomposition）算法联合基阶与高模式波对理论模型和实例数据进行横波速度反演,反演结果表明联合反演增强了反演的稳定性,提高了反演的精度.展开更多
文摘The elastic plate vibration model is studied under the external force. The size of the source term by the given mode of the source and some observations from the body of the plate is determined over a time interval, which is referred to be an inverse source problem of a plate equation. The uniqueness theorem for this problem is stated, and the fundamental solution to the plate equation is derived. In the case that the plate is driven by the harmonic load, the fundamental solution method （FSM） and the Tikhonov regularization technique axe used to calculate the source term. Numerical experiments of the Euler-Bernoulli beam and the Kirchhoff-Love plate show that the FSM can work well for practical use, no matter the source term is smooth or piecewise.
文摘We treat even-order tensors with Einstein product as linear operators from tensor space to tensor space, define the mill spaces and the ranges of tensors, and study their relationship. We extend the fundamental theorem of linear algebra for matrix spaces to tensor spaces. Using the new relationship, we characterize the least-squares （M） solutions to a multilineax system and establish the relationship between the minimum-norm （N） leastsquares （M）solution of a multilinear system and the weighted Moore-Penrose inverse of its coefficient tensor. We also investigate a class of even-order tensors induced by matrices and obtain some interesting properties.
文摘针对柯西声学反问题,即部分边界信息未知的声学问题,本文采用局部基本解法,对基于局部基本解法的声学反问题模拟及Matlab实现进行研究。采用新型半解析无网格配点法,将中心节点处的声压表示成局部支撑域内支撑节点处声压的线性组合,再通过可测边界节点的已知物理量,使内部节点和不可测边界节点的声压值满足控制方程,建立一个大型稀疏线性方程,获得不可测边界的声压值。同时,给出局部基本解法的计算模型及其数值离散格式,并以Matlab为软件平台,设计了声学反问题仿真计算程序,开发了图形用户界面(graphics user interface,GUI)。仿真结果表明,该方法计算精度高,数值稳定,对含有噪声的边界数据可得到较好的反演结果。该研究为声学反问题的数值模拟提供了一种新的思路。
文摘研究了六层层状介质模型瑞利波基阶和高模式波相速度对横波速度、深度的敏感性,结果表明：基阶波较高模式波对7m以内浅部地层的横波速度更敏感,敏感性频带在10-25Hz范围内,峰值频带集中在18Hz左右;高模式波较基阶波对深部地层的横波速度更敏感,敏感性频带宽,峰值分散.基阶波对浅层的敏感性和高模式波穿透深度更深的特点为近地表岩土层二维横波速度结构的联合反演提供了前提条件.利用阻尼最小二乘SVD（Singular Value Decomposition）算法联合基阶与高模式波对理论模型和实例数据进行横波速度反演,反演结果表明联合反演增强了反演的稳定性,提高了反演的精度.
