正规矩阵特征值扰动的新估计

设A,B均为正规矩阵,关于正规矩阵的特征值扰动,有结论 (n∑i=1︱μτ(i)-λi︱2)(1/2)≤n(1/2)‖E‖F,其中λi,μi分别为A,B的特征值.通过新的方法证明给出特征值扰动上界的新估计,并改进了以上结论.     

小黏性气体振动特征值的二阶摄动解

探讨了求一类满足边界平坦性条件的有界域内小黏性气体微振动的单特征值的更高阶摄动解 .利用边界层展开法 ,匹配特征值所满足的内场和外场微分方程 ,得到特征值的二阶摄动解 ,并为解决相近的振动特征值问题提供了一个可行的求解途径     

High precision topographic data on Lop Nor basin's Lake "Great Ear" ? and the timing of its becoming a dry salt lake

High precision elevation measurements using DGPS were carried out along three representative tran- sects for the "Great Ear" area, a dry salt lake within the Lop Nor basin. Results indicate that the Lop Nor basin is only 5.2 m deep and its lowest point occurs at the center of the "Great Ear". In addition, the basin is asymmetric - steeper in the southwest (0.19‰) and gentler in the northeast (0.09‰). Points along the same "Great Ear" ring were found to have an identical elevation value, but different when from different ones (lower towards the center). The spacing of the "Great Ear" rings was found to be closely related with the surface steepness. The closer the "Great Ear" rings are spaced, the steeper the ground surface, and vice versa. These findings support the argument that the "Great Ear" rings are the former shoreline trails left behind by Lop Nor water during the last few episodes of recession towards its total dry up. A comprehensive analysis of the high precision elevation data, historical accounts, aerial and satellite photographs and imagery, and official topographic maps of the study area suggests that the "Great Ear" area in the Lop Nor basin was incorrectly mapped as being covered by a great body of water on the 1963 topographic maps. A re-interpretation of the 1958 aerial photographs and newer remote sensing imagery indicated that the "Great Ear" ring structure was already in place in 1958 and it continued to appear on the subsequent remote sensing data without any major changes. It is estimated that lake water in the "Great Ear" area of the Lop Nor basin disappeared between the late 1930s and early 1940s.     

边界拟合坐标系中的流动方程

本文提出了流体力学解析边界拟合坐标系方法，及建立在这种坐标系基础上对流动方程进行摄动处理的方法，并列举几种流动建立了解析边界拟合坐标系中的方程。     

时域中系统鲁棒稳定性的定量计算

本文定量地考虑了当系统参数受到干扰时的稳定性问题。目的为对以状态空间法表示的线性系统鲁棒稳定性的定量计算提出一个统一的结论。文中首先对摄动的分类及对用李亚普诺夫理论求解受扰系统鲁棒稳定性的历史结果进行了述评,进而对其摄动的允许界限的计算提出了新方法。实例表明所示结果较少保守性。     

结构动力分析中Kuhar方法的改进和收敛性

本文介绍了结构动力分析中基于Ｋｕｈａｒ方法的动力缩减迭代法，应用矩阵摄动理论证明了其收敛性，算例说明了方法的有效性     

用有效势方法讨论汤川核力场中圆轨道的稳定性

以汤川核力场为例，说明用有效势方法讨论有心力场中圆形轨道的稳定性，数学处理比较简明，物理图象也比较清晰。进而指出非径向微扰引起的速度矩变化对稳定圆轨道半径ｒ＿０的影响，导出两者变化的数量关系，说明在汤川核力场中维持稳定圆运动对微扰量所加的限制。     

定量研究化学反应活性的的理论模型

应用杂化轨道和键轨道理论,以广义微扰理论为基础,建立了定量研究加成反应、取代反应、环合反应等的反应活性模型,并对氢键体系及Diels-Alder进行了讨论。     

一类三点边值问题的微分不等式及其奇异摄动

本文先研究如下类型的三点边值问题{y″=f(t,y,y′),a＜t＜c y(a)=A,y(b)=y(c)的微分不等式理论,然后利用所得到的定理,研究如下形式的二阶拟线性微分方程的边值问题{εy″=f(t,y)y′ g(t,y) y(a)=A,y(b)=y(c)的奇异摄动.     

船舶运动与受扰Kalman估计精度的统计分析

考察船舶水动力参数在标称值附近按均匀分布发生随机变化时,船舶纵向运动姿态及受扰Kalman估计的统计性能.针对某船,在5级海情,18节航速及45度航向常规工况下,当船舶水动力系数按均匀分布发生士10%、±20%随机变化时,给出船舶姿态及受扰Kalman估计精度的概率建模方法及应用.仿真结果表明,当水动力系数出现摄动时,估计精度服从对数正态分布,平均估计精度与未出现摄动时相比无显著变化.