源于课本 高于课本——一道数学应用题赏析

纵观近几年来的江苏省高考数学试题和各地的模拟试题,源于课本的题型占据了一定的份量,如这次扬州二模试题(这次考试为扬州、泰州、南通联考)的第18题就是一个很好的例子,本试题为应用题,试题新颖,牵涉到函数,导数,不等式的     

声波水平折射引起水平位移椭圆极化和声能流水平偏转

针对矢量水听器测向的应用要求,研究了三维水声传播问题中水平折射对声矢量场特性的影响。理论分析表明,水平折射可使质点水平位移从线性极化转变为椭圆极化,同时引起声能流方向的水平偏转。声能流方向的水平偏转导致波达方向偏离目标水平方位,对目标水平方位估计造成误差。采用虚源法仿真了倾角为2.86°的楔形波导中的三维声矢量场,并给出了空间各点处由水平折射引起的单矢量水听器目标方位估计误差。结果显示,部分区域中由水平折射引起的目标方位估计误差可达10°以上。      

海洋声学中三维抛物方程非均匀网格模型

在海洋声学中,三维抛物方程模型可以有效考虑三维空间的声传播效应。然而,采用三维抛物方程模型分析三维空间内的声传播问题时,计算时间较长,并且需要消耗较大的计算机内存,因此给远距离声场的快速精确计算带来了很大困难。为此,将非均匀网格Galerkin离散化方法用于三维直角坐标系下的水声抛物方程模型中,深度算子和水平算子Galerkin离散方式由均匀网格变为非均匀网格。仿真结果表明,三维直角坐标系下非均匀网格离散的抛物方程模型,在保持计算精度、提高计算速度的同时,可以实现远距离声场的快速预报。另外,针对远距离局部海底地形与距离有关的三维声传播问题,给出了声场快速计算方法;在海底保持水平的区域,采用经典Kraken模型,重构抛物方程算法的初始场,随后依次递推求解地形与距离有关海底下的三维声场。采用改进模型,证明了远距离楔形波导声强增强效应。      

高掺杂InGaAsP材料的荧光光谱和Moss-Burstein移动

本文研究了77K下,n型InGaAsP材料的阴极荧光。利用导带到类受主能级跃迁的模型,考虑到高掺杂样品带尾效应的影响,计算了高掺杂样品阴极荧光光谱随掺杂浓度变化的Moss-Burstein移动。理论计算结果与实验值较好地符合。     

Three-dimensional parabolic equation model for seismo-acoustic propagation: Theoretical development and preliminary numerical implementation

A three-dimensional(3D) parabolic equation(PE) model for sound propagation in a seismo-acoustic waveguide is developed in Cartesian coordinates, with x, y, and z representing the marching direction, the longitudinal direction, and the depth direction, respectively. Two sets of 3D PEs for horizontally homogenous media are derived by rewriting the 3D elastic motion equations and simultaneously choosing proper dependent variables. The numerical scheme is for now restricted to the y-independent bathymetry. Accuracy of the numerical scheme is validated, and its azimuthal limitation is analyzed. In addition, effects of horizontal refraction in a wedge-shaped waveguide and another waveguide with a polyline bottom are illustrated. Great efforts should be made in future to provide this model with the ability to handle arbitrarily irregular fluid-elastic interfaces.     

沉积层声学特性对浅海低频声场分布的影响

已有对浅海低频水声场的讨论多是关注声能量在水体中的分布特性,对水体下沉积层、基底中低频声传播的同步研究相对较少。本文基于波动方程,在柱坐标系下推导了一种浅海水体/海底统一波导下低频声能流的计算模型,在此基础上结合具体仿真算例与波动理论阐述了不同沉积层声学参数对声场能量分布的影响规律及机理。仿真结果表明,在沉积层纵波声速>水中声速>沉积层横波声速的前提下,沉积层中密度与纵波声速数值越大,声能量越趋于保留在水体中而不向海底泄漏,横波声速的影响正好相反;沉积层厚度增加到一定量后,基底对流体层中声传播的影响可近似忽略不计。      

源于课本 高于课本——一道数学应用题赏析

纵观近几年来的江苏省高考数学试题和各地的模拟试题,源于课本的题型占据了一定的份量,如这次扬州二模试题（这次考试为扬州、泰州、南通联考）的第18题就是一个很好的例子,本试题为应用题,试题新颖,牵涉到函数,导数,不等式的综合知识以及控制变量的思想,要求考生具备很强的说理能力．     

Developments of parabolic equation method in the period of 2000–2016

Parabolic equation(PE) method is an efficient tool for modelling underwater sound propagation, particularly for problems involving range dependence. Since the PE method was first introduced into the field of underwater acoustics,it has been about 40 years, during which contributions to extending its capability has been continuously made. The most recent review paper surveyed the contributions made before 1999. In the period of 2000–2016, the development of PE method basically focuses on seismo-acoustic problems, three-dimensional problems, and realistic applications. In this paper, a review covering the contribution from 2000 to 2016 is given, and what should be done in future work is also discussed.     

采用能量守恒和高阶Padé近似的三维水声抛物方程模型

为了充分考虑海底地形随三维空间变化的海洋环境中水平方位角耦合效应对声传播的影响,建立了一种三维柱坐标系下流体高阶抛物方程算法。该算法采用泰勒近似将二维方根算子分裂成一维方根算子,并采用分裂步进的高阶Pade近似将一维方根算子写成微分算子有理分式连乘的形式,进而应用Galerkin离散化方法来处理微分算子,最终将微分方程写成矩阵方程的形式;采用能量守恒近似来处理海底边界,以考虑复杂海底对于声传播的影响;采用交替方向隐式格式,实现了三维声场的步进计算。楔形和海底山等典型海域声场仿真计算表明,相比于已有的声场计算模型,三维柱坐标系下高阶抛物方程模型可以更加精确地计算楔形海域和海底山区域的三维声场,实现水平方位全空间声场计算。