论文标题
d'Alembert数字化:一种可视化物质电磁波的波脉冲方法,并得出有限的差异时间域方法,用于求解麦克斯韦方程
d'Alembert Digitized: A Wave Pulse Method for Visualizing Electromagnetic Waves in Matter and for Deriving the Finite Difference Time Domain Method for Numerically Solving Maxwell's Equations
论文作者
论文摘要
提出了一种可视化物质中电磁波和得出有限差差时域法(FDTD)的替代方法,以模拟一个维系统的麦克斯韦方程。该方法使用D'AlemberT将波的分裂分解为任意形状的前后脉冲,并允许随着位置变化的网格间距和材料属性。在具有不同折射指标的材料之间的边界以及通过导电材料的部分反射,传播和衰减之间的边界之间的无分散介电材料,部分反射和传输中波的恒定速度,而无需求助于指数函数,三角函数功能或复杂数字。 Placing d'Alembert's method on a grid is shown to be equivalent to FDTD and allows for a simple and visual proof that FDTD is exact for dielectrics when the ratio of the spatial and temporal grid spacing is the wave speed, a straightforward way to incorporate reflectionless boundary conditions, and a derivation that FDTD retains second order accuracy when the grid spacing varies with position and the material parameters make sudden跳过图层边界。
An alternative way of visualizing electromagnetic waves in matter and of deriving the Finite Difference Time Domain method (FDTD) for simulating Maxwell's equations for one dimensional systems is presented. The method uses d'Alembert's splitting of waves into forward and backward pulses of arbitrary shape and allows for grid spacing and material properties that vary with position. Constant velocity of waves in dispersionless dielectric materials, partial reflection and transmission at boundaries between materials with different indices of refraction, and partial reflection, transmission, and attenuation through conducting materials are derived without recourse to exponential functions, trigonometric functions, or complex numbers. Placing d'Alembert's method on a grid is shown to be equivalent to FDTD and allows for a simple and visual proof that FDTD is exact for dielectrics when the ratio of the spatial and temporal grid spacing is the wave speed, a straightforward way to incorporate reflectionless boundary conditions, and a derivation that FDTD retains second order accuracy when the grid spacing varies with position and the material parameters make sudden jumps across layer boundaries.