电磁波在空时多周期调制磁介质填充波导中的传播

E. Gevorkyan
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引用次数: 1

摘要

研究了任意截面的理想规则波导中电磁波的特性。假设波导填充在空间和时间上是多周期调制的,且调制深度较小。通过这种方式,波导填充的调制不会导致不同波导模式之间的相互作用。在麦克斯韦方程组的基础上,得到了电矢量和磁矢量纵向分量的波动方程。他们描述了波导的横向电场(TE)和横向磁场(TM)场。这些波动方程是带周期系数的二阶偏微分方程。利用变量变换,将其化为具有周期系数的Mathieu-Hill型常微分方程。在波导调制深度较小的假设下,当两波之间的一阶Wulff-Bragg条件不满足时,在信号波与调制波之间的“弱”相互作用的频域内,对调制深度进行了一阶逼近,得到了这些方程的解。本文得到的TE和TM场的解析表达式表明,在小调制深度的第一近似下,TE和TM场是由三个复振幅和复频率的时空谐波组成的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Propagation of Electromagnetic Waves in a Waveguide with Space-Time Multiperiodically Modulated Magnetodielectric Filling
The properties of electromagnetic waves in an ideal regular waveguide that is characterized by arbitrary cross-section are studied. It is assumed, that the filling of waveguide is multiperiodically modulated in space and time, and the modulation depths are small. By this the modulation of the waveguide filling does not lead to the interaction between different waveguide modes. The wave equations for the longitudinal components of the electric and magnetic vectors are obtained based on the system of Maxwell's equations. They describe the waveguide's transverse-electric (TE) and transverse-magnetic (TM) fields. These wave equations are partial differential equations of second order with periodic coefficients. Using change of variables, they are reduced to ordinary differential equations with periodic coefficients of the Mathieu-Hill type. Under the assumption of small modulation depths of the waveguide filling solutions of these equations are found in the first approximation with respect to the modulation depths in the frequency domain of the “weak” interaction between the signal wave and the modulation wave, when the first-order Wulff-Bragg condition between the waves, reflected from the filling inhomogeneities, is not satisfied. The analytical expressions, obtained in this article for the TE and TM fields, show that in the first approximation in terms of small modulation depths the TE and TM fields are given as a set of three space-time harmonics with specified complex amplitudes and frequencies.
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