A high-order accurate scheme for Maxwell's equations with a generalized dispersive material model

被引:20
|
作者
Angel, Jordan B. [1 ,3 ]
Banks, Jeffrey W. [1 ]
Henshaw, William D. [1 ]
Jenkinson, Michael J. [1 ]
Kildishev, Alexander, V [2 ]
Kovacic, Gregor [1 ]
Prokopeva, Ludmila J. [2 ]
Schwendeman, Donald W. [1 ]
机构
[1] Rensselaer Polytech Inst, Dept Math Sci, Troy, NY 12180 USA
[2] Purdue Univ, Sch Elect & Comp Engn, W Lafayette, IN 47907 USA
[3] NASA, Ames Res Ctr, Sci & Technol Corp, Moffett Field, CA 94035 USA
关键词
Generalized dispersive material model; Dispersive FDTD; Electromagnetics; Composite overlapping grids; TIME-DOMAIN FORMULATION; TRANSIENT PROPAGATION; HYDRODYNAMIC MODEL; WAVE-PROPAGATION; UPWIND SCHEMES; FDTD; MEDIA; ABSORPTION; GENERATION;
D O I
10.1016/j.jcp.2018.11.021
中图分类号
TP39 [计算机的应用];
学科分类号
081203 ; 0835 ;
摘要
A high-order accurate scheme for solving the time-domain Maxwell's equations with a generalized dispersive material model is described. The equations for the electric field are solved in second-order form, and a general dispersion model is treated with the addition of one or more polarization vectors which obey a set of auxiliary differential equations (ADE). Numerical methods are developed for both second-order and fourth-order accuracy in space and time. The equations are discretized using finite-differences, and advanced in time with a single-stage, three-level, space-time scheme which remains stable up to the usual explicit CFL restriction, as proven using mode analysis. Because the equations are treated in their second-order form, there is no need for grid staggering, and instead a collocated grid is used. Composite overlapping grids are used to treat complex geometries with boundary-conforming grids, and a high-order upwind dissipation is added to ensure robust and stable approximations on overlapping grids. Numerical results in two and three space dimensions confirm the accuracy and stability of the new schemes. (C) 2018 Elsevier Inc. All rights reserved.
引用
收藏
页码:411 / 444
页数:34
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