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CONSERVATIVE MODELING OF 3-D ELECTROMAGNETIC FIELDS .1. PROPERTIES AND ERROR ANALYSIS

机译:3-D电磁场的保守建模.1。属性和错误分析

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Conservation of electric current and magnetic flux can be explicitly enforced by modeling Maxwell's equations on a staggered grid, where the different field components are sampled at points offset relative to each other. A staggered finite-difference (SFD) approximation gives divergence-free magnetic fields and electric currents ensuring good behavior at all periods. Comparisons of SFD solutions with 2-D quasi-analytic solutions are very good (similar to 1% rms error). When a modeled region can be subdivided into uniform subdomains, comparison of analytic solutions and SFD approximations show that the greatest differences occur near the Nyquist wavenumbers; the SFD solutions do not attenuate in space as rapidly as the analytic solutions. The accuracy of a computed SFD solution can be estimated from its wavenumber content. For test cases the accuracy estimates are surprisingly close to the actual accuracies. Grid requirements for modeling short horizontal wavelength components of a solution seem more demanding than for modeling the infinite wavelength (plane-wave) component: for 2% accuracy 4 pi samples are required per horizontal wavelength compared to two samples per skin depth for the plane-wave component. [References: 19]
机译:电流和磁通量的守恒可以通过在交错网格上对麦克斯韦方程组建模来明确地强制执行,在该网格上,在互不相同的点采样不同的场分量。交错的有限差分(SFD)近似值可提供无散度的磁场和电流,从而确保所有期间的行为良好。 SFD解决方案与二维准分析解决方案的比较非常好(类似于1%rms误差)。当建模区域可以细分为统一的子域时,解析解与SFD近似值的比较表明,最大的差异出现在奈奎斯特波数附近; SFD解决方案在空间中的衰减不如分析解决方案那么快。计算出的SFD解决方案的准确性可以从其波数含量估算出来。对于测试用例,准确度估计令人惊讶地接近实际精度。建模解决方案的短水平波长分量的网格要求似乎比建模无限波长(平面波)分量的网格要求更高:对于2%的精度,每个水平波长需要4 pi样本,而平面的每个趋肤深度需要两个pi样本。波分量。 [参考:19]

著录项

  • 来源
    《Geophysics》 |1996年第5期|p. 1308-1318|共11页
  • 作者

    Smith JT.;

  • 作者单位

    UNIV CALIF BERKELEY DEPT MAT SCI & MINERAL ENGN BERKELEY CA 94720 USA;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 地球物理学;
  • 关键词

    Finite-difference; Equations;

    机译:有限差分;等式;
  • 入库时间 2022-08-18 00:20:13

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