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Spectral Domain Immittance Method: Analyzing Plane Waves and Current Decomposition

This document discusses the Spectral Domain Immittance (SDI) method, focusing on the representation of a finite current sheet as multiple infinite phased current sheets. It explores how to decompose the current into components that excite TMz and TEz plane waves. The document outlines the launching properties of these waves within an infinite medium, leading to the development of Transverse Equivalent Network (TEN) modeling equations. Additional examples illustrate the practical application of the approach, addressing the behavior of currents and fields in free space.

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Spectral Domain Immittance Method: Analyzing Plane Waves and Current Decomposition

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  1. ECE 6341 Spring 2014 Prof. David R. Jackson ECE Dept. Notes 38

  2. Spectral Domain Immittance (SDI) Method

  3. SDI Method (cont.) ks The finite current sheet is thus represented as a set of infinite phased current sheets: where This phased current sheet launches a pair of plane waves as shown below:

  4. SDI Method (cont.) ks Goal: Decompose the current into two parts: one that excites only a pair of TMz plane waves, and one that excites only a pair of TEzplane waves.

  5. SDI Method (cont.) Define: Launching of plane wave by source:

  6. SDI Method (cont.)

  7. SDI Method (cont.)

  8. SDI Method (cont.) TMz

  9. SDI Method (cont.) TEz

  10. SDI Method (cont.) Proof of launching property: Consider an arbitrary surface current. An infinite medium is considered, since we are only looking at the launching property of the waves. At z = 0 we have that Note: This follows from the fact that the magnetic vector potential component Ax is an even function of z (imagining the current to be in the xdirection for simplicity here).

  11. SDI Method (cont.) Hence

  12. SDI Method (cont.) Two cases of interest:

  13. SDI Method (cont.) Split current into two parts: Launches TEz Launches TMz

  14. Transverse Fields H E TMz :

  15. Transverse Fields (cont.) H E TEz :

  16. Transverse Equivalent Network TEN modeling equations:

  17. TEN (cont.) Source

  18. TEN (cont.) Source

  19. Source Model Phased current sheet inside layered medium

  20. Source Model (cont.) so Hence Also Hence

  21. Source Model (cont.) TMz Model:

  22. Source Model (cont.) TEz Model: (derivation omitted)

  23. Source Model (cont.) The transverse fields can then be found from

  24. Source Model (cont.) Introduce normalized voltage and current functions: (following the notation of K. A. Michalski) Then we can write

  25. Source Model (cont.) Hence

  26. Example Find for z0 due to a surface current at z= 0, with The current is radiating in free space.

  27. Example Decompose current into two parts:

  28. Example (cont.)

  29. Example (cont.)

  30. Example (cont.) Hence

  31. Example (cont.) TMz Model For z>0:

  32. Example (cont.) TEz Model For z> 0:

  33. Example (cont.) Hence where

  34. Example (cont.) Substituting in values, we have: Hence or

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