Physics:Electric-field integral equation

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Short description: Calculation of electric field generated by current distribution

The electric-field integral equation is a relationship that allows the calculation of an electric field (E) generated by an electric current distribution (J).

Derivation

When all quantities in the frequency domain are considered, a time-dependency ejwt that is suppressed throughout is assumed.

Beginning with the Maxwell equations relating the electric and magnetic field, and assuming a linear, homogeneous media with permeability μ and permittivity ε: ×𝐄=jωμ𝐇×𝐇=jωε𝐄+𝐉

Following the third equation involving the divergence of H 𝐇=0 by vector calculus we can write any divergenceless vector as the curl of another vector, hence ×𝐀=𝐁 where A is called the magnetic vector potential. Substituting this into the above we get ×(𝐄+jω𝐀)=0 and any curl-free vector can be written as the gradient of a scalar, hence 𝐄+jω𝐀=Φ where Φ is the electric scalar potential.[lower-alpha 1] These relationships now allow us to write 1μ××𝐀1μk2𝐀=𝐉jωεΦ where k=ωμε, which can be rewritten by vector identity as 1μ(𝐀)1μ2𝐀1μk2𝐀=𝐉jωεΦ

As we have only specified the curl of A, we are free to define the divergence,[1] and choose the following: 𝐀=jωεμΦ which is called the Lorenz gauge condition. The previous expression for A now reduces to 1μ2𝐀+1μk2𝐀=𝐉 which is the vector Helmholtz equation. The solution of this equation for A is 𝐀(𝐫)=μ4π𝐉(𝐫) G(𝐫,𝐫)d𝐫 where G(𝐫,𝐫) is the three-dimensional homogeneous Green's function given by G(𝐫,𝐫)=ejk|𝐫𝐫||𝐫𝐫|

By combining the above definitions of the electric scalar potential and the Lorenz gauge, we can now write what is called the electric field integral equation (EFIE), relating the electric field E to the vector potential A 𝐄=jω𝐀+1jωε(𝐀)

We can further represent the EFIE in the dyadic form as 𝐄=jωVd𝐫𝐆(𝐫,𝐫)𝐉(𝐫) where 𝐆(𝐫,𝐫) here is the dyadic homogeneous Green's Function given by 𝐆(𝐫,𝐫)=14π[𝐈+k2]G(𝐫,𝐫)

Interpretation

The EFIE describes a radiated field E given a set of sources J, and as such it is the fundamental equation used in antenna analysis and design. It is a very general relationship that can be used to compute the radiated field of any sort of antenna once the current distribution on it is known. The most important aspect of the EFIE is that it allows us to solve the radiation/scattering problem in an unbounded region, or one whose boundary is located at infinity. For closed surfaces, it is possible to use the Magnetic Field Integral Equation or the Combined Field Integral Equation, both of which result in a set of equations with improved condition number compared to the EFIE. However, the MFIE and CFIE can still contain resonances.

In scattering problems, it is desirable to determine an unknown scattered field Es that is due to a known incident field Ei. Unfortunately, the EFIE relates the scattered field to J, not the incident field, so we do not know what J is. This sort of problem can be solved by imposing the boundary conditions on the incident and scattered field, allowing one to write the EFIE in terms of Ei and J alone. Once this has been done, the integral equation can then be solved by a numerical technique appropriate to integral equations such as the method of moments.

Applications

The EFIE is often used to calculated electromagnetic fields via the method of moments.

References

  • Gibson, Walton C. The Method of Moments in Electromagnetics. Chapman & Hall/CRC, 2008. ISBN 978-1-4200-6145-1
  • Harrington, Roger F. Time-Harmonic Electromagnetic Fields. McGraw-Hill, Inc., 1961. ISBN 0-07-026745-6.
  • Balanis, Constantine A. Advanced Engineering Electromagnetics. Wiley, 1989. ISBN 0-471-62194-3.
  • Chew, Weng C. Waves and Fields in Inhomogeneous Media. IEEE Press, 1995. ISBN 0-7803-4749-8.
  • Rao, Wilton, Glisson. Electromagnetic Scattering by Surfaces of Arbitrary Shape. IEEE Transactions on Antennas and Propagation, vol, AP-30, No. 3, May 1982. doi:10.1109/TAP.1982.1142818
  1. This is the general definition of the electric scalar potential. In the special case when the magnetic field is static (time invariant), it reduces to the more familiar 𝐄=Φ.



  1. By the Helmholtz theorem, a vector field is described completely by its divergence and curl. As we have defined only the curl of A, we may choose any divergence, provided that we consistently use this definition in all subsequent analysis.