Section 5.6 · Topic 7 of 11
5.6.7 The Helmholtz equations
The phasor equations can now be solved for and separately, in the same way as the wave equations of Section 5.5 were obtained in the time domain. Consider a homogeneous medium with and , containing the impressed sources and .
The equation for the electric field
Take the curl of 1, written as :
Insert 2 in the form of Eq. (5.6.13), :
Use the vector identity (Section 2.2) with (see the box below):
The equation for the magnetic field
Take the curl of 2:
and with (from 4), .
In a conducting medium the free charge density that appears in 3 includes charge carried by the conduction current. The divergence of Eq. (5.6.13) gives , and the continuity of the impressed source, , turns this into , where is now the charge density of the source alone. In a homogeneous medium is a constant and . In a lossless medium and this is just 3.
In a homogeneous medium with permeability and complex permittivity ,
with the wave number
where is the Laplacian. is the phase constant in and the attenuation constant in . In a source-free region (, )
and each Cartesian component obeys the scalar equation .
The Helmholtz equation is the wave equation for one frequency. Where the wave equation of Section 5.5 had , the Helmholtz equation has , a number.
The comparison can be made exact. In a source-free conducting medium the wave equation of Section 5.5 carries the term ,
and . The first derivative in time, which made the lossy wave equation awkward, has become the imaginary part of . In a lossless medium is real, and , and in free space
A source-free field must satisfy both and . The Helmholtz equation was derived with the divergence condition already used, and it does not imply it. The field in free space at satisfies the Helmholtz equation, but it points along its own direction of variation, has and cannot exist without charge (Exercise 5.6.6).