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Maxwell's equations

Until the 19th century electric and magnetic effects were seen as two independent physical occurences. In 1820 Oersted proved, that electric currents can influence the needle of a compass. Ampère and Faraday laid the foundation for the unified theory of electrodynamics, which was elaborated by James Clerk Maxwell (1831-1879).

His famous equations are the starting point for our investigations:

                 ( )

In order to solve these equations for our purpose, we have to make several assumptions. First, we neglect any displacement currents , which are typically relevant only at radio frequencies (in the MHz regime), and set . In the quasistatic approximation we omit the the term

                 ( )

Secondly, we assume, that there are no free charges (. The simplified Maxwell equations are given by

                 ( )

Then, we require the field intensity and the flux intensity to obey the constitutive relationship

         .        ( )

If the material is nonlinear (e.g. ferromagnetic), the permeability ( is a function of B.

                 ( )

However, we will consider only linear materials in this case in this project.

The relationship between the electric field intensity and the current density is given by

         .        ( )

Now we introduce a magnetic vector potential , and define it as

                 ( )

which guarantees the validity of Maxwell's second equation. Then we can rewrite the fourth equation and obtain

                 ( )

With the Coulomb gauge condition

                 ( )

and the well known operator relation

                 ( )

we find

         .        ( )

Inserting (7) in the third Maxwell equation yields

         .        ( )

In the case of 2D problems, we can integrate this equation and get

                 ( )

and together with constitutive relationship between the electric field intensity and the current density we obtain

                 ( )

Finally we insert this in (11) to eliminate and arrive at

         ,        ( )

where represents the applied current sources.

Finally, we restrict ourselves to time harmonic problems, in which all fields oscillate harmonically at one fixed frequency. Thus, we can use a phasor transformation and rewrite the magnetic vector potential as

                 ( )

in which is the complex amplitude. By substituting this ansatz in (15) we can eliminate the time derivative and finally arrive at

         .        ( )

next up previous contents
Next: The finite element method Up: Calculation of eddy currents Previous: Calculation of eddy currents Contents


© 1999 Werner Scholz
werner.scholz (at) tuwien.ac.at