• DocumentCode
    761834
  • Title

    DC current distributions and magnetic fields using the T-omega edge-element method

  • Author

    Webb, J.P. ; Forghani, B.

  • Author_Institution
    Dept. of Electr. Eng., McGill Univ., Montreal, Que., Canada
  • Volume
    31
  • Issue
    3
  • fYear
    1995
  • fDate
    5/1/1995 12:00:00 AM
  • Firstpage
    1444
  • Lastpage
    1447
  • Abstract
    When steady currents flow in solid conductors, the current distributions are not known in advance, and a 3D finite-element analysis of the magnetostatic fields must also involve an analysis of the currents. To find the currents, either of two potentials can be used: the electric scalar potential or a vector potential T for the current density. The scalar potential has the disadvantage of producing a current density that is only approximately solenoidal, and is therefore incompatible with Ampere´s Law for the magnetic field. The vector potential gives solenoidal currents. It may conveniently be found by applying the T-Ω edge element method, an existing method for eddy current problems, in one of two ways: setting the frequency so low that the DC solution is obtained; or solving first for T, then for Ω. Either way, both the current distribution and the magnetic field are obtained, and the solution is ideally suited for subsequent transient analysis. Results from three test problems confirm the validity of the method
  • Keywords
    current density; current distribution; electromagnetism; magnetic fields; transient analysis; 3D finite-element analysis; DC current distributions; T-omega edge-element method; current density; magnetic fields; magnetostatic fields; solenoidal currents; solid conductors; transient analysis; vector potential; Conductors; Current density; Current distribution; Eddy currents; Electric potential; Finite element methods; Magnetic analysis; Magnetic fields; Magnetostatics; Solids;
  • fLanguage
    English
  • Journal_Title
    Magnetics, IEEE Transactions on
  • Publisher
    ieee
  • ISSN
    0018-9464
  • Type

    jour

  • DOI
    10.1109/20.376300
  • Filename
    376300