• DocumentCode
    861149
  • Title

    Line element for efficient computation of the magnetic field created by thin iron plates

  • Author

    Brunotte, Xavier ; Meunier, Gérard

  • Author_Institution
    Lab. de Magnetisme du Navire, CNRS, St. Martin d´´Heres, France
  • Volume
    26
  • Issue
    5
  • fYear
    1990
  • fDate
    9/1/1990 12:00:00 AM
  • Firstpage
    2196
  • Lastpage
    2198
  • Abstract
    The problem of computing the magnetic anomaly created by iron ships in the Earth´s field is considered. From a modeling point of view, one of the major characteristics of this problem is the external and uniform magnetic source (the Earth´s field). A good way of taking this into account is to simulate infinity and to use the reduced scalar potential as the state function. The major difficulty in modeling ships is the presence of sophisticated 3-D geometries due to the disproportion between the global size of a ship and the thickness of the iron plates. The modeling of the thin iron plates is examined, and it is shown that an efficient method is to use line elements in 2-D and surface elements in 3-D. The authors present the finite-element formulations used, applied to scalar potentials (reduced or total). The formulations using line elements have been successfully applied, even to a magnetic region with small permeability values. Results in 2-D and comparisons with analytical solutions and actual measurements are presented
  • Keywords
    finite element analysis; iron; magnetic fields; 3-D geometries; Earth´s field; Fe; Fe ships; finite-element formulations; global size; line element; line elements; magnetic anomaly; magnetic field; permeability values; reduced scalar potential; state function; thin Fe plates; uniform magnetic source; Computational modeling; Earth; Finite element methods; Geometry; H infinity control; Iron; Magnetic fields; Marine vehicles; Permeability; Solid modeling;
  • fLanguage
    English
  • Journal_Title
    Magnetics, IEEE Transactions on
  • Publisher
    ieee
  • ISSN
    0018-9464
  • Type

    jour

  • DOI
    10.1109/20.104667
  • Filename
    104667