• DocumentCode
    1453923
  • Title

    Electromagnetic scattering by anisotropic impedance half and full planes illuminated at oblique incidence

  • Author

    Nepa, Paolo ; Manara, Giuliano ; Armogida, Andreina

  • Author_Institution
    Dept. of Inf. Eng., Pisa Univ., Italy
  • Volume
    49
  • Issue
    1
  • fYear
    2001
  • fDate
    1/1/2001 12:00:00 AM
  • Firstpage
    106
  • Lastpage
    108
  • Abstract
    The three-dimensional electromagnetic (EM) scattering from half and full plane configurations, both characterized by a perfectly conducting and an anisotropic impedance face, is analyzed. The anisotropic impedance boundary condition considered for the loaded face is suitable for modeling corrugated surfaces or strip-loaded grounded dielectric slabs used to realize artificially hard or soft surfaces, with a tensor surface impedance exhibiting a vanishing impedance along the corrugations or strips and a diverging impedance in the orthogonal direction. Previous rigorous solutions, valid when the vanishing impedance direction is either parallel or perpendicular to the edge, are generalized here to the case in which the direction of vanishing impedance is arbitrarily oriented
  • Keywords
    anisotropic media; electric impedance; electromagnetic wave scattering; 3D EM scattering; anisotropic impedance boundary condition; anisotropic impedance face; anisotropic impedance full plane; anisotropic impedance half plane; artificially hard surfaces; artificially soft surfaces; corrugated surfaces; electromagnetic scattering; oblique incidence illumination; perfectly conducting face; strip-loaded grounded dielectric slabs; tensor surface impedance; vanishing impedance direction; Anisotropic magnetoresistance; Boundary conditions; Corrugated surfaces; Dielectrics; Electromagnetic analysis; Electromagnetic scattering; Slabs; Strips; Surface impedance; Tensile stress;
  • fLanguage
    English
  • Journal_Title
    Antennas and Propagation, IEEE Transactions on
  • Publisher
    ieee
  • ISSN
    0018-926X
  • Type

    jour

  • DOI
    10.1109/8.910537
  • Filename
    910537