Introduction To Modern Planar Transmission Lines. Anand K. Verma

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potential with momentum. The magnetic vector potential
could be considered as the potential momentum per unit charge, just as the electric scalar potential ϕ is the potential energy per unit charge [J.16]. The potential momentum
is obtained as follows:

      (1.1.2)equation

      It is to be noted that at a location in the space, even for zero images and images fields, the potentials images and ϕ could exist [B.11]. Aharonov–Bohm predicted that the potential fields images and ϕ, in the absence of images and images, could influence a charged particle. Tonomura and collaborators experimentally confirmed the validity of Aharonov–Bohm prediction. The Aharonov–Bohm effect demonstrates that images and images fields only partly describe the EM‐fields in quantum mechanics. The vector potential also has to be retained for a complete description of the EM‐field quantum mechanically [J.3, J.16, J.17]. However, to solve the classical electromagnetic problems, such as guided wave propagation and radiation from antenna, Heaviside formulation of Maxwell equations and potential functions as additional tools is adequate.

      EM‐Modeling of Medium

      The above brief review omitted developments in the electromagnetic properties of the material medium. A few important developments could be summarized. In 1837, Faraday introduced the concept of the dielectric constant of a material. In 1838, he introduced the concept of electric polarization images in dielectrics under the influence of the external electric field. Soon after the discovery of the electron in 1897 by J.J. Thomson, the models around electrons were developed to describe the electromagnetic properties of a material. Around 1898, John Gaston Leathem obtained an important relation images, connecting the displacement of charges in a material with polarization. Kelvin, in the year 1850, developed the concept of magnetic permeability and susceptibility with separate concepts of images, images, and images to characterize a magnetic material. In 1900, Drude developed the electrical conduction model, now known as the Drude model, after electron theory. Subsequently, the model was extended to the dielectric medium by Lorentz in 1905. The model called the Drude‐Lorentz model explains the dispersive property of dielectrics. In the year 1912, Debye developed the concept of dipole moment and obtained equations relating it to the dielectric constant. These models laid the foundation to study of the electric and magnetic properties of natural and engineered materials under the influence of external fields [B.4, B.6, B.7, B.12]

      1.1.3 Development of the Transmission Line Equations

      Kelvin's Cable Theory

      During the period 1840–1850, several persons conceived the idea of telegraph across the Atlantic Ocean. Finally, in the year 1850, the first under‐sea telegraphy, between Dover (Kent, England) and Calais (France), was made operational. However, no cable theory was available at that time to understand the electrical behavior of signal transmission over the undersea cable.

      In 1854, Kelvin modeled the under‐sea cable as a coaxial cable with an inner conductor of wire surrounded by an insulating dielectric layer, followed by the saline sea‐water acting as the outer conductor [J.18, B.1]. The coaxial cable was modeled by him as a distributed RC circuit with the series resistance R per unit length (p.u.l.) and shunt capacitance C p.u.l. It was the time of the fluid model of electricity. Kelvin further conceived the flow of electricity similar to the flow of heat in a conductor. Fourier analysis of 1D heat flow was in existence since 1822. Following the analogy of heat equation of Fourier, Kelvin obtained the diffusion type equation for the transmitted voltage signal over the under‐sea coaxial cable:

      Heaviside Transmission Line Equation

      The limitation of the speed of telegraph signals was not understood at that time. The RC model of the cable, leading to the diffusion equation, and use of the time‐domain pulse could not explain it. Moreover,

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