Search engine for discovering works of Art, research articles, and books related to Art and Culture
ShareThis
Javascript must be enabled to continue!

Inhomogeneous Wave Equation, Liénard-Wiechert Potentials, and Hertzian Dipole in Weber Electrodynamics

View through CrossRef
<p>Aiming to bypass the equation of the Lorentz force, this study analyzes Maxwell's equations from the perspective of a receiver at rest. This approach is necessary because experimental results suggest that the general validity of the Lorentz force is questionable in non-stationary cases. Calculations in the receiver's rest frame are complicated, and thus, rarely performed. However, after a Lorentz boost, the resulting force should be identical to the force obtained when the problem is considered in the rest frame of the transmitter with the Lorentz force applied, as is commonly done. Yet, this is not the case. Instead, Maxwell's equations lead to Weber electrodynamics. The present article demonstrates this result by deriving and solving the inhomogeneous wave equation from Maxwell's equations. Subsequently, it is shown that the resulting force is a relativistic generalization of the Weber force. Furthermore, the Hertzian dipole, i.e., a simple antenna, is mathematically investigated and discussed from the viewpoint of Weber electrodynamics for the first time.</p>
Institute of Electrical and Electronics Engineers (IEEE)
Title: Inhomogeneous Wave Equation, Liénard-Wiechert Potentials, and Hertzian Dipole in Weber Electrodynamics
Description:
<p>Aiming to bypass the equation of the Lorentz force, this study analyzes Maxwell's equations from the perspective of a receiver at rest.
This approach is necessary because experimental results suggest that the general validity of the Lorentz force is questionable in non-stationary cases.
Calculations in the receiver's rest frame are complicated, and thus, rarely performed.
However, after a Lorentz boost, the resulting force should be identical to the force obtained when the problem is considered in the rest frame of the transmitter with the Lorentz force applied, as is commonly done.
Yet, this is not the case.
Instead, Maxwell's equations lead to Weber electrodynamics.
The present article demonstrates this result by deriving and solving the inhomogeneous wave equation from Maxwell's equations.
Subsequently, it is shown that the resulting force is a relativistic generalization of the Weber force.
Furthermore, the Hertzian dipole, i.
e.
, a simple antenna, is mathematically investigated and discussed from the viewpoint of Weber electrodynamics for the first time.
</p>.

Related Results

Inhomogeneous Wave Equation, Liénard-Wiechert Potentials, and Hertzian Dipole in Weber Electrodynamics
Inhomogeneous Wave Equation, Liénard-Wiechert Potentials, and Hertzian Dipole in Weber Electrodynamics
<p>Aiming to bypass the Lorentz force, this study analyzes Maxwell's equations from the perspective of a receiver at rest. This approach is necessary because experimental res...
Inhomogeneous Wave Equation, Liénard-Wiechert Potentials, and Hertzian Dipole in Weber Electrodynamics
Inhomogeneous Wave Equation, Liénard-Wiechert Potentials, and Hertzian Dipole in Weber Electrodynamics
<p>Aiming to bypass the Lorentz force, this study analyzes Maxwell's equations from the perspective of a receiver at rest. This approach is necessary because experimental res...
Inhomogeneous Wave Equation, Liénard-Wiechert Potentials, and Hertzian Dipole in Weber Electrodynamics
Inhomogeneous Wave Equation, Liénard-Wiechert Potentials, and Hertzian Dipole in Weber Electrodynamics
<p>Aiming to bypass the Lorentz force, this study analyzes Maxwell's equations from the perspective of a receiver at rest. This approach is necessary because experimental res...
The waveform comparison of three common-used fractional viscous acoustic wave equations
The waveform comparison of three common-used fractional viscous acoustic wave equations
Abstract The forward simulation of the viscous acoustic wave equation is an essential part of geophysics and energy resources exploration research. The viscous acoustic sei...
Hurricane Eloise Directional Wave Energy Spectra
Hurricane Eloise Directional Wave Energy Spectra
ABSTRACT Directiona1 wave energy spectra, calculated from data recorded during Hurricane Eloise (Gulf of Mexico, 1975), are presented. The spectra, based on an en...
Wave Force Calculations for Stokes and Non-Stokes Waves
Wave Force Calculations for Stokes and Non-Stokes Waves
ABSTRACT A new wave particle velocity procedure permits calculation of forces from regular wave profiles of more or less arbitrary wave crest to height ratios, as...
Wave-Equation Migration: Two Approaches
Wave-Equation Migration: Two Approaches
ABSTRACT A conventional stacked seismic section displays data only as a passing wave-field recorded at selected points on the earth's surface. In regions of compl...
Receiver Balancing In Off-Centered Acoustic Logging Data
Receiver Balancing In Off-Centered Acoustic Logging Data
Abstract Modern multi-pole acoustic logging tools require addition and subtraction of signals from different combinations of receivers. To enable the correct subt...

Back to Top