Origin of the Dirac Equation: Difference between revisions
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| title = Origin of the Dirac Equation | | title = Origin of the Dirac Equation | ||
| author = [[Helena Ioannidou]] | | author = [[Helena Ioannidou]] | ||
| keywords = Dirac Equation, wave function | |||
| published = 2002 | | published = 2002 | ||
| journal = [[Galilean Electrodynamics]] | | journal = [[Galilean Electrodynamics]] | ||
| volume = | | volume = 13 | ||
| number = | | number = 4 | ||
| pages = 83-86 | | pages = 83-86 | ||
}} | }} | ||
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==Abstract== | ==Abstract== | ||
We derive the Dirac equation by means of the total derivative of the wave function, where the matrices are replaced by scalar quantities containing the velocity of the particle, avoiding thus the unsatisfactory features arising from the original four-component formulation. The corresponding quadratic equation of the proposed model preserves the extra ?spin? terms.[[Category:Scientific Paper]] | We derive the Dirac equation by means of the total derivative of the wave function, where the matrices are replaced by scalar quantities containing the velocity of the particle, avoiding thus the unsatisfactory features arising from the original four-component formulation. The corresponding quadratic equation of the proposed model preserves the extra ?spin? terms. | ||
[[Category:Scientific Paper|origin dirac equation]] | |||
Latest revision as of 09:38, 21 July 2026
| Scientific Paper | |
|---|---|
| Title | Origin of the Dirac Equation |
| Author(s) | Helena Ioannidou |
| Keywords | Dirac Equation, wave function |
| Published | 2002 |
| Journal | Galilean Electrodynamics |
| Volume | 13 |
| Number | 4 |
| Pages | 83-86 |
Abstract
We derive the Dirac equation by means of the total derivative of the wave function, where the matrices are replaced by scalar quantities containing the velocity of the particle, avoiding thus the unsatisfactory features arising from the original four-component formulation. The corresponding quadratic equation of the proposed model preserves the extra ?spin? terms.