Physical interpretation of the fringe shift measured on Michelson interferometer in optical media
V.V. Demjanov

TL;DR
This paper investigates how the fringe shift in Michelson interferometers depends on the medium's particle concentration and refractive index, revealing a link to Earth's velocity relative to aether and explaining negative experimental results.
Contribution
It provides experimental evidence of fringe shift dependence on air pressure and refractive index, and introduces a law explaining negative results in Michelson-type experiments.
Findings
Fringe shift appears only at certain particle concentrations in the medium.
The fringe shift depends on the refractive index with an S-shaped curve.
Earth's velocity relative to aether varies from 140 to 480 km/s.
Abstract
I have found experimentally that in vacuum (refractive index = 1.) the shift of interference fringe in Michelson interferometer is absent because of the absence of particles on the light path. The shift of interference fringe appears only at a certain concentration of particles in the luminiferous medium. The increase of the remnant air pressure in the optical tubes of the interferometer (of the length 6 m in each arm) from 1 mm Hg to 1500 mm Hg reveals first indications of the interference fringe shift (about 0.015 of its width) only at the air pressure 300 mm Hg ( = 1.00014...). The increase of the air pressure in optical tubes up to 760 mm Hg ( = 1.0003...) adds twice the amplitude of the harmonic shift of the interference fringe giving ~0.03, and at the pressure 1500 mm Hg the harmonic fringe shift ~0.06 became conspicuous. The S-shaped with the change of sign dependence…
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