Terrestrial Experimental Evidence of a Viscous Fermionic Condensate (ψ-field)

Alexander Shlyapik

doi:10.5281/zenodo.19638180

April 18, 2026Open Access

Terrestrial Experimental Evidence of a Viscous Fermionic Condensate (ψ-field)

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Key Points

The research aims to explore the implications of the Fermionic Universe Hypothesis on local physical anomalies.
Formalization of the Fermionic Universe Hypothesis parameters including viscosity, mass, and packing coefficient.
Investigation of local physical anomalies in relation to the viscous medium described by the hypothesis.
Identification of specific physical anomalies linked to interactions with the viscous medium.
Establishment of parameters including dynamic viscosity at 1.2 × 10−15 Pa·s and mass quantum at 4.8 keV.

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Implication

Experimental evidence demonstrates physical anomalies as effects of interaction with a viscous substrate.

Abstract

IntroductionThe Fermionic Universe Hypothesis (FUH) postulates that the vacuum is a physicalviscous medium characterized by the following parameters:• Dynamic viscosity: η = 1.2 × 10−15 Pa·s.• Media mass quantum: mψ = 4.8 keV.• Packing coefficient: β = 0.618.This paper formalizes local physical anomalies as direct consequences of matter interactingwith this substrate.

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Alexander Shlyapik (2026) studied this question.

synapsesocial.com/papers/69e5c42603c2939914029c3b https://doi.org/10.5281/zenodo.19638180

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Terrestrial Experimental Evidence of a Viscous Fermionic Condensate (ψ-field)

Key Points

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Abstract

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Cite This Study

Terrestrial Experimental Evidence of a Viscous Fermionic Condensate (ψ-field)

Key Points

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Implication

Abstract

Discussion

Cite This Study

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