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Within the OCEAN rheological paradigm, this paper presents a biophysical framework where biological life is modeled as a localized compaction of the Viscous Fermionic Condensate (VFC). We redefine homoeostasis and aging through the dynamics of shear resistance. The standard metabolic heat generation (36.6◦C) is derived via the Rayleigh dissipation function of hemodynamics. Biological senescence is mathematically formulated as a progressive phase transition toward infinite viscosity (petrification), establishing a direct analytical link between tissue fluidity and lifespan.
Shlyapik A. 2026. Rheological Model of Biological Systems: Life as a Balance of Ocean Viscosity. PREPRINTS.RU. https://doi.org/10.24108/preprints-3115663