The paper examines the physical properties of coherence boundaries influencing subatomic particle behavior, suggesting implications for understanding dissipation phenomena.
If frictionless persistence of subatomic particle rotation is enforced by coherence constraints in a particle-supporting environment, then dissipation and coupling to ordinary laboratory degrees of freedom must occur at a boundary where those constraints fail. This paper examines the physical properties of that boundary region, treated not as a geometric surface but as a dynamical interface between two regimes with different allowed processes. Without assuming detailed microphysics, we define a small set of operational boundary parameters—effective thickness, coupling strength, anisotropy, thresholds, dissipation localization, and memory—and show how they map onto long-standing experimental observables in nuclear, atomic, and solid-state physics. We argue that many phenomena traditionally interpreted as intrinsic nuclear or environmental effects may instead be boundary-mediated manifestations of coherence breakdown. A set of discriminating experimental signatures is presented that can distinguish boundary-dominated coupling from bulk dissipation or intrinsic-property models using existing techniques. The aim is to place the coherence-boundary concept at direct experimental risk and to clarify whether such a boundary constitutes a real physical object with measurable properties.
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Stephen Euin Cobb (2026) studied this question.
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