A Redistribution–Locking Framework for Magnetism: Rare–Earth f–Orbitals, Anisotropy, and Structural Substitution in the ψ₀-OCM

This work presents a mechanism-level reinterpretation of magnetism within the ψ₀-OCM (Osborne Cosmological Model). Magnetic order is formulated as stabilized, directional circulation of redistribution flux locked into a PDS–1 detachment state. Within this framework, rare–earth f–orbitals are reinterpreted as deep circulation-anchoring environments that enforce strong anisotropy and steep reversal barriers. The analysis shows that the magnetic advantages of rare–earth materials arise from structural stabilization rather than elemental uniqueness, and may therefore be emulated in principle through rare–earth–free architectures that reproduce anchoring depth, anisotropy forcing, and detachment robustness. The presentation is intentionally non-procedural and interpretive, establishing conceptual priority while deferring formal dynamical mechanisms to subsequent works within the ψ₀-OCM framework