Yang–Mills Dynamics from Projective Spectral Entropy

Q12 carries out the vertical variation of the projective spectral entropy $S_\Pi[g,\mathcal{A}]$ and derives the Yang–Mills equations from the Seeley–DeWitt coefficient $a_4$. Together with the horizontal metric variation, this completes the spectral derivation of gravity and gauge response from one functional on supplied geometric and gauge data. Q12's vertical theorem holds at a supplied fixed base metric and is conditional on a supplied compact gauge group and admissible connection; its emergent-base reading requires the unestablished hypothesis [H-L].

Overview

The Gravity paper showed that the horizontal variation of the projective spectral entropy functional \[ S_\Pi[g] = \tfrac{1}{2}\log\det' A_g \] with respect to the base metric produces the Einstein tensor as the infrared-dominant response, via the Seeley–DeWitt coefficient $a_2$.

Q12 carries out the complementary vertical variation. The operator $A_g$ is extended to \[ A_{g,\mathcal{A}} = -(\nabla^{\mathcal{A}})^2 + E \] on the vector bundle associated with a supplied compact gauge group, and the Seeley–DeWitt coefficient $a_4$ is computed. Q12 does not select that group.

The extended functional $S_\Pi[g,\mathcal{A}]$ contains the renormalized Yang–Mills term with logarithmic coupling, and its vertical variation yields the Yang–Mills equations $D_\mu F^{a\mu\nu} = 0$ in the current-free sector.

Status distinction. The $a_4$ calculation and vertical theorem hold at a supplied fixed metric. Identifying that metric with the Cosmochrony emergent base $g^{\mu\nu}=2\eta^{\mu\nu}$ is separately conditional on [H-L].

Core contributions

Spectral stratification as an organisational principle

Beyond the technical derivation, Q12 identifies a conceptual principle that distinguishes the Cosmochrony approach from conventional unification schemes.

In standard group-theoretic unification, gravity and gauge interactions are sought at the same algebraic level — different representations of a common group $G_{\mathrm{unif}}$. Their combination requires finding a symmetry large enough to accommodate both.

The present framework suggests a different picture: gravity and gauge dynamics are separated by geometric direction (horizontal vs. vertical variation on the admissible bundle) and by spectral order ($a_2$ vs. $a_4$ in the Seeley–DeWitt hierarchy). Their distinct UV behaviours — quadratic divergence for gravity, logarithmic for gauge — are structural consequences of this separation, not independent empirical inputs.

Implication for unification. The difficulty of incorporating gravity into the Standard Model framework may reflect a difference of Seeley–DeWitt order rather than the absence of a common symmetry group. The natural organisational space for unification in this framework is spectral and variational, not primarily group-theoretic.

Relation to the Cosmochrony programme

Q12 is the vertical counterpart to the Gravity paper. Each sector follows from the same functional by varying in a different direction; joining the two variations, and the conditional system that results, belongs to Q13:

The compact gauge group and connection are hypotheses of the vertical construction. O31 version 2.0 withdraws the claimed colour co-admissibility and $\mathrm{SU}(3)$ identification, so Q12 establishes no colour factor or complete Standard Model gauge group.

The joint variation — the conditional Einstein–Yang–Mills system and the $a_4$-order back-reaction $T^{\mathrm{YM}}_{\mu\nu}$ — is carried out in Q13, where the couplings likewise remain independent renormalized matching data, so no numerical value for $G_N g_{\mathrm{YM}}^2$ follows.

Open directions

References

Jérôme Beau. Yang–Mills Dynamics from Projective Spectral Entropy: Vertical Heat-Kernel Variation on the Admissible Fibre, 2026. doi:10.5281/zenodo.20189137