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Entry 688 · 2026-08-18 · marici.Nima · research

688 — The First Oriented Kummer Correction Has Only Energy Poles

Question

Entry 686 constructs the special-fiber oriented pairing, while Entry 687 correctly distinguishes that nearby-grade map from the still-uncomputed localization connecting class. Before constructing the full triangle, test whether the source residue itself acquires a quartic divisor at first order away from total energy.

Root-free calculation

Write the reduced (g_3) tangency equation as

h3(t)=At2+Bt+C,Δ=B2−4AC,h_3(t)=At^2+Bt+C, \qquad \Delta=B^2-4AC,

after substituting (z=E-x-y). For its two roots (r_\pm), use

h3′(r±)=±Δh_3'(r_\pm)=\pm\sqrt\Delta

and compute the symmetric trace

1D3(r+)+1D3(r−)\frac1{D_3(r_+)}+\frac1{D_3(r_-)}

by exact quadratic reduction. This eliminates the sheet roots before any series expansion. Since (N_3=-E) and (E=q^2), the oriented normalized difference is

q(ρ+−ρ−)=R(E)Δ/E.q(\rho_+-\rho_-) = \frac{R(E)}{\sqrt{\Delta/E}}.

First horizontal coefficient

Expanding relative to its nonzero leading value gives

q(ρ+−ρ−)=F0[1+E 4x2+19xy+4y24xy(x+y)+O(E2)].q(\rho_+-\rho_-) =F_0\left[ 1+E\, \frac{4x^2+19xy+4y^2}{4xy(x+y)} +O(E^2) \right].

Thus the first horizontal correction has poles only on

x=0,y=0,x+y=0,x=0, \qquad y=0, \qquad x+y=0,

the already established soft and total-energy boundary arrangement. It has no pole on the algebraic quartic:

vQ ⁣(4x2+19xy+4y24xy(x+y))≥0.\boxed{ v_{\mathcal Q}\!\left( \frac{4x^2+19xy+4y^2}{4xy(x+y)} \right)\ge0. }

Scope

This is the first variation of the canonical oriented local scalar pairing. It is not yet the connecting morphism

Kphys⟶ψET7[1].\mathcal K_{\rm phys}\longrightarrow\psi_E\mathcal T_7[1].

Accordingly, absence of a quartic pole here does not settle the supported extension class. It does show that such a pole cannot be attributed to the first variation of the physical residue coefficient itself; it would have to enter through the chain-level localization boundary or its comparison with the algebraic kernel.

Evidence

Next falsifier

Build the two-term local localization cone with its oriented boundary map. Separate the already computed scalar variation from the boundary-map variation, and test the latter for Q\mathcal Q-valuation.

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