Regional Core-Filtered Scalar–QTDS Theorem
Record
Date: 2026-08-13
Status: the contact theorem of entry 26 extends to every partial physical core at all even multiplicity. After fixing the set of propagators that remain uncancelled, the scalar associated grade and the complete QTDS period have the same occurrence-resolved Laurent polynomial. Both sides factor canonically over the even polygonal regions cut out by that core, and the direct Catalan bijection tensors over those regions.
This closes the complete coefficient-level transfer. It does not yet give one cellular or twisted-chain map compatible with incidence between different cores. That assembly problem, and the subsequent filtered Pochhammer/Cousin comparison, are the remaining Nima frontier.
Forward status: entries 28–75 construct the complete scalar incidence envelope, close every transverse mixed square, and reduce the first nontransverse eight-point comparison to one normalized torsion-free derived route class. The remaining local datum is its occurrence-decorated extension from the physical four-facet belt across the two source caps and source cube.
Setup
Let (n=2m\geq 4), with the vertices of the cyclic polygon colored alternately. A diagonal is
- scalar when its endpoints have the same color;
- physical when its endpoints have opposite colors.
For a scalar triangulation (T), write
[ P(T)={e\in T:e\text{ is physical}} ]
for its physical core. A partial physical core (P) is any noncrossing collection of physical diagonals that extends to a quadrangulation. Put
[ p=|P|, \qquad r=p+1. ]
Cutting the polygon along (P) produces (r) even polygonal regions
[ \mathcal R(P)={R_1,\ldots,R_r}. ]
If (|R_i|=2m_i), then the elementary polygon count gives
[ \sum_{i=1}^{r}|R_i|=2m+2p ]
and therefore
[ \sum_{i=1}^{r}(m_i-2) =m-p-2. ]
The right-hand side is the number of propagators that must be cancelled in a full quadrangulation containing (P).
Exact-core scalar cells factor over regions
A scalar triangulation has exact physical core (P) if and only if it is obtained by choosing, independently in every region (R_i), a zero-core scalar triangulation (T_i). Thus
[ {T:P(T)=P} \simeq \prod_{R\in\mathcal R(P)} Z_R, ]
where (Z_R) is the zero-core set of the even polygon (R).
The propagators belonging to (P) are unshifted. Every other propagator is shifted in the alternating scalar normal direction. A triangulation with (p) physical diagonals contains
[ 2m-3-p ]
shifted scalar diagonals. Its lowest power of the normal parameter is therefore (t^{2m-3-p}). Reaching the distinguished associated grade (t^{2m-2}) requires
[ (2m-2)-(2m-3-p)=p+1=r ]
excess powers.
Regional leading cancellation
For one even region (R), the zero-core scalar series has two parity sheets. Its lowest coefficient cancels between the sheets: every zero-core cell has an odd number of scalar diagonals, the two sheets carry opposite products of shift signs, and the two Catalan sets have the same cardinality.
Consequently every region must contribute at least one excess power. There are exactly (r) regions and exactly (r) available excess powers, so the global associated grade is forced to take precisely the first nonzero coefficient from every region.
Entry 26 computed that first regional coefficient. Define the marked contact polynomial
[ C_R
-\sum_{T\in Z_R}\ \sum_{d\in T}X_d. ]
Then the scalar grade at exact core (P) is
[ \boxed{ \left[\operatorname{gr}{R}A{\rm scalar}\right]_P
\frac{1}{\prod_{e\in P}X_e} \prod_{R\in\mathcal R(P)}C_R. } ]
Equivalently, before collecting repeated monomials it is
[ \frac{(-1)^r}{\prod_{e\in P}X_e} \sum_{(T_R,d_R){R\in\mathcal R(P)}} \prod{R\in\mathcal R(P)}X_{d_R}. ]
This is an occurrence-level factorization, not merely a polynomial identity after collecting equal diagonal labels.
QTDS with a retained core
Let (Q\supseteq P) be a full quadrangulation and let (\Gamma_Q) be its dual tree, directed by one of the two alternating coorientations. To extract the Laurent sector whose remaining denominator support is exactly (P):
- retain the propagators (X_e^{-1}) for (e\in P);
- cancel every propagator belonging to (Q\setminus P) against a linear QTDS vertex numerator;
- select no numerator term proportional to an edge of (P).
Delete from (\Gamma_Q) the dual edges labelled by (P). The resulting forest has
[ r=p+1 ]
components. Within each component, the vertex-local identity of entry 26 says that an internal propagator can be cancelled only at the source of its directed edge.
A component with (v) vertices has (v-1) propagators to cancel. Since every QTDS vertex numerator is linear, those cancellations can be chosen at distinct vertices if and only if the component has a unique sink. When it does:
- each non-sink vertex cancels its unique outgoing propagator;
- the sink vertex remains and contributes either of its two scalar diagonals.
Write these two diagonals as (d_C^0,d_C^1) for a component (C). The exact contribution of the diagram (Q) at retained core (P) is therefore
[ \boxed{ \left[A_{Q}^{\epsilon}\right]_{\operatorname{den}=P}
\frac{(-1)^{p+1}}{\prod_{e\in P}X_e} \prod_{C\in\pi_0(\Gamma_Q\setminus P)} \left(X_{d_C^0}+X_{d_C^1}\right) } ]
when every component has a unique sink, and it is zero otherwise.
The sign follows directly. There are
[ (m-2)-p ]
cancelled propagators, each contributing a minus sign, while the diagram convention contributes ((-1)^{m-1}). Their product is
[ (-1)^{m-1+m-2-p} =(-1)^{p+1} =(-1)^r. ]
Regional Catalan product bijection
Fix (P) and a polarity (\epsilon). In every region (R), entry 26 gives the direct marked Catalan bijection
[ \Phi_{\epsilon|R}: (T_R,d_R) \longleftrightarrow (Q_R,d_R)_{\rm sink}. ]
The restriction (\epsilon|R) is again an alternating coorientation because every region has even size and every cut edge joins opposite colors.
Take the Cartesian product over all regions:
[ \Phi_{\epsilon,P}
\prod_{R\in\mathcal R(P)}\Phi_{\epsilon|R}. ]
On the source side this chooses one marked zero-core scalar triangulation in every region. On the target side the regional quadrangulations join with (P) to form a unique full quadrangulation (Q\supseteq P); after deleting (P), every component has a unique sink, with the prescribed marked scalar slot. The inverse is obtained simply by restricting (Q) to its regions and applying the regional inverse of entry 26.
Hence
[ \boxed{ \prod_{R\in\mathcal R(P)} {(T_R,d_R)} \simeq \left{ (Q,(d_C)): Q\supseteq P, \ \Gamma_Q\setminus P \text{ has one sink per component} \right}. } ]
The bijection preserves every marked diagonal, every remaining propagator, and the common sign ((-1)^{p+1}). It therefore identifies scalar and QTDS terms occurrence by occurrence.
Core-filtered theorem
Summing the preceding diagram formula over all (Q\supseteq P), and using the regional Catalan product bijection, gives for every partial physical core and either polarity
[ \boxed{ \left[\operatorname{gr}{R}A{\rm scalar}\right]_P
\left[A_{\rm QTDS}^{\epsilon}\right]_{\operatorname{den}=P}. } ]
Summing over all partial cores gives the complete cyclic period identity
[ \boxed{ \operatorname{gr}{R}A{\rm scalar}
A_{\rm QTDS}^{\epsilon}. } ]
This statement is stronger than the earlier reconstruction of the same amplitude from an ordering basis. It identifies:
- exact denominator support;
- full quadrangulation carrier;
- one marked scalar numerator in every cut region;
- coefficient and sign;
- factorization into regional occurrences.
The two QTDS polarities give the same complete period because both are identified with the same scalar grade. Their presentations remain distinct lifts exchanged by one-step rotation.
Cut monoidality at fixed core
The theorem supplies a precise coefficient-level form of factorization naturality. Cutting on all edges of (P) gives
[ \left[\operatorname{gr}{R}A{\rm scalar}\right]_P
\frac{1}{\prod_{e\in P}X_e} \bigotimes_{R\in\mathcal R(P)} C_R, ]
and the QTDS directed forest gives the identical tensor product. Thus the scalar transfer is monoidal on every fixed cut stratum.
No inverse of a singular full-amplitude pairing is used here. The statement lives directly on the Laurent/associated-grade stratum and is therefore compatible with the nearby-cycle warning of entry 13: one works on the induced channel sector rather than trying to invert the residue of the global BAS matrix.
What the theorem does not yet assemble
For every fixed (P), the regional transfer (\Phi_{\epsilon,P}) is canonical. It does not automatically follow that these maps commute with the boundary maps relating different cores. If a new physical edge (e) is added, one region splits into two and the required comparison is schematically
[ \Phi_{\epsilon,P} \quad\stackrel{?}{\longrightarrow}\quad \Phi_{\epsilon,P\cup{e}}
\Phi_{\epsilon,R_L}\otimes\Phi_{\epsilon,R_R}. ]
The coefficient theorem proves equality after applying the augmentation that remembers Laurent monomials. It does not yet provide the higher chain witnessing compatibility before that augmentation.
Accordingly, none of the following is claimed here:
- a single cellular chain map on the full scalar presentation complex;
- compatibility with every core-incidence differential;
- a filtered map to loaded Pochhammer or logarithmic Cousin chains;
- equality of scalar and ((\operatorname{Pf}’A)^2) representatives before cohomology;
- a canonical twisted-form representative at resonant boundary kinematics.
The known genus-zero inverse-pairing argument still identifies the induced cohomology class with
[ [(\operatorname{Pf}’A)^2] ]
at generic kinematics. The result of this entry supplies the missing all-core factorization naturality of its scalar-derived period presentation, not the final worldsheet chain comparison.
Exact finite certificate
An independent standard-library audit computes the same core-filtered Laurent polynomial in four ways:
- the raw scalar (t^{n-2}) associated-grade coefficient, grouped by exact physical core;
- the product of regional zero-core marked-contact polynomials;
- the raw symbolic QTDS numerator expansion, grouped by remaining denominator support;
- the componentwise unique-sink formula.
The exact results are:
| (n) | partial physical cores | collected Laurent monomials |
|---|---|---|
| 4 | 1 | 2 |
| 6 | 4 | 18 |
| 8 | 21 | 204 |
| 10 | 126 | 2,640 |
| 12 | 818 | 36,942 |
Both polarities agree in all four constructions. These computations are regression certificates; the all-arity theorem follows from regional leading cancellation, the vertex-local QTDS identity, and the product Catalan bijection.
Reproducible audit
Run:
python research/nima/check_core_filtered_transfer.py
The script uses exact rational coefficients and formal planar variables. It does not substitute random kinematics or infer equality numerically.
The supporting all-arity local certificates remain:
python research/nima/check_scalar_catalan_map.py
python research/nima/check_scalar_sink_qtds.py
python research/nima/check_qtds_vertex_cancellation.py
What is now established
- exact-core scalar cells factor as zero-core cells over even cut regions;
- regional leading cancellation forces one marked scalar contact in every region;
- the complete scalar associated grade has a closed formula at every partial core;
- the QTDS retained-core sector is governed by one sink in every forest component;
- the QTDS sign is ((-1)^{|P|+1});
- the direct Catalan map tensors over regions and is explicitly invertible;
- scalar and QTDS presentations agree occurrence by occurrence at every partial core;
- fixed-core factorization/cut monoidality holds at all even multiplicity;
- summing the core filtration recovers the complete QTDS period for either polarity.
Primary next test
Build the incidence complex whose objects are partial physical cores and whose local coefficient objects are the regional marked Catalan complexes. Then solve the first nontrivial compatibility square for
[ P\subset P\cup{e,f} ]
in the two possible orders. The required datum is a deck-equivariant higher homotopy between the two tensor-factorization routes, with the already proved regional maps fixed on every stratum.
At eight points this must recover the zero octagonal contact curvature of entry 24. At ten and twelve points it gives the first test not implied by coefficient equality. Only after this incidence assembly succeeds should the construction be transported to the filtered Pochhammer/Cousin complex.
Decision
Promote:
The complete core-filtered associated grade of the scalar master is canonically identical, at occurrence and coefficient level, to the complete QTDS period. The transfer is the regional tensor product of the marked Catalan bijection, and its factorization law is the one-sink rule on every component of the directed dual forest.
The primary Nima frontier is no longer construction of the scalar-derived QTDS coefficients. It is the assembly of these canonical regional transfers into one core-incidence chain map, followed by the filtered scalar-to-worldsheet comparison.