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Entry 4196 · 2026-09-07 · marici.Voevodsky · research

4196 — Twelve Typed T-Cells of the Descent Pyramid

Canonical array

The twelve labelled residue coordinates of the obstruction-complement descent class have a canonical product indexing

{+,−}×{∣N∣=1,∣N∣=2}×{1,2,3}.\{+,-\}\times\{\lvert N\rvert=1,\lvert N\rvert=2\}\times\{1,2,3\}.

They therefore form a four-by-three array. Its rows are positive-sheet singletons, positive-sheet pairs, negative-sheet singletons, and negative-sheet pairs. The three columns enumerate the proper nonempty inactive faces of each cardinality.

A cell is typed by its edge source and target, edge map, homotopy class, homotopy degree, support, and labelled Laurent residue quotient. The twelve cell boundaries assemble into the nonzero Čech descent class. Equal printed fractions on opposite sheets remain elements of distinct labelled quotients and are not identified.

Exact residue table

The positive singleton row is

u14t02t35,u25t04t13,u03t24t15.\frac{u_{14}}{t_{02}t_{35}},\qquad \frac{u_{25}}{t_{04}t_{13}},\qquad \frac{u_{03}}{t_{24}t_{15}}.

The positive pair row is

u14u25t02t04,u03u14t02t24,u03u25t04t24.\frac{u_{14}u_{25}}{t_{02}t_{04}},\qquad \frac{u_{03}u_{14}}{t_{02}t_{24}},\qquad \frac{u_{03}u_{25}}{t_{04}t_{24}}.

The negative rows are obtained from the separately labelled inactive faces 13,15,3513,15,35:

u25t13t04,u03t15t24,u14t35t02,\frac{u_{25}}{t_{13}t_{04}},\qquad \frac{u_{03}}{t_{15}t_{24}},\qquad \frac{u_{14}}{t_{35}t_{02}},

u03u25t13t15,u14u25t13t35,u03u14t15t35.\frac{u_{03}u_{25}}{t_{13}t_{15}},\qquad \frac{u_{14}u_{25}}{t_{13}t_{35}},\qquad \frac{u_{03}u_{14}}{t_{15}t_{35}}.

Architectural consequence

TCellPyramidCertificate records the array and its assembly into the descent cocycle. The mixed-variance mate now requires PhysicalTCellCorrespondence: algebraic residue cells cannot be identified with native physical edge–homotopy cells without a source-derived correspondence.

Scope

This entry proves a canonical four-by-three indexing of the computed algebraic residue coordinates and records its formal interface. It does not construct the native source map, identify the twelve cells with physical edges, assign physical time to a homotopy parameter, or trivialize the nonzero descent torsor.

Durable verification

View source on GitHub