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DerivedAlgGeo.CategoryTheory.Triangulated.StabilityCondition.Mukai.GeometricInput

Geometric inputs for the Mukai tilt argument #

The abstract weak-slope and Mukai-charge layers determine the imaginary part of the tilted-heart positivity argument. Two genuinely geometric statements remain before the exponential charge is a stability function:

This file names those obligations without adding them to MukaiChargeData or MukaiWeakSlopeCompat. They are object-classification results, not part of the definition of a charge or of its compatibility with slope. A geometric K3 specialization can discharge the first from support dimension and ampleness, and the second from stable factors plus the stable-sheaf Mukai-square bound.

The contracts are propositions rather than a bundled structure. They can be proved independently, and consumers that need only one do not acquire the other as an artificial field.

The boundary contract is parameterized by a predicate on the factors: HasBoundaryMukaiDecompositionWith P asks only for a nonempty decomposition into positive-rank factors at the cutoff, each satisfying P. Which predicate a surface can supply, and why it forces Re Z > 0, is decided by the consumer; Mukai/Tilting.lean proves it for the exact Hodge margin and for a uniform lower bound realForm ≥ -δ. The margin and δ contracts are abbreviations of the parent, and the K3 contract is only the child specialization δ = 1.

The rank-zero torsion classification needed by the tilt argument.

Only the residual boundary case is assumed: rank and degree both vanish. Positive-degree rank-zero torsion is already in the open upper half-plane by MukaiWeakSlopeCompat.im_charge_eq_degree_of_rank_zero.

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    Boundary decomposition into factors satisfying a predicate.

    This is the parent contract of the boundary case. A nonzero object of the torsion-free class sitting exactly on the cutoff must admit a nonempty finite family of factors whose Mukai classes sum to its class, each of positive rank, each on the cutoff, and each satisfying P. Positive rank and the cutoff slope are what put every factor on Im Z = 0; they are not surface-specific. The predicate P is the only surface-specific input, and the contract does not say how P forces Re Z > 0: a consumer proves that separately and hands it to MukaiWeakSlopeCompat.mem_semiClosedUpperHalfPlane_of_shift_hnFree_of_pred.

    For coherent sheaves the factors are the Jordan--Hölder factors of a μ-semistable sheaf (an object of the torsion-free class whose slope equals the cutoff is forced to be semistable), and P records whatever bound the surface provides for a stable sheaf. Different surfaces differ only in P.

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      The factorwise input under the exact boundary margin.

      The predicate is the exact quantity the Hodge-index estimate places below 2 * r * Re Z:

      0 < 2 * realForm b v + rank(v)² * b ω ω.

      Different factors may use different bounds, and no integrality estimate or global constant is encoded. Surface-specific APIs can prove this directly or derive it from a more recognizable inequality such as realForm ≥ -δ.

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        The factorwise Mukai input at the torsion-free boundary, with an arbitrary lower bound.

        Every factor is required to have realForm at least -δ. No stability predicate is invented here: once a geometric Jordan--Hölder API exists, its stable factors should be used to prove this proposition.

        The lower bound is parameterized because -1 is the K3/2-CY value coming from the stable-simple self-Ext argument, not part of boundary factorization itself. It remains factorwise because a quadratic lower bound is not additive.

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          The historical K3-normalized boundary contract.

          This is the δ = 1 specialization of HasBoundaryMukaiDecompositionWithLowerBound. It remains as a named wrapper so existing K3 consumers keep their API while new surface realizations choose their own geometric lower bound explicitly.

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