The Ideal Stratum and Deformation Persistence of Knot Types
Abstract
We study a knot type through the ropelength-filtered spaces of its thick representatives. For a knot type and a scale parameter , let be the space of representatives of with thickness at least and length at most , modulo reparametrization and orientation-preserving Euclidean isometries. The basic equivalence relation is defined by admissible deformations: two representatives are equivalent at scale if they can be joined through representatives that remain in . The resulting admissible components form a one-parameter persistence object as increases. We prove that the first birth level of this admissible-component persistence is exactly the ropelength . The initial layer is the ideal stratum of . Thus the ropelength-minimizing locus is not treated merely as a set of ideal shapes, but as the birth stratum of a constrained deformation theory. We define the ideal admissible-component set , the ideal component number , and pairwise ideal merge scales. For the fixed knot type , the central invariant introduced here is the ropelength ultrapseudometric defined for . We prove that this function is finite-valued and satisfies the strong triangle inequality. The pure merge Vietoris--Rips filtration is a secondary simplicial encoding of this ultrapseudometric structure: it records the same zero-dimensional merge data and has no higher-dimensional homological content beyond the merge partition itself. We also compute the basic case of the unknot and indicate finite polygonal and diagrammatic approximations as further directions.
Cite
@article{arxiv.2604.17905,
title = {The Ideal Stratum and Deformation Persistence of Knot Types},
author = {Makoto Ozawa},
journal= {arXiv preprint arXiv:2604.17905},
year = {2026}
}
Comments
21 pages, LaTeX. Revised version. Streamlined exposition; clarified admissible-component persistence, ideal merge scales, the merge ultrapseudometric, and pure merge Vietoris--Rips filtration