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Radial normalization scales the radial contact form by the inverse squared radius

Proved
BirkhoffGlobalSection.radial_normalization_contact_identity

by caleb · Sep 27, 2026 · Mathlib 0df444a (Lean v4.33.1)

contact-geometrydynamical-systemssymplectic-geometry

For a nonzero point y∈R4y\in\mathbb R^4y∈R4, put N(y)=∑iyi2N(y)=\sum_i y_i^2N(y)=∑i​yi2​ and r(y)=y/N(y)r(y)=y/\sqrt{N(y)}r(y)=y/N(y)​. The radial map is smooth near yyy, has values in the unit three-sphere, is odd, and satisfies

αr(y)(Dryv)=αy(v)N(y)(v∈R4),\alpha_{r(y)}(Dr_yv)=\frac{\alpha_y(v)}{N(y)}\qquad(v\in\mathbb R^4),αr(y)​(Dry​v)=N(y)αy​(v)​(v∈R4),

where αy(v)=−ω(y,v)/2\alpha_y(v)=-\omega(y,v)/2αy​(v)=−ω(y,v)/2. In particular, radial normalization preserves positivity of contact evaluation. The identity applies to all ambient vectors and uses Euclidean squared radius independently of the norm instance on the coordinate space.

Preamble
import Definitions.Def_BirkhoffGlobalSection_TransverseHopf
open scoped ContDiff
Formal statement
namespace BirkhoffGlobalSection

theorem radial_normalization_contact_identity
    (y : Phase) (hy : 0 < zNormSq y + wNormSq y) :
    ContDiffAt ℝ ∞ radialNormalize y ∧
      radialNormalize y ∈ unitThreeSphere ∧
      radialNormalize (-y) = -radialNormalize y ∧
      ∀ v : Phase,
        phaseRadialContact (radialNormalize y) (fderiv ℝ radialNormalize y v) =
          phaseRadialContact y v / (zNormSq y + wNormSq y) := by sorry

end BirkhoffGlobalSection
Source
Direct identity from Def_BirkhoffGlobalSection_TransverseHopf: r(y)=N(y)^(-1/2)y and alpha_y(v)=-omega(y,v)/2. Bilinearity and omega(y,y)=0 give r^*alpha=N^(-1)alpha. These are the homogeneous radial contact-form conventions used in Hryniewicz–Salomão, arXiv:1505.02713v3, Section 1.3, https://arxiv.org/html/1505.02713v3.

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