Radial normalization scales the radial contact form by the inverse squared radius
ProvedBirkhoffGlobalSection.radial_normalization_contact_identitycontact-geometrydynamical-systemssymplectic-geometry
For a nonzero point , put and . The radial map is smooth near , has values in the unit three-sphere, is odd, and satisfies
where . 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.