Surface deformation of ODEs

Given a first-order ODE u=ϕ(x,u), the associated surface can be deformed while preserving A=1 and Au. The family of metrics is parametrized by ϵ(x,u)C(U):

gϵ=(1+ϕ2e2ϵϕe2ϵϕe2ϵe2ϵ),

with orthonormal frame {A,eϵu}. The original surface corresponds to ϵ=0.

Curvature under deformation

The Gaussian curvature of Sϵ is

Kϵ=A(Δϵ)Δϵ2,whereΔϵ=A(ϵ)+ϕu.

The key observation: the second-order operator acting on normal variations along the geodesic flow A factorises as

A2+Kϵ=TϵSϵ,

into two first-order deformation operators (they encode the effect of ϵ through Δϵ):

Tϵ(h)=A(h)+Δϵh,Sϵ(h)=A(h)Δϵh.

This is the same algebraic structure as ladder operators in SUSY QM. The function Δϵ plays the role of a superpotential: A2+Kϵ is a Schrödinger-type operator factorised as (A+Δϵ)(AΔϵ).

Why the factorisation matters

The Jacobi equation for a normal component δ along A is A2(δ)+Kϵδ=0, i.e.

(TϵSϵ)(δ)=0.

Hence either Sϵ(δ)=0 or Tϵ(Sϵ(δ))=0, and each condition yields an integrating factor (see Lemma in paper):

Thus a non-trivial relative Jacobi field on any Sϵ unlocks integrability by quadratures. In particular, constant curvature Kϵ=k makes δ explicit (solve δ+kδ=0), so the deformed surface always produces a Jacobi field — see constant curvature integrability.

QM object ODE-surface analogue
Hamiltonian H=d2/dx2+V(x) A2+Kϵ
Zero-energy mode Hψ=0 A2δ+Kϵδ=0
Superpotential W Δϵ=A(ϵ)+ϕu
Ladder operators A±=d/dx+W Tϵ, Sϵ

Conceptual summary

Deformation expands the search space: instead of requiring the original surface to have special geometry (flatness, constant curvature), we can deform it via ϵ until Sϵ acquires the needed property. The deformation operators Tϵ,Sϵ track how the curvature changes and directly factor the Jacobi operator, linking geometry to integrability.

Related notes: relative Jacobi field, constant curvature integrability, Riemannian metric for a first-order ODE, Gauss curvature of an ODE-surface

Reference: @panalvarez2023surfaces