Alphabeta Math
Pipeline-generated
How statement and proof provenance work

The first chip identifies the source of the statement or construction; the second identifies the source of its local proof or verification.

  • Literature-sourced: the exact statement appears in a cited source; only wording and notation differ.
  • AI-adapted: a semantically identical restatement of literature-sourced material, modulo indexing, notation, and boundary cases adopted by the library.
  • AI-generated: a genuinely novel statement formulated by AI, with no source for the claim itself.

These labels describe origin, not correctness: citations and verification chips remain separate evidence.

Gradient Like Vector Fields and Morse Trajectories — Examples

1 · Prerequisites

None. This page is self-contained.

2 · Summary

These calculations test the descending sign, endpoint geometry, and the noncompact completeness qualification without imposing Morse--Smale transversality.

3 · Logical flowchart

4 · Definitions, theorems and proofs

None yet.

5 · Examples, counterexamples and false statements

ExampleConstruction: Literature-sourcedVerification: Literature-sourcedjudge pass (gpt-5.6-terra)audited 2026-09-06Open item page →

Negative-gradient lines for a quadratic Morse function

Example

On Rr×Rs with its Euclidean metric, let f(u,v)=−∣u∣2+∣v∣2. Its negative-gradient equation is

u˙=2u,v˙=−2v.

Verification

Given: The quadratic function f(u,v)=−∣u∣2+∣v∣2 on Euclidean space.

1.1givenalgebra

Solving the separated equations gives u(t)=e2tu0 and v(t)=e−2tv0. Thus the forward-stable coordinate disk is {u=0} and the backward-unstable disk is {v=0}.

2.1step 1.1algebra∎

Directly, ddtf(u(t),v(t))=−4∣u(t)∣2−4∣v(t)∣2, which is strictly negative away from the origin.

ExampleConstruction: Literature-sourcedVerification: Literature-sourcedjudge pass (gpt-5.6-terra)audited 2026-09-06Open item page →

Meridian trajectories for height on the sphere

Example

On the round S2⊂R3, let f(x,y,z)=z. The intrinsic gradient is grad⁡f=ez−z(x,y,z), so the negative gradient is z(x,y,z)−ez. Its nonconstant orbits are the meridians from the north pole to the south pole.

Verification

Given: The round unit sphere and the height function f(x,y,z)=z.

1.1givenalgebra

The tangential projection of ez is ez−z(x,y,z), so the displayed vector field is the negative gradient. Along it, z˙=z2−1<0 whenever ∣z∣<1.

2.1step 1.1∎

The longitude is constant along the flow, while z decreases from 1 to −1. Therefore every nonpolar longitude gives a meridian from north to south, a one-parameter family before quotienting by time translation.

ExampleConstruction: Literature-sourcedVerification: Literature-sourcedjudge pass (gpt-5.6-terra)audited 2026-09-06Open item page →

Gradient flow for a Morse function on the flat torus

Example

On the flat torus with angular coordinates (θ,ϕ), take f(θ,ϕ)=cos⁡θ+cos⁡ϕ. Its critical points are (0,0) (maximum, index 2), (π,0) and (0,π) (saddles, index 1), and (π,π) (minimum, index 0). The negative-gradient equations are

θ˙=sin⁡θ,ϕ˙=sin⁡ϕ.

Verification

Given: The flat two-torus and f(θ,ϕ)=cos⁡θ+cos⁡ϕ.

1.1givenalgebra

Differentiating gives df=−sin⁡θ dθ−sin⁡ϕ dϕ, hence the displayed negative-gradient equations. Their zeros give exactly the four listed critical points, and the diagonal Hessian diag⁡(−cos⁡θ,−cos⁡ϕ) gives the stated indices.

2.1step 1.1algebra∎

The circles θ∈{0,π} and ϕ∈{0,π} are invariant and supply the coordinate-circle separatrices. On either component of S1∖{0,π}, each nonconstant coordinate trajectory has backward limit 0 and forward limit π (it increases on (0,π) and decreases on (π,2π) in the displayed coordinate). Thus the trajectories off those circles run from the maximum to the minimum in four arc-choice components. In each component, quotienting the two integration constants by common time translation leaves a one-parameter family.

CounterexampleConstruction: Literature-sourcedVerification: Literature-sourcedjudge pass (gpt-5.6-terra)audited 2026-09-06Open item page →

Using the positive gradient reverses the stable and unstable dimensions

Statement refuted

For f(u,v)=−∣u∣2+∣v∣2, one may use the positive gradient while retaining the descending convention that the unstable dimension equals the Morse index.

Counterexample

Given: The Euclidean quadratic f(u,v)=−∣u∣2+∣v∣2 evolved by +grad⁡f.

1.1givenalgebra

The positive-gradient equations are u˙=−2u and v˙=2v, so u(t)=e−2tu0 and v(t)=e2tv0.

2.1step 1.1∎

Thus the forward-stable space is {v=0} of index dimension and the backward-unstable space is {u=0} of coindex dimension. The labels are reversed from the descending convention, refuting the assertion.

CounterexampleConstruction: Literature-sourcedVerification: Literature-sourcedjudge pass (gpt-5.6-terra)audited 2026-09-06Open item page →

A gradient flow on a noncompact manifold can be incomplete

Statement refuted

Every negative-gradient vector field on a noncompact manifold is complete.

Counterexample

Given: The Euclidean line and f(x)=−x3/3.

1.1givenalgebra

Since grad⁡f=−x2∂x, the negative-gradient field is x2∂x and its equation is x˙=x2.

2.1step 1.1algebra∎

For x0>0, the solution is x(t)=x0/(1−x0t), which tends to +∞ as t↑1/x0. Hence its maximal interval has a finite positive endpoint and the field is incomplete.

This witnesses incompleteness only: f is not offered as a Morse-function example.

Sources