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An ambient isotopy preserves the orientation of an invariant round sphere

Statement

Let H:R3×I→R3 be an ambient isotopy with H0=id (Smooth isotopies, diffeotopies and ambient isotopies) and suppose H1 maps the closed unit ball B3⊆R3 to itself. Then H1 restricts to a diffeomorphism of the unit sphere S2=∂B3 of degree +1; that is, H1∣S2 preserves the boundary orientation of S2 (Induced boundary orientation). Consequently, if r:R3→R3 is a linear reflection in a plane through the origin (so det⁡r=−1 and r preserves S2), there is no such ambient isotopy with H1∣S2=r∣S2.

Facts & Assumptions

Given: An ambient isotopy H:R3×I→R3 with H0=id and H1(B3)=B3.

[F1]

Each Ht is a diffeomorphism of R3 and H is smooth; in particular every differential dHt(x) is an invertible linear map (Smooth isotopies, diffeotopies and ambient isotopies, Diffeomorphisms and local diffeomorphisms of manifolds).

[F2]

The entries of the Jacobian matrix of the smooth map (x,t)↦Ht(x) are partial derivatives of a C∞ function of several variables and are therefore continuous; the determinant is a polynomial in the matrix entries (Ck maps and multi-index derivative notation in Euclidean space, Directional derivatives and partial derivatives of a map U⊆Rm→Rn, For every fixed finite size at least one, the determinant of a real square matrix is a polynomial in its matrix entries).

[L1]

A continuous real function on I=[0,1] that never vanishes and is positive at 0 is positive everywhere (Intermediate value theorem, by bisection with a canonical left-half rule: a continuous function on [a,b] takes every value between f(a) and f(b)).

[L2]

A diffeomorphism of manifolds with boundary maps the boundary onto the boundary and the interior onto the interior (Diffeomorphisms preserve interior and boundary).

[L3]

The boundary orientation of S2=∂B3 is the outward-normal-first orientation of Induced boundary orientation applied to the oriented closed ball; S2 is a nonempty connected orientable boundaryless manifold (Orientable manifolds).

[L4]

A diffeomorphism between nonempty connected oriented boundaryless manifolds has degree +1 if it preserves orientation and −1 if it reverses it (Degree of an orientation-preserving or reversing diffeomorphism). A linear reflection r with det⁡r=−1 restricts to a diffeomorphism of S2 that reverses the outward-normal-first boundary orientation, since r maps the ball onto itself, carries outward normals to outward normals, and reverses the ambient orientation; hence r∣S2 has degree −1 by the same proposition.

Proof

technique · direct
1.1F1F2L1

Fix x∈R3 and put φ(t):=det⁡dHt(x) for t∈I. The function φ is continuous on I by [F2], and it never vanishes because each dHt(x) is invertible by [F1]; since φ(0)=det⁡id=1>0, the intermediate value property [L1] gives φ(t)>0 for every t∈I. Hence dHt(x) is orientation-preserving at every (x,t), and in particular H1 preserves the orientation of R3 at every point.

2.1F1L2step 1.1

Since H1 is a diffeomorphism and H1(B3)=B3, [L2] shows that H1 maps the interior of B3 onto the interior and the sphere S2=∂B3 onto itself; thus H1∣S2:S2→S2 is a diffeomorphism. Moreover dH1 carries the outward transverse direction of S2 at each p to the outward transverse direction at H1(p): the interior maps to the interior, so a tangent vector pointing into the ball maps to a vector pointing into the ball, and an outward transverse vector maps to an outward transverse vector: the inward boundary coordinate of the image vanishes at the boundary, is positive on the interior side, and has nonzero normal derivative by invertibility, so that derivative is positive. Orthogonality to the sphere need not be preserved.

3.1L3L4step 1.1step 2.1

The restriction H1∣S2 preserves the outward-normal-first boundary orientation of [L3]: if (v1,v2) is a positive basis of TpS2, so that (np,v1,v2) is a positive basis of TpR3 with np outward, then step 1.1 makes (dH1(np),dH1(v1),dH1(v2)) positive at H1(p), and dH1(np) is an outward vector by step 2.1, so (dH1(v1),dH1(v2)) is a positive basis of TH1(p)S2. Hence H1∣S2 is an orientation-preserving diffeomorphism of S2, and [L4] gives deg⁡(H1∣S2)=+1.

4.1L4step 3.1∎

Let r:R3→R3 be a linear reflection, det⁡r=−1, preserving S2. By [L4] the restriction r∣S2 reverses the boundary orientation and has degree −1, while every diffeomorphism H1∣S2 arising as above has degree +1 by step 3.1; therefore H1∣S2=r∣S2 is impossible, and no such ambient isotopy can restrict to the reflection.

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