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An ambient isotopy preserves the orientation of an invariant round sphere
Statement
Let be an ambient isotopy with (Smooth isotopies, diffeotopies and ambient isotopies) and suppose maps the closed unit ball to itself. Then restricts to a diffeomorphism of the unit sphere of degree ; that is, preserves the boundary orientation of (Induced boundary orientation). Consequently, if is a linear reflection in a plane through the origin (so and preserves ), there is no such ambient isotopy with .
Facts & Assumptions
Given: An ambient isotopy with and .
Each is a diffeomorphism of and is smooth; in particular every differential is an invertible linear map (Smooth isotopies, diffeotopies and ambient isotopies, Diffeomorphisms and local diffeomorphisms of manifolds).
The entries of the Jacobian matrix of the smooth map are partial derivatives of a function of several variables and are therefore continuous; the determinant is a polynomial in the matrix entries ( maps and multi-index derivative notation in Euclidean space, Directional derivatives and partial derivatives of a map , For every fixed finite size at least one, the determinant of a real square matrix is a polynomial in its matrix entries).
A continuous real function on that never vanishes and is positive at is positive everywhere (Intermediate value theorem, by bisection with a canonical left-half rule: a continuous function on takes every value between and ).
A diffeomorphism of manifolds with boundary maps the boundary onto the boundary and the interior onto the interior (Diffeomorphisms preserve interior and boundary).
The boundary orientation of is the outward-normal-first orientation of Induced boundary orientation applied to the oriented closed ball; is a nonempty connected orientable boundaryless manifold (Orientable manifolds).
A diffeomorphism between nonempty connected oriented boundaryless manifolds has degree if it preserves orientation and if it reverses it (Degree of an orientation-preserving or reversing diffeomorphism). A linear reflection with restricts to a diffeomorphism of that reverses the outward-normal-first boundary orientation, since maps the ball onto itself, carries outward normals to outward normals, and reverses the ambient orientation; hence has degree by the same proposition.
Proof
Fix and put for . The function is continuous on by [F2], and it never vanishes because each is invertible by [F1]; since , the intermediate value property [L1] gives for every . Hence is orientation-preserving at every , and in particular preserves the orientation of at every point.
Since is a diffeomorphism and , [L2] shows that maps the interior of onto the interior and the sphere onto itself; thus is a diffeomorphism. Moreover carries the outward transverse direction of at each to the outward transverse direction at : 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.
The restriction preserves the outward-normal-first boundary orientation of [L3]: if is a positive basis of , so that is a positive basis of with outward, then step 1.1 makes positive at , and is an outward vector by step 2.1, so is a positive basis of . Hence is an orientation-preserving diffeomorphism of , and [L4] gives .
Let be a linear reflection, , preserving . By [L4] the restriction reverses the boundary orientation and has degree , while every diffeomorphism arising as above has degree by step 3.1; therefore is impossible, and no such ambient isotopy can restrict to the reflection.
Depends on
- $C^k$ maps and multi-index derivative notation in Euclidean space
- Smooth isotopies, diffeotopies and ambient isotopies
- Induced boundary orientation
- Diffeomorphisms preserve interior and boundary
- Degree of an orientation-preserving or reversing diffeomorphism
- Diffeomorphisms and local diffeomorphisms of manifolds
- Orientable manifolds
- Intermediate value theorem, by bisection with a canonical left-half rule: a continuous function on $[a,b]$ takes every value between $f(a)$ and $f(b)$
- For every fixed finite size at least one, the determinant of a real square matrix is a polynomial in its matrix entries
- Higher derivatives and the classes $C^k$ and $C^\infty$
- Directional derivatives and partial derivatives of a map $U\subseteq\mathbb{R}^m\to\mathbb{R}^n$
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Sources
- Morris W. Hirsch, Differential Topology (Graduate Texts in Mathematics 33, Springer 1976; full text retrieved from the Internet Archive Wayback Machine snapshot of the luis.impa.br course copy), Chapter 8 “Isotopy”, §1, printed pp. 177–183 (Theorems 1.1–1.8 and Exercises 3, 7, 9, 10, 11, 16, printed pp. 182–184) (standard reference, not scraped)
- C. T. C. Wall, Differential Topology (Cambridge Studies in Advanced Mathematics 156, Cambridge University Press 2016; full text retrieved from the Internet Archive Wayback Machine snapshot of the ETH Zürich course copy), Chapter 6 §§6.2–6.4, printed pp. 169–192 (Theorem 6.2.1; Propositions 6.3.1 and 6.3.3; Theorems 6.3.2, 6.3.4, 6.3.6, 6.4.5, 6.4.8 and 6.4.9; Lemma 6.3.5) (standard reference, not scraped)