Isotopy

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Classification of embeddings up to isotopy is a classical problem in topology, see [Skopenkov2016c, \S1].

1 Definition of ambient isotopy

For manifolds M,N two embeddings f,g:N\to M are called ambiently isotopic, if there exists a homeomorphism onto F:\Rr^m\times I\to\Rr^m\times I such that

  • F(y,0)=(y,0) for each y\in\Rr^m,
  • F(f(x),1)=(g(x),1) for each x\in N, and
  • F(\Rr^m\times\{t\})=\Rr^m\times\{t\} for each t\in I.

See [Skopenkov2006, Figure 1.1]. An ambient isotopy is the above homeomorphism F, or, equivalently, a family of homeomorphisms F_t:\Rr^m\to\Rr^m generated by the map F in the obvious manner. The latter family can be seen as a homotopy \Rr^m\times I\to\Rr^m.

Evidently, isotopy is an equivalence relation on the set of embeddings of N into \Rr^m.

This notion of isotopy is also called ambient isotopy in contrast to the non-ambient isotopy defined just below.

2 Other equivalence relations

Ambient isotopy is a stronger equivalence relation than non-ambient isotopy, isoposition, concordance, bordism, etc.

Two embeddings f,g:N\to\Rr^m are called non-ambient isotopic, if there exists an embedding F:N\times I\to\Rr^m\times I such that

  • F(x,0)=(f(x),0),
  • F(x,1)=(g(x),1) for each x\in N and
  • F(N\times\{t\})\subset\Rr^m\times\{t\} for each t\in I.

In the DIFF category or for m-n\ge3 in the PL or TOP category non-ambient isotopy implies ambient isotopy [Hirsch1976], [Hudson&Zeeman1964], [Hudson1966], [Akin1969], [Edwards1975]. For m-n\le2 this is not so: e.g., any knot S^1\to\Rr^3 is non-ambiently PL isotopic to the trivial one, but not necessarily ambiently PL isotopic to it.

Two embeddings f,g:N\to\Rr^m are said to be (orientation preserving) isopositioned, if there is an (orientation preserving) homeomorphism h:\Rr^m\to\Rr^m such that h\circ f=g.

For embeddings into \Rr^m PL orientation preserving isoposition is equivalent to PL ambient isotopy (the Alexander-Guggenheim Theorem) [Rourke&Sanderson1972, 3.22].

Two embeddings f,g:N\to\Rr^m are said to be (ambiently) concordant if there is a homeomorphism (onto) F:\Rr^m\times I\to\Rr^m\times I (which is called a concordance) such that

  • F(y,0)=(y,0) for each y\in\Rr^m and
  • F(f(x),1)=(g(x),1) for each x\in N.

The definition of non-ambient concordance is analogously obtained from that of non-ambient isotopy by dropping the last condition of level-preservation.

In the DIFF category or for m-n\ge3 in the PL or TOP category non-ambient concordance implies ambient concordance and ambient isotopy [Lickorish1965], [Hudson1970], [Hudson&Lickorish1971]. (This is not so in the PL or TOP category for codimension 2.) This result allows a reduction of the Knotting Problem to the relativized Embedding Problem, see [SkopenkovC, \S1].

3 References

]{Skopenkov2016c}. == Definition of ambient isotopy == ; For manifolds $M,N$ two [[Embedding|embeddings]] $f,g:N\to M$ are called [[Wikipedia:Ambient_isotopy|ambiently isotopic]], if there exists a homeomorphism onto $F:\Rr^m\times I\to\Rr^m\times I$ such that * $F(y,0)=(y,0)$ for each $y\in\Rr^m,$ * $F(f(x),1)=(g(x),1)$ for each $x\in N,$ and * $F(\Rr^m\times\{t\})=\Rr^m\times\{t\}$ for each $t\in I.$ See \cite[Figure 1.1]{Skopenkov2006}. An ''ambient isotopy'' is the above homeomorphism $F$, or, equivalently, a family of homeomorphisms $F_t:\Rr^m\to\Rr^m$ generated by the map $F$ in the obvious manner. The latter family can be seen as a homotopy $\Rr^m\times I\to\Rr^m$. Evidently, isotopy is an equivalence relation on the set of embeddings of $N$ into $\Rr^m$. This notion of isotopy is also called ''ambient'' isotopy in contrast to the ''non-ambient'' isotopy defined just below. == Other equivalence relations == ; Ambient isotopy is a stronger equivalence relation than non-ambient isotopy, isoposition, concordance, bordism, etc. Two embeddings $f,g:N\to\Rr^m$ are called ''non-ambient'' isotopic, if there exists an embedding $F:N\times I\to\Rr^m\times I$ such that * $F(x,0)=(f(x),0)$, * $F(x,1)=(g(x),1)$ for each $x\in N$ and * $F(N\times\{t\})\subset\Rr^m\times\{t\}$ for each $t\in I$. In the DIFF category or for $m-n\ge3$ in the PL or TOP category non-ambient isotopy implies ambient isotopy \cite{Hirsch1976}, \cite{Hudson&Zeeman1964}, \cite{Hudson1966}, \cite{Akin1969}, \cite{Edwards1975}. For $m-n\le2$ this is not so: e.g., any knot $S^1\to\Rr^3$ is non-ambiently PL isotopic to the trivial one, but not necessarily ambiently PL isotopic to it. Two embeddings $f,g:N\to\Rr^m$ are said to be (orientation preserving) ''isopositioned'', if there is an (orientation preserving) homeomorphism $h:\Rr^m\to\Rr^m$ such that $h\circ f=g$. For embeddings into $\Rr^m$ PL orientation preserving isoposition is equivalent to PL ambient isotopy (the Alexander-Guggenheim Theorem) \cite[3.22]{Rourke&Sanderson1972}. Two embeddings $f,g:N\to\Rr^m$ are said to be ''(ambiently) concordant'' if there is a homeomorphism (onto) $F:\Rr^m\times I\to\Rr^m\times I$ (which is called a ''concordance'') such that * $F(y,0)=(y,0)$ for each $y\in\Rr^m$ and * $F(f(x),1)=(g(x),1)$ for each $x\in N$. The definition of ''non-ambient concordance'' is analogously obtained from that of non-ambient isotopy by dropping the last condition of level-preservation. In the DIFF category or for $m-n\ge3$ in the PL or TOP category non-ambient concordance implies ambient concordance and ambient isotopy \cite{Lickorish1965}, \cite{Hudson1970}, \cite{Hudson&Lickorish1971}. (This is not so in the PL or TOP category for codimension 2.) This result allows a reduction of the [[High codimension embeddings: classification#Introduction|Knotting Problem]] to the relativized [[High codimension embeddings: classification#Introduction|Embedding Problem]], see \cite[$\S\S1].

1 Definition of ambient isotopy

For manifolds M,N two embeddings f,g:N\to M are called ambiently isotopic, if there exists a homeomorphism onto F:\Rr^m\times I\to\Rr^m\times I such that

  • F(y,0)=(y,0) for each y\in\Rr^m,
  • F(f(x),1)=(g(x),1) for each x\in N, and
  • F(\Rr^m\times\{t\})=\Rr^m\times\{t\} for each t\in I.

See [Skopenkov2006, Figure 1.1]. An ambient isotopy is the above homeomorphism F, or, equivalently, a family of homeomorphisms F_t:\Rr^m\to\Rr^m generated by the map F in the obvious manner. The latter family can be seen as a homotopy \Rr^m\times I\to\Rr^m.

Evidently, isotopy is an equivalence relation on the set of embeddings of N into \Rr^m.

This notion of isotopy is also called ambient isotopy in contrast to the non-ambient isotopy defined just below.

2 Other equivalence relations

Ambient isotopy is a stronger equivalence relation than non-ambient isotopy, isoposition, concordance, bordism, etc.

Two embeddings f,g:N\to\Rr^m are called non-ambient isotopic, if there exists an embedding F:N\times I\to\Rr^m\times I such that

  • F(x,0)=(f(x),0),
  • F(x,1)=(g(x),1) for each x\in N and
  • F(N\times\{t\})\subset\Rr^m\times\{t\} for each t\in I.

In the DIFF category or for m-n\ge3 in the PL or TOP category non-ambient isotopy implies ambient isotopy [Hirsch1976], [Hudson&Zeeman1964], [Hudson1966], [Akin1969], [Edwards1975]. For m-n\le2 this is not so: e.g., any knot S^1\to\Rr^3 is non-ambiently PL isotopic to the trivial one, but not necessarily ambiently PL isotopic to it.

Two embeddings f,g:N\to\Rr^m are said to be (orientation preserving) isopositioned, if there is an (orientation preserving) homeomorphism h:\Rr^m\to\Rr^m such that h\circ f=g.

For embeddings into \Rr^m PL orientation preserving isoposition is equivalent to PL ambient isotopy (the Alexander-Guggenheim Theorem) [Rourke&Sanderson1972, 3.22].

Two embeddings f,g:N\to\Rr^m are said to be (ambiently) concordant if there is a homeomorphism (onto) F:\Rr^m\times I\to\Rr^m\times I (which is called a concordance) such that

  • F(y,0)=(y,0) for each y\in\Rr^m and
  • F(f(x),1)=(g(x),1) for each x\in N.

The definition of non-ambient concordance is analogously obtained from that of non-ambient isotopy by dropping the last condition of level-preservation.

In the DIFF category or for m-n\ge3 in the PL or TOP category non-ambient concordance implies ambient concordance and ambient isotopy [Lickorish1965], [Hudson1970], [Hudson&Lickorish1971]. (This is not so in the PL or TOP category for codimension 2.) This result allows a reduction of the Knotting Problem to the relativized Embedding Problem, see [SkopenkovC, \S1].

3 References

]{SkopenkovC}.
== References == {{#RefList:}} [[Category:Definitions]] [[Category:Embeddings of manifolds]]\S1].

1 Definition of ambient isotopy

For manifolds M,N two embeddings f,g:N\to M are called ambiently isotopic, if there exists a homeomorphism onto F:\Rr^m\times I\to\Rr^m\times I such that

  • F(y,0)=(y,0) for each y\in\Rr^m,
  • F(f(x),1)=(g(x),1) for each x\in N, and
  • F(\Rr^m\times\{t\})=\Rr^m\times\{t\} for each t\in I.

See [Skopenkov2006, Figure 1.1]. An ambient isotopy is the above homeomorphism F, or, equivalently, a family of homeomorphisms F_t:\Rr^m\to\Rr^m generated by the map F in the obvious manner. The latter family can be seen as a homotopy \Rr^m\times I\to\Rr^m.

Evidently, isotopy is an equivalence relation on the set of embeddings of N into \Rr^m.

This notion of isotopy is also called ambient isotopy in contrast to the non-ambient isotopy defined just below.

2 Other equivalence relations

Ambient isotopy is a stronger equivalence relation than non-ambient isotopy, isoposition, concordance, bordism, etc.

Two embeddings f,g:N\to\Rr^m are called non-ambient isotopic, if there exists an embedding F:N\times I\to\Rr^m\times I such that

  • F(x,0)=(f(x),0),
  • F(x,1)=(g(x),1) for each x\in N and
  • F(N\times\{t\})\subset\Rr^m\times\{t\} for each t\in I.

In the DIFF category or for m-n\ge3 in the PL or TOP category non-ambient isotopy implies ambient isotopy [Hirsch1976], [Hudson&Zeeman1964], [Hudson1966], [Akin1969], [Edwards1975]. For m-n\le2 this is not so: e.g., any knot S^1\to\Rr^3 is non-ambiently PL isotopic to the trivial one, but not necessarily ambiently PL isotopic to it.

Two embeddings f,g:N\to\Rr^m are said to be (orientation preserving) isopositioned, if there is an (orientation preserving) homeomorphism h:\Rr^m\to\Rr^m such that h\circ f=g.

For embeddings into \Rr^m PL orientation preserving isoposition is equivalent to PL ambient isotopy (the Alexander-Guggenheim Theorem) [Rourke&Sanderson1972, 3.22].

Two embeddings f,g:N\to\Rr^m are said to be (ambiently) concordant if there is a homeomorphism (onto) F:\Rr^m\times I\to\Rr^m\times I (which is called a concordance) such that

  • F(y,0)=(y,0) for each y\in\Rr^m and
  • F(f(x),1)=(g(x),1) for each x\in N.

The definition of non-ambient concordance is analogously obtained from that of non-ambient isotopy by dropping the last condition of level-preservation.

In the DIFF category or for m-n\ge3 in the PL or TOP category non-ambient concordance implies ambient concordance and ambient isotopy [Lickorish1965], [Hudson1970], [Hudson&Lickorish1971]. (This is not so in the PL or TOP category for codimension 2.) This result allows a reduction of the Knotting Problem to the relativized Embedding Problem, see [SkopenkovC, \S1].

3 References

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