English
Noun
- A continuous
deformation of one
continuous function to
another
- A theory associating
a system of groups to each
topological
space
- A system of groups associated to a topological space
In
topology, two
continuous functions
from one
topological
space to another are called homotopic (
Greek
homos = identical and topos = place) if one can be "continuously
deformed" into the other, such a deformation being called a
homotopy between the two functions. An outstanding use of homotopy
is the definition of
homotopy
groups and
cohomotopy
groups, important
invariants
in
algebraic
topology.
In practice, there are technical difficulties in
using homotopies with certain pathological spaces. Consequently
most algebraic topologists work with
compactly
generated spaces,
CW complexes,
or
spectra.
Formal definition
Formally, a homotopy between two
continuous functions f and g from a topological space X to a
topological space Y is defined to be a continuous function H: X
× [0,1] → Y from the
product
of the space X with the
unit
interval [0,1] to Y such that, for all points x in X,
H(x,0)=f(x) and H(x,1)=g(x).
If we think of the second
parameter of H as "time", then
H describes a "continuous deformation" of f into g: at time 0 we
have the function f, at time 1 we have the function g.
Properties
Continuous functions f and g (both from
topological space X to Y) are said to be homotopic iff there is a
homotopy H taking f to g as described above. Being homotopic is an
equivalence
relation on the set of all continuous functions from X to Y.
This homotopy relation is compatible with
function
composition in the following sense: if f1, g1: X → Y
are homotopic, and f2, g2: Y → Z are homotopic, then their
compositions f2 o f1 and g2 o g1: X → Z are homotopic as
well.
Homotopy equivalence and null-homotopy
Given two spaces X
and Y, we say they are homotopy equivalent or of the same homotopy
type if there exist continuous
maps f:
X → Y and g: Y → X such that g o f is homotopic
to the
identity
map idX and f o g is homotopic to idY.
The maps f and g are called homotopy equivalences
in this case. Clearly, every
homeomorphism is a
homotopy equivalence, but the converse is not true: for example, a
solid disk is not homeomorphic to a single point, although the disk
and the point are homotopy equivalent.
Intuitively, two spaces X and Y are homotopy
equivalent if they can be transformed into one another by bending,
shrinking and expanding operations. For example, a solid disk or
solid ball is homotopy equivalent to a point, and R2 - is homotopy
equivalent to the
unit circle
S1. Those spaces that are homotopy equivalent to a point are called
contractible.
A function f is said to be null-homotopic if it
is
homotopic to a
constant function. (The homotopy from f to a constant function is
then sometimes called a null-homotopy.) For example, it is simple
to show that a map from the
circle S1 is null-homotopic
precisely when it can be extended to a map of the disc D2.
It follows from these definitions that a space X
is contractible if and only if the identity map from X to
itself—which is always a homotopy
equivalence—is null-homotopic.
Homotopy invariance
Homotopy equivalence is important
because in
algebraic
topology many concepts are homotopy invariant, that is, they
respect the relation of homotopy equivalence. For example, if X and
Y are homotopy equivalent spaces, then:
An example of an algebraic invariant of
topological spaces which is not homotopy-invariant is
compactly supported homology (which is, roughly speaking, the
homology of the
compactification, and compactification is not
homotopy-invariant).
Homotopy category
The idea of homotopy can be turned into a
formal category of
category
theory. The homotopy category is the category whose objects are
topological spaces, and whose morphisms are homotopy equivalence
classes of continuous maps. Two topological spaces X and Y are
isomorphic in this category if and only if they are
homotopy-equivalent. Then a
functor on the category of
topological spaces is homotopy invariant if it can be expressed as
a functor on the homotopy category.
For example, homology groups are a functorial
homotopy invariant: this means that if f and g from X to Y are
homotopic, then the
group
homomorphisms induced by f and g on the level of
homology
groups are the same: Hn(f) = Hn(g) : Hn(X) → Hn(Y) for
all n. Likewise, if X and Y are in addition
path-connected, then the
group homomorphisms induced by f and g on the level of
homotopy
groups are also the same: πn(f) = πn(g) :
πn(X) → πn(Y).
Relative homotopy
In order to define the
fundamental
group, one needs the notion of homotopy relative to a subspace.
These are homotopies which keep the elements of the subspace fixed.
Formally: if f and g are continuous maps from X to Y and K is a
subset of X, then we say
that f and g are homotopic relative to K if there exists a homotopy
H: X × [0,1] → Y between f and g such that
H(k,t) = f(k) = g(k) for all k∈K and t∈[0,1].
Also, if g is a
retract
from X to K and f is the identity map, this is known as a strong
deformation
retract of X to K.
Timelike homotopy
On a
Lorentzian
manifold, certain curves are distinguished as
timelike. A
timelike
homotopy between two timelike curves is a homotopy such that
each intermediate curve is timelike. No
closed
timelike curve (CTC) on a Lorentzian manifold is timelike
homotopic to a point (that is, null timelike homotopic); such a
manifold is therefore said to be
multiply
connected by timelike curves. A manifold such as the
3-sphere can be
simply
connected (by any type of curve), and yet be multiply timelike
connected.
Homotopy extension property
Another useful property
involving homotopy is the
homotopy extension property, which characterizes the extension
of a homotopy between two functions from a subset of some set to
the set itself. It is useful when dealing with
cofibrations.
Isotopy
In case the two given continuous functions f and g
from the topological space X to the topological space Y are
homeomorphisms,
one can ask whether they can be connected 'through homeomorphisms'.
This gives rise to the concept of isotopy, which is a homotopy, H,
in the notation used before, such that for each fixed t, H(x,t)
gives a homeomorphism.
Requiring that two homeomorphisms be isotopic
really is a stronger requirement than that they be homotopic. For
example, the map of the
unit disc in R2
defined by f(x,y) = (−x, −y) is
equivalent to a 180-degree
rotation around the origin, and
so the identity map and f are isotopic because they can be
connected by rotations. However, the map on the interval
[−1,1] in R defined by f(x) = −x is not
isotopic to the identity. Loosely speaking, any homotopy from f to
the identity would have to exchange the endpoints, which would mean
that they would have to 'pass through' each other. Moreover, f has
changed the orientation of the interval, hence it cannot be
isotopic to the identity.
In
geometric
topology—for example in
knot
theory—the idea of isotopy is used to construct
equivalence relations. For example, when should two knots be
considered the same? We take two knots, K1 and K2, in
three-
dimensional
space. The intuitive idea of deforming one to the other should
correspond to a path of homeomorphisms: an isotopy starting with
the identity homeomorphism of three-dimensional space, and ending
at a homeomorphism, h, such that h moves K1 to K2. An
ambient
isotopy, studied in this context, is an isotopy of the larger
space, considered in light of its action on the embedded
submanifold.
homotopy in German: Homotopie
homotopy in Spanish: Homotopía
homotopy in French: Homotopie
homotopy in Hebrew: הומוטופיה
homotopy in Italian: Omotopia
homotopy in Dutch: Homotopie-equivalentie
homotopy in Japanese: ホモトピー
homotopy in Polish: Homotopia
homotopy in Portuguese: Homotopia
homotopy in Russian: Гомотопия
homotopy in Serbian: Хомотопија
homotopy in Finnish: Homotopia
homotopy in Vietnamese: Đồng
luân