Stratifold
In differential topology, a branch of mathematics, a stratifold is a generalization of a differentiable manifold where certain kinds of singularities are allowed. More specifically a stratifold is stratified into differentiable manifolds of different dimensions. Stratifolds can be used to construct new homology theories. For example, they provide a new geometric model for ordinary homology. The concept of stratifolds was invented by Matthias Kreck. The basic idea is similar to that of a topologically stratified space, but adapted to differential topology.
Definitions
Before we come to stratifolds, we define a preliminary notion, which captures the minimal notion for a smooth structure on a space: A differential space is a pair where X is a topological space and C is a subalgebra of the continuous functions such that a function is in C if it is locally in C and is in C for smooth and A simple example takes for X a smooth manifold and for C just the smooth functions.For a general differential space and a point x in X we can define as in the case of manifolds a tangent space as the vector space of all derivations of function germs at x. Define strata has dimension i For an n-dimensional manifold M we have that and all other strata are empty. We are now ready for the definition of a stratifold, where more than one stratum may be non-empty:
A k-dimensional stratifold is a differential space where S is a locally compact Hausdorff space with countable base of topology. All skeleta should be closed. In addition we assume:
[Image:suspension.svg|thumb|upright|right|The suspension]
- The are i-dimensional smooth manifolds.
- For all x in S, restriction defines an isomorphism of stalks
- All tangent spaces have dimension ≤ k.
- For each x in S and every neighbourhood U of x, there exists a function with and .
An important subclass of stratifolds are the regular stratifolds, which can be roughly characterized as looking locally around a point in the i-stratum like the i-stratum times a -dimensional stratifold. This is a condition which is fulfilled in most stratifold one usually encounters.
Examples
There are plenty of examples of stratifolds. The first example to consider is the open cone over a manifold M. We define a continuous function from S to the reals to be in C if and only if it is smooth on and it is locally constant around the cone point. The last condition is automatic by point 2 in the definition of a stratifold. We can substitute M by a stratifold S in this construction. The cone is oriented if and only if S is oriented and not zero-dimensional. If we consider the cone with bottom, we get a stratifold with boundary S.Other examples for stratifolds are one-point compactifications and suspensions of manifolds, algebraic varieties with only isolated singularities and simplicial complexes.
Bordism theories
[Image:Pair of pants cobordism (pantslike).svg|thumb|right| An example of a bordism relation]In this section, we will assume all stratifolds to be regular. We call two maps from two oriented compact k-dimensional stratifolds into a space X ''bordant if there exists an oriented -dimensional compact stratifold T'' with boundary S + such that the map to X extends to T. The set of equivalence classes of such maps is denoted by The sets have actually the structure of abelian groups with disjoint union as addition. One can develop enough differential topology of stratifolds to show that these define a homology theory. Clearly, for since every oriented stratifold S is the boundary of its cone, which is oriented if One can show that Hence, by the Eilenberg-Steenrod uniqueness theorem, for every space X homotopy-equivalent to a CW-complex, where H denotes singular homology. For other spaces these two homology theories need not be isomorphic.
There is also a simple way to define equivariant homology with the help of stratifolds. Let G be a compact Lie group. We can then define a bordism theory of stratifolds mapping into a space X with a G-action just as above, only that we require all stratifolds to be equipped with an orientation-preserving free G-action and all maps to be G-equivariant. Denote by the bordism classes. One can prove for every X homotopy equivalent to a CW-complex.