Last time we defined crystalline cohomology by defining the crystalline site. Our setup was to fix a PD-scheme and look at an
-scheme
to which
extends. Remember that the objects of the site
were triples
that we short-handed with
. Today we’ll start by re-examining these objects. We can give a little better description which will help us figure out what a sheaf on this site is. Recall that the full subcategory of the category
of presheaves (of sets) on the site is a topos which we’ll denote
.
Suppose is an object of
, i.e. a sheaf. This just means it is a functor
that also satisfies for any covering
the following sequence being exact
.
Let’s fix some object and some sheaf
. If
is a Zariski open set then define
and
. There is an inclusion
, which by construction is a map in the category
, so by virtue of being a contravariant functor we get
. The contravariant functor
is a sheaf on the Zariski site of
which we denote
.
We have a proposition that the data of a sheaf on
is equivalent to the data that for ever
-PD thickening
we assign a Zariski sheaf on
denoted conspicuously by
and for every morphism
we assign a map
satisfying two compatibility conditions.
1) If is another map then we have a commutative diagram
and
2) If is an open immersion, the map
is an isomorphism.
Using this new characterization it is much easier to describe what the structure sheaf in this site should be, since to give a sheaf I need to give on every thickening
a Zariski sheaf and we have a natural Zariski structure sheaf
. This assignment can be seen to satisfy the conditions and hence we have a crystalline sheaf. Note that this was not the only choice that works, though. We’ve already pointed out that
, so we could also assign
which is another crystalline sheaf that we’ll denote
.
For our last example, let’s just create a new sheaf from our two above by taking . This is actually a sheaf of P.D. ideals in
and we’ll call it
. By construction it sits in an exact sequence
.
The last thing to point out for today is that this alternate way of thinking about crystalline sheaves is that it really gives us a way of thinking in Zariski terms which we’re already familiar with. In particular, if is a map of crystalline sheaves we can check whether it is an isomorphism (or surjective or injective) on stalks by checking for each
and each
-P.D. thickening
of a neighborhood if the map
is an isomorphism.