3.1 Complex structure
Let , and , and denote , .
We regard as a toric Fano manifold , with moment polytope corresponding to the anticanonical class . More explicitly is the -simplex inside spanned by the vertices
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in particular is a reflexive integral Delzant polytope, with dual polytope
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being the -simplex spanned by the vertices .
The integral points
parametrize monomials in the anticanonical linear system . We study the family of hypersurfaces
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(8) |
Here are a fixed collection of coefficients, with corresponding to the unique interior integral point . For any vertex of , we require . The function is defined for those for which ; by assumption , and otherwise. The natural piecewise linear extension of to is assumed to be concave, whose domains of linearity are by assumption simplices, producing a triangulation of . Using the adjunction formula, we can write down a holomorphic volume form on , such that along
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(9) |
with the standard coordinates on .
We will always assume , and all the constants in the estimates are independent of .
Example 3.1.
The Fermat family is given explicitly as
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(10) |
namely we choose for corresponding to the monomials and , and choose to be the piecewise linear function with value at the origin and at the vertices of .
The key notion to describe the complex structure degeneration is a piecewise linear object called the tropicalisation of the hypersurfaces. Define the nonnegative piecewise linear function on by
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The tropicalisation is defined as the nonsmooth locus of , or equivalently the locus inside where the maximum is achieved by at least two values of . There is precisely one bounded component in the complement of ,
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whose boundary . The relation between the hypersurfaces and the tropicalisation is furnished by the rescaled log map,
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The image is called the amoeba. The following Prop. will be tacitly used frequently, as it allows us to think of regions on efficiently in terms of the regions on , up to a tiny amount of fuzziness.
Proposition 3.2.
(cf. [23, Prop. 3.2]) The amoebas converge in the Hausdorff distance to in the Hausdorff distance as . In fact
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Proof.
(sketch) Let and let saturate the maximum for . Applying to the inequality
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we see
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so . The other inequality of the claim can be proved by constructing local models of in regions whose -images are close to , and then use the implicit function theorem to show is a small perturbation of these local models.
∎
Example 3.3.
In the Fermat family example above is the reflexion of .
The tropicalisation is naturally stratified according to the subset of saturating the maximum . This induces a kind of quantitative stratification structure on for .
Lemma 3.4.
There is a fixed number , such that for and any (or ), there is a simplex in the triangulation of , verifying for .
Proof.
(Sketch) For any fixed , the function is a concave function of . By our assumptions, the set of saturating the maximum must be the set of vertices of some simplex in the triangulation of . A more effective version of this observation is the Lemma in the case, and the case follows by Prop. 3.2.
∎
Given a simplex in the triangulation, we associate a subset :
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Clearly if , then . The intuition is that larger correspond to more nongeneric regions, and the complement of their neighbourhoods correspond to more generic regions.
Notation.
We need a few terminologies to describe . The face of dual to is . The outward normal cone to is
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By the Delzant polytope property is isomorphic to , where is the dimension of the minimal face of containing .
The Minkowski sum of two sets means .
Lemma 3.5.
(compare [23, Lemma 3.1]) If then
Lemma 3.6.
.
Proof.
Let .
If achieves the maximum , then . If not, then the
maximum is achieved by at least two , so for some with .
∎
Remark 3.7.
The intuition is that a neighbourhood of corresponds to a toric region, while controls how approaches the toric boundary of , and the stratification is related to how the toric boundary components intersect.
Our next goal is to assign good holomorphic charts to related to the stratification structure. We first consider the toric region, which shall be covered by -charts. Let be the primitive integral outward normal vector to a facet of . The chart parametrised by is contained inside the region
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(11) |
Let , and choose an integral basis for . Then the monomials provide the local -coordinates on the chart, since by the implicit function theorem is locally a graph . In fact by the defining equation (8) of the hypersurface
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whence the holomorphic volume form is (cf. (9))
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(12) |
(Here are suitably oriented to take care of .) We regard the above region as an open subset of , and denote the chart as the largest -invariant subset, delineated by a collection of affine linear inequalities on the variables .
In the tropical limit , the region becomes
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Inside this the limiting version of is
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Later we shall also need the slightly shrinked regions for : let
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whose largest -invariant subset is
. The tropical limit of is
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containing the limiting version of
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As the choice of varies, such regions cover a neighbourhood of as a consequence of Lemma 3.4; so do . This means the charts of toric type already cover part of the neighbourhood of the toric boundary.
Example 3.8.
In the case, are elliptic curves, and the toric charts cover the entire . In the case, are quartic K3 surfaces, and the toric charts cover most parts of including a large portion of the intersection of with the toric boundary of , but do not cover a tiny neighbourhood of the 24 points located at the intersection of with .
We now consider the neighbourhood of the toric boundary near the stratum , but keeping away from higher strata and from .
Here
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Since
most terms in the defining equation (8) are negligible in our region, the hypersurface is locally approximately
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We focus on the subregion where achieves the maximal magnitude for , and achieves the second largest magnitude. These two magnitudes must be of comparable size by the hypersurface equation. Choose an integral basis for the outward normal cone ,
so for . Denote the vertices of as for , and choose an integral basis of . Choose so that is an integral basis of , and complete this into an integral basis for , providing -variables . We then find for , with , and we can demand because . These provide the -variables for , which can vanish on the toric boundary. On this local piece of ,
the variables and furnish a set of local coordinates as the -variable is expressible locally as a function of theirs.
The holomorphic volume form (9) is
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(13) |
up to choosing appropriate ordering of the coordinates. Here is the divisibility of inside the group
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Notice is uniformly equivalent to in this region.
Remark 3.9.
The discussion above can be simplified if one assumes the triangulation of is maximal, namely each simplex is -isomorphic to the standard simplex. We choose not to do so because this stronger assumption would exclude the Fermat family.
Remark 3.10.
A problem when we work with the coordinates is the inequality constraint to keep and as the two dominant monomials. This means such a holomorphic chart is not quite as simple as the product of with a long annulus in . In practice we will cover this region by lots of simpler charts which we call the charts of boundary type. Let be any point in this region, such that is large but still comparable to 1 (to guarantee the chart overlaps nontrivially with some toric type chart). The associated chart uses the same coordinates as above, but describes only a small region:
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where is a fixed dimensional constant. These charts have an interpretation in terms of the strata (cf. Lemma 3.5): the point corresponds roughly to a point on the face , and allowing to decrease to zero corresponds to taking the Minkowski sum with the outward normal cone , so the tropical analogue of our small chart is .
Example 3.11.
For generic quartic K3 surfaces, the following simple situation models a small neighbourhood of the 24 points on . Locally the dominant monomials are , where are -coodinates which vanish on toric boundaries, and is a -coordinate; together are local coordinates on . The local model hypersurface is
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so can be used as local coordinates on the hypersurface.
The holomorphic volume form on the hypersurface is (up to a normalising factor)
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This is the typical boundary type behaviour. A significant part of the boundary type region overlaps with the toric region. In this example, when is not too small, we can view as a -coordinates, so provides a toric type chart, as we can express . In this chart
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which agrees with the standard holomorphic volume form in toric type charts. The same behaviour happens when is not too small. The problem mentioned in Remark 3.10 is due to the fact that this local model is only a valid approximate description of the K3 for satisfying some inequality constraints. The prescription of charts of boundary type means that we are simultaneously using the charts for many choices of parameters . Notice the scaling symmetry
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means that there is no obviously preferred chart of boundary type. More concrete examples can be found in [30, section 1.1.6].
Local charts of the toric type and the boundary type cover the entire hypersurface for , and a substantial portion of any boundary type chart is in fact already covered by toric charts. Almost all the measure is contained in the toric type region.