Deformations of corank $1$ frontals
C. Mu\~noz-Cabello, J.J. Nu\~no-Ballesteros, R. Oset Sinha

TL;DR
This paper develops a new theoretical framework for understanding deformations of corank 1 frontals, including stability, versality, and classification, without relying on contact geometry, and proves a version of Mond's conjecture.
Contribution
It introduces a frontal Thom-Mather theory, characterizes stability and versality, and classifies stable corank 1 frontals in complex dimensions.
Findings
Proves a frontal version of Mond's conjecture in dimension 1.
Provides a complete classification of stable corank 1 frontals from a0a0 to a0a0.
Develops methods for constructing stable and versal frontal unfoldings.
Abstract
We develop a Thom-Mather theory of frontals analogous to Ishikawa's theory of deformations of Legendrian singularities but at the frontal level, avoiding the use of the contact setting. In particular, we define concepts like frontal stability, versality of frontal unfoldings or frontal codimension. We prove several characterizations of stability, including a frontal Mather-Gaffney criterion, and of versality. We then define the method of reduction with which we show how to construct frontal versal unfoldings of plane curves and show how to construct stable unfoldings of corank 1 frontals with isolated instability which are not necessarily versal. We prove a frontal version of Mond's conjecture in dimension 1. Finally, we classify stable frontal multigerms and give a complete classification of corank 1 stable frontals from to .
| Plane curve | Versal frontal unfolding | |
|---|---|---|
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Taxonomy
TopicsGeometric Analysis and Curvature Flows · Topological and Geometric Data Analysis · Geometric and Algebraic Topology
Deformations of corank frontals
C. Muñoz-Cabello, J.J. Nuño-Ballesteros, R. Oset Sinha
Departament de Matemàtiques, Universitat de València, Campus de Burjassot, 46100 Burjassot, Spain
Departament de Matemàtiques, Universitat de València, Campus de Burjassot, 46100 Burjassot, SPAIN. Departamento de Matemática, Universidade Federal da Paraíba CEP 58051-900, João Pessoa - PB, BRAZIL
Abstract.
We develop a Thom-Mather theory of frontals analogous to Ishikawa’s theory of deformations of Legendrian singularities but at the frontal level, avoiding the use of the contact setting. In particular, we define concepts like frontal stability, versality of frontal unfoldings or frontal codimension. We prove several characterizations of stability, including a frontal Mather-Gaffney criterion, and of versality. We then define the method of reduction with which we show how to construct frontal versal unfoldings of plane curves and show how to construct stable unfoldings of corank 1 frontals with isolated instability which are not necessarily versal. We prove a frontal version of Mond’s conjecture in dimension 1. Finally, we classify stable frontal multigerms and give a complete classification of corank 1 stable frontals from to .
Work of Juan J. Nuño-Ballesteros and R. Oset Sinha partially supported by Grant PID2021-124577NB-I00 funded by MCIN/AEI/ 10.13039/501100011033 and by “ERDF A way of making Europe”
1. Introduction
The study of frontal mappings has flourished rapidly in the last decade. Roughly speaking a frontal is a mapping where and are and -dimensional manifolds such that the image of has a well defined tangent hyperplane at each point. More precisely, is a frontal if it admits a Legendrian lift such that , where is the canonical fibration. When the Legendrian lift is an immersion we say that is a wave front. The concept of frontals was first introduced by Fujimori, Saji, Umehara and Yamada in [7] (see also [29]) and since then it has been of great interest to differential geometers, singularists and contact topologists. The fact of having a well defined normal at each point allows one to study differential geometric properties and invariants in singular spaces ([4, 16, 21, 24, 25]), on the other hand, when studying contact and symplectic topology front singularities are unavoidable [3] and understanding the generic (or stable) situations is crucial.
In [14], Ishikawa developed the analogue of the Thom-Mather theory for corank one Legendrian singularities and he stated the main notions like infinitesimal deformations, stability, versality, etc. Our purpose in this paper is to construct a Thom-Mather theory of singularities of frontals, but downstairs, at the level of frontals, and thus, avoiding the use of the contact setting. In particular, we consider deformations that come from unfoldings of the frontal . We show that such unfoldings come from a deformation of its Legendrian lift if and only if is frontal as a mapping. Taking local charts of and we study map germs under -equivalence, i.e. smooth changes of coordinates in source and target. Here, smooth means when or holomorphic when . The case of frontal surfaces () was studied in a previous paper ([22]) where analytic/toplogical invariants were defined and characteristations of finite frontal codimension were given, amongst other interesting results on surfaces, using some of the definitions and results that will be given in this paper.
In Section 3 we define the concept of frontal stability and versality. We define a frontal codimension and prove that a frontal is stable if and only if it has frontal codimension 0. We also give a characterisation of versality analogous to Mather’s versality theorem. Section 4 gives a geometric criterion for stability, a frontal Mather-Gaffney criterion which states that a frontal is stable if and only if it has isolated instability. Sections 5 and 6 are devoted to show how to construct stable frontals as frontal versal unfoldings of plane curves or as a well defined sum of frontal unfoldings. We define the frontal reduction of an -versal unfolding of a plane curve and prove that it is, in fact, a versal frontal unfolding. As a by product we relate the frontal codimension of a plane curve with its -codimension and prove the frontal Mond conjecture (stated in [22]) in dimension 1, which says that the frontal codimension is less than or equal to the frontal Milnor number (the number of spheres in a stable deformation) with equality if the germ is quasi-homogeneous. We also give a method to construct stable unfoldings which are not necessarily versal. We then turn our attention to characterizing stability of frontal multigerms defining a frontal Kodaira-Spencer map which also yields a tangent space to the iso-singular locus (the manifold along which the frontal is trivial). Finally we use our methods to obtain a complete list of stable 3-dimensional frontals in . Note that generic wave fronts were classified by Arnol’d in [1] and, on the other hand, Ishikawa classified stable Legendrian maps (which may have different projected frontals), but, until now, a complete classification of stable frontals was only known for ([1]) and ([23]).
For technical reasons in order to use Ishikawa’s results we restrict ourselves to the case of frontals whose Legendrian lift has corank 1.
2. Frontal map-germs
Let be a smooth manifold of dimension . A field of hyperplanes over is a contact structure for if, for all , there exist an open neighbourhood of and a such that
- (1)
; 2. (2)
the fibre of at is ; 3. (3)
.
We call the local contact form of , and define a contact manifold as a pair , where is a contact structure on . Given a smooth manifold of dimension , a submersion is a Legendrian fibration for if, for all ,
[TABLE]
Example 2.1**.**
Let be the projectivised cotangent bundle of , and . The differential -form
[TABLE]
defines a contact structure on . The projection given by is a Legendrian fibration under this contact structure.
Definition 2.2**.**
Let , be Legendrian fibrations. A diffeomorphism between contact manifolds is
- (1)
a contactomorphism, if ; 2. (2)
a Legendrian diffeomorphism if it is a contactomorphism and there exists a diffeomorphism such that .
We say is contactomorphic to if there is a contactomorphism .
A well-known result by Darboux states that any two contact manifolds of the same dimension admit a local diffeomorphism such that (see e.g. [27], §20.1). In particular, if , is locally contactomorphic to the contact manifold described in Example 2.1; therefore, we can restrict oruselves to the setting given in Example 2.1.
Let be an open subset. A mapping is integral if .
Definition 2.3**.**
A smooth mapping is frontal if there exist an integral mapping and a Legendrian fibration such that . If is an immersion, we say is a wave front. Similarly, a hypersurface is frontal (resp. a wave front) if there exists a frontal map (resp. wave front) such that .
Definition 2.4**.**
Let be a finite set. A smooth multigerm is frontal if it has a frontal representative . Given a hypersurface , is a frontal hypersurface germ if there exists a frontal map germ such that .
Let be an integral map and : there exist such that
[TABLE]
where are coordinates for . Setting , this is equivalent to for all . Since is a fibre bundle, we can find for each pair an open neighbourhood of and an open such that . Therefore, is contact equivalent to the mapping , known as the Nash lift of .
If we assume that is nowhere dense in , the differential form is uniquely determined by , giving us a one-to-one correspondence between and . Such a frontal map is known as a proper frontal map (according to Ishikawa [15]). We also define the integral corank of a proper frontal as the corank of its Nash lift.
For the rest of this article, we shall assume all frontal map germs are proper. Note that the notion of topological properness (i.e. the preimage of a compact subset is compact) is not used throughout this article.
Example 2.5**.**
Let be the smooth map germ given by
[TABLE]
It is easy to see that has corank and the singular set is nowhere dense in . Furthermore, the assumption that implies that the Jacobian ideal of is generated by , and thus it is a proper frontal map germ by Proposition 2.6 below. In particular, the differential -form
[TABLE]
verifies that for all , and has corank equal to the number of that are greater than . Therefore, the integral corank of is also equal to the number of greater than . In particular, is a wave front when all are equal to .
Proposition 2.6** ([15], Lemma 2.3).**
Let be a map germ. If is frontal, then the Jacobian ideal of is principal (i.e. it is generated by a single element). Conversely, if is principal and is nowhere dense in , then is a proper frontal map germ.
If has corank , we may choose local coordinates in the source and target such that
[TABLE]
in which case is the ideal generated by and , and we recover the following criterion by Nuño-Ballesteros [23]:
Corollary 2.7**.**
Let be a frontal map germ of corank , and choose coordinates in the source and target such that is given as in Equation (2). Then is a frontal map germ if and only if either or .
We shall say that is in prenormal form if it is given as in Equation (2) with for some , in which case the Nash lift becomes
[TABLE]
In particular, note that if , then , and is a wave front.
3. Lowering Legendrian equivalence
The first strides in the classification of frontal mappings were done by Arnol’d and his colleagues in a series of articles published in the 1970s and 1980s. In his work, he established a notion of equivalence native to Legendrian maps (known as Legendrian equivalence) and developed a classification of all simple, stable wave fronts (see [27], Chapter 21).
Ishikawa extended Arnol’d’s theory of Legendrian equivalence to the broader class of integral mappings in [14], defining a notion of infinitesimal stability and showing that an integral map of corank at most is Legendrian stable if and only if it is infinitesimally stable. He also showed that all Legendrian stable integral mappings of corank at most belong to a special family called open Whitney umbrellas, giving a characterisation of stable umbrellas in terms of a certain -algebra .
The goal of this section is to formulate a notion of frontal stability and versality that does not require the use of contact geometry.
Remark 3.1**.**
Let be a proper frontal map germ with Nash lift . Since is an equivalence class in a projective space, there exists a such that is non-vanishing, so we can rewrite Equation (1) as
[TABLE]
where the hat symbol denotes an ommited summand. We then define local coordinates on such that and
[TABLE]
These are known as the Darboux coordinates of . In particular, Equation (4) implies that the mapping shares the same singular set with . Therefore, there exists a representative of which is immersive outside of a nowhere dense subset of .
Definition 3.2**.**
Let be finite sets. Two integral map germs
[TABLE]
are Legendre equivalent if there exists a diffeomorphism and a Legendrian diffeomorphism such that .
Arnol’d showed in [27], §20.4 that a Legendrian diffeomorphism is locally determined by a choice of Legendrian fibrations in the source and target, and a diffeomorphism between the base spaces. Nonetheless, his proof was based on the fact that a Legendrian diffeomorphism preserves the fibres, and no explicit expression is given for .
Theorem 3.3**.**
Given a diffeomorphism , the mapping
[TABLE]
induces a Legendrian diffeomorphism .
Proof.
Let : since is a diffeomorphism, and is a well-defined diffeomorphism. Furthermore, it is clear that
[TABLE]
by construction. Therefore, we only need to show that .
Let and . Since is a submersion, , and it follows from (5) that
[TABLE]
Conversely, let . Since is a diffeomorphism, there exists a unique such that . By definition of , we have
[TABLE]
By (5), this implies that , from which follows that . ∎
Remark 3.4**.**
Let be a smooth -parameter family of diffeomorphisms. Given in an open neighbourhood of [math], we know by Theorem 3.3 that we can lift onto a Legendrian diffeomorphism . Since is a fibre bundle and is a paracompact Hausdorff space, is a fibration (see [26], Corollary 2.7.14), so it verifies the homotopy lifting property. Therefore, the -parameter family defined in this way is, indeed, a lift of the family .
Corollary 3.5**.**
Let :
- (1)
if is -equivalent to and is frontal, is frontal; 2. (2)
if and are frontal, is Legendrian equivalent to if and only if is -equivalent to .
Proof.
Assume that is frontal: there exist an integral map germ such that , where is the canonical bundle projection. Now let , be diffeomorphisms such that : by Theorem 3.3, we can lift onto a Legendrian diffeomorphism . Therefore, the map is an integral map such that , and is frontal. This proves the first item.
For the second item, the “only if” is proved in a similar fashion. For the “if”, let and be diffeomorphisms such that , with Legendrian. By definition of Legendrian diffeomorphism, there exists a diffeomorphism such that , from which follows that
[TABLE]
proving the second item. ∎
3.1. Unfolding frontal map germs
The theory of Legendrian equivalence describes homotopic deformations of a pair via integral deformations, deformations of which are themselves integral for any fixed . Nonetheless, frontal deformations often fail to preserve the frontal nature across the parameter space, as showcased in Example 3.6 below.
Example 3.6**.**
Let be the plane curve . The -parameter deformation verifies that is frontal for all . If is a -form such that for all in an open neighbourhood of , a simple computation shows that must be given in the form
[TABLE]
for some . Therefore, does not yield an integral deformation at .
Definition 3.7**.**
Let be a frontal germ. An unfolding of is frontal if it is frontal as a map germ.
Theorem 3.8**.**
Let be a frontal map germ. A -parameter unfolding of is frontal if and only if is an integral deformation of .
Proof.
Let be a frontal -parameter unfolding for : there is a such that for all . If we set , we can write
[TABLE]
for some . Therefore, may be regarded as a -parameter deformation of and the Nash lift of ,
[TABLE]
is an integral -parameter deformation of . Since is an integral map, for all . Properness of then implies that , and thus the map germ (6) is an integral deformation of .
Conversely, let be an integral deformation of . Taking coordinates in the source and Darboux coordinates in the target, the integrability condition becomes
[TABLE]
for . Consider the differential form given by
[TABLE]
Using the integrability condition above, we have
[TABLE]
Therefore, for all and is frontal. ∎
Remark 3.9**.**
Properness of is required for the “if” direction, since is not guaranteed to be a deformation of , even if it is integral. Nonetheless, the “only if” direction does not require properness.
The space of infinitesimal integral deformations of an integral , defined by Ishikawa in [14], is given by
[TABLE]
This space is linear when has corank at most ([14]), but it is known to have a conical structure in higher coranks. Counterexamples can be constructed using a similar procedure as in [11]. We also set as the subspace of given by those which are trivial Legendrian deformations of .
Definition 3.10**.**
Let be a frontal map germ of integral corank at most . We define the space of infinitesimal frontal deformations of as
[TABLE]
As shown in Theorem 3.12 below, is the linear projection of . Therefore, if the integral corank of is at most , is -linear; for this reason, any results involving will implicitly assume that has integral corank at most . An alternative, direct proof is also given for corank frontal map germs in Remark 5.12 below.
Lemma 3.11**.**
Given a frontal map germ , .
Proof.
Let , be two smooth -parameter families of diffeomorphisms and . It is clear by construction that the vector field germ given by is in .
By Theorem 3.3, we can lift onto a smooth -parameter family of Legendrian diffeomorphisms, in which case we can lift onto an integral deformation . Using Theorem 3.8, we then see that the unfolding is frontal. Therefore, the vector field germ given by is in , and thus . ∎
Theorem 3.12**.**
Let be a frontal map germ and be the canonical bundle projection. The mapping given by is a -linear isomorphism and induces an isomorphism
[TABLE]
Proof.
Let and be an integral -parameter deformation of and : by Theorem 3.8, is a frontal -parameter unfolding of . Furthermore, using the chain rule, we see that , so and is well-defined. Conversely, let and be a frontal -parameter deformation of with : by Theorem 3.8, we can lift onto an integral -parameter deformation of . Using the chain rule, it then follows that , so .
We move onto injectivity. Let be an integral -parameter deformation of with . If we assume that , then
[TABLE]
Our goal is to show that we can write for some , so that and thus .
Since is an integral deformation of , it verifies the identity
[TABLE]
Taking the coefficient of on both sides of the equation and simplifying yields
[TABLE]
Taking gives us the homogeneous system of equations
[TABLE]
for . Using the observation from Remark 3.1 and the continuity of , we conclude that and thus .
It only remains to show that . Let : there exist -parameter families , of diffeomorphisms such that , with Legendrian. Since is Legendrian for all in a neighbourhood of [math], there exists a -parameter family of diffeomorphisms such that for all . We then have that , hence .
Conversely, if , there exist -parameter families , of diffeomorphisms such that . Using Theorem 3.3, there exists a -parameter family of Legendrian diffeomorphisms such that , and thus we can lift onto , whose image via is . ∎
Remark 3.13**.**
Let be a frontal map germ: Theorem 3.12 states that . Since has corank , a resut by Ishikawa [14] states that
[TABLE]
wherein denotes the natural lifting of the contact form in . Taking Darboux coordinates in ,
[TABLE]
In particular, if has corank and it is given in prenormal form, Equation (8) is equivalent to
[TABLE]
where are given as in Equation (3).
Definition 3.14**.**
The frontal codimension of is defined as the dimension of . We say is -finite or has finite frontal codimension if .
3.2. Frontal versality and stability
In the previous subsection, we formulated the notions of integral deformation and Legendrian codimension purely in terms of frontal unfoldings. We now show that Ishikawa’s results concerning the Legendrian stability and versality of pairs from [14] have a direct parallel in our theory of frontal deformations.
Definition 3.15**.**
A frontal map germ is stable as a frontal or -stable if every frontal unfolding of is -trivial.
Corollary 3.16**.**
A frontal map germ is stable as a frontal if and only if is Legendrian stable.
Proof.
Assume is stable as a frontal and let be an integral deformation of : by Theorem 3.8, defines a frontal unfolding of . Stability of then implies that is -equivalent to . By Corollary 3.5, this then implies that is Legendrian equivalent to . Since the choice of was arbitrary, we conclude is Legendrian stable. The opposite direction is shown similarly. ∎
Corollary 3.17**.**
A frontal map germ is -stable if and only if its -codimension is [math].
Proof.
Corollary 3.16 states that is -stable if and only if its Nash lift is Legendrian stable. Since has corank at most , so does , and a result by Ishikawa [14] states that is Legendrian stable for the bundle projection if and only if . However, it follows from Theorem 3.12 that this is equivalent to . ∎
Example 3.18**.**
The following frontal hypersurfaces are stable as frontals:
- (1)
Cusp: 2. (2)
Folded Whitney umbrella:
Let be a frontal map germ with -parameter unfolding , not necessarily frontal. Recall that the pullback of by is defined as the -paramter unfolding
[TABLE]
Definition 3.19**.**
Let be a frontal map germ. A frontal unfolding of is -versal or versal as a frontal if, given any other frontal unfolding of , there exist unfoldings and of the identity such that
[TABLE]
for some map germ .
Lemma 3.20**.**
Given a frontal map germ , a frontal unfolding is -versal if and only if is a Legendre versal deformation of .
Proof.
Assume is a versal frontal unfolding of and let be an -parameter integral deformation of . Theorem 3.8 implies that the -parameter unfolding is frontal. By versality of , there exist unfoldings , of the identity map germ and a smooth map germ such that .
Let be a representative of which is a proper frontal map, and be a representative of such that . A simple computation shows that ; therefore, since is nowhere dense in , is nowhere dense in and is a proper frontal map. Theorem 3.8 then states that lifts into integral deformation of .
Now consider representatives , , and such that as mappings. Since is a smooth -parameter family of diffeomorphisms, we can lift it onto a -parameter family of smooth Legendrian diffeomorphisms . Therefore,
[TABLE]
and is a versal Legendrian deformation of .
Conversely, let be a versal integral deformation of and be a frontal -parameter unfolding of . Theorem 3.8 implies that the -parameter deformation is integral. By versality of , there exist smooth families of diffeomorphisms and and a smooth map germ verifying the following:
- (1)
is a Legendrian diffeomorphism for all ; 2. (2)
and are the identity map germs; 3. (3)
.
By Item 1, we can find a smooth family of diffeomorphisms such that and is the identity map germ. It follows that
[TABLE]
If we now consider the unfoldings and , we have . We conclude that is versal as a frontal. ∎
Theorem 3.21** (Frontal versality theorem).**
Given a frontal map germ ,
- (1)
* admits a frontal versal unfolding if and only if it is -finite;* 2. (2)
a frontal unfolding of is versal as a frontal if and only if
[TABLE]
To show Theorem 3.21, we shall make use of
Theorem 3.22** (Ishikawa’s Legendre versality theorem [14]).**
Given an integral of corank at most ,
- (1)
* admits a versal Legendrian unfolding if and only if its Legendrian codimension is finite;* 2. (2)
a Legendrian unfolding of is versal if and only if
[TABLE]
Proof of Theorem 3.21.
By Lemma 3.20, a frontal unfolding of is versal as a frontal if and only if the smooth family is a versal Legendre deformation of . In particular, it follows from Theorem 3.8 that admits a versal Legendrian deformation if and only if admits a versal frontal unfolding. This fact shall be used to prove both items.
By Theorem 3.22, admits a -versal unfolding if and only if has finite Legendre codimension. However, it was proved in Theorem 3.12 that this is equivalent to being -finite. This shows the first Item.
We move onto the second Item. If is -versal, is a Legendre versal unfolding of by Lemma 3.20 and Equation (9) holds. Computing the image via on both sides of Equation (9) and using Theorem 3.12, we get
[TABLE]
Conversely, let us assume that (10) holds: using Theorem 3.12, we see that (9) holds as well. Therefore, is versal as a frontal. This shows the second Item. ∎
4. A geometric criterion for -finiteness
The Mather-Gaffney criterion states that a smooth is -finite if and only if there is a finite representative with isolated instability. For example, the generic singularities for are transversal double points, with Whitney umbrellas and triple points in the accumulation (see e.g. [20] §4.7). This implies that generic frontal singularities such as the folded Whitney umbrella (see Example 3.18) are not -finite, since it contains cuspidal edges near the origin. Nonetheless, cuspidal edges are generic within the subspace of frontal map germs ([1]), which suggests the existence of a Mather-Gaffney-type criterion for frontal hypersurfaces.
Proposition 4.1**.**
A germ of analytic plane curve is -finite if and only if it is -finite.
Proof.
If is -finite, it is clear that it is also -finite, since
[TABLE]
Assume is -finite, and let be a representative of . By the Curve Selection Lemma [2], is an isolated subset in , so we can assume (by shrinking if necessary) that is a smooth submanifold of and . By the Mather-Gaffney criterion, it then follows that is -finite, as stated. ∎
Given a frontal map and , let . We define as the sheaf of -modules given by the stalk . We also set (resp. ) as the sheaf of vector fields on (resp. ) and the quotient sheaves
[TABLE]
Remark 4.2**.**
If is finite, we can take coordinates in and such that . By [13], we have the identity
[TABLE]
which is a -finite algebra by [12]. Since is finite, is -finite.
Proposition 4.3** ([14]).**
Let be a frontal map germ. If is -equivalent to an analytic (not necessarily integral) such that ,
[TABLE]
where are the coordinates of in the fibres of .
Remark 4.4**.**
Let and be given as in the statement above. If we assume that has corank and is given as in Equation (2), .
Corollary 4.5**.**
Let be a frontal map germ. If is finite and , there is a representative of such that is a coherent sheaf.
Proof.
Using Proposition 4.3, we have
[TABLE]
Since is finite, is -finite, as shown in Remark 4.2. Therefore, the stalk of at is finitely generated and is of finite type.
Let be an open set and an epimorphism of -modules. Since is a Noetherian ring, every submodule of is finitely generated. In particular, is finitely generated. We then conclude that is a coherent sheaf. ∎
Theorem 4.6** (Mather-Gaffney criterion for frontal maps).**
Let be a frontal map germ. If is finite and , is -finite if and only if there exists a representative of such that the restriction is locally -stable.
Proof.
The case for follows easily from the Mather-Gaffney criterion for -equivalence and Proposition 4.1. Therefore, we assume .
Suppose first that has finite -codimension: by Corollary 4.5, is a coherent sheaf. In addition,
[TABLE]
By Rückert’s Nullstellensatz, there exists an open neighbourhood of [math] in such that . Therefore, every other stalk of is [math], and the restriction of to is -stable, where .
Conversely, suppose that there exists a representative such that the restriction is locally -stable. Given , , so there exists an open neighbourhood of [math] in such that . By Rückert’s Nullstellensatz, it follows that the dimension of the stalk of at [math] is finite, but that dimension is equal to . We conclude that the germ of at [math] is -finite. ∎
5. Frontal reduction of a corank map germ
In [22], we presented the notion of frontalisation for a fold surface , and proved that the frontalisation process preserves some of the topological invariants of . We also defined frontal versions of Mond’s , , and singularities (see [18]), observing that none of them are wave fronts. We now seek to describe a more general procedure to generate frontals using arbitrary corank map germs.
Example 5.1**.**
Let be the parametrised curve : the unfolding given by
[TABLE]
is an -miniversal deformation for . By Proposition 2.7 and since , is frontal if and only if . If is such that , a simple computation then shows that the identity
[TABLE]
holds if and only if , and . Setting , we obtain the unfolding
[TABLE]
which is a swallowtail singularity.
In this section, we show that the frontal reduction of the versal unfolding of a plane curve is a -versal unfolding. The proof of this result gives a procedure to compute the frontal reduction of a given unfolding (versal or otherwise) via a system of polynomial equations, which may be solved using a computer algebra system such as Oscar or Singular.
Remark 5.2** (Piuseux parametrisation).**
Let be an analytic plane curve with isolated singularities. There exists a such that . By Piuseux’s Theorem (see e.g. [28], Theorem 2.2.6, or [5], Theorem 5.1.1), if , for some . Therefore, is -equivalent to the plane curve
[TABLE]
In particular, is -finite (and thus finitely determined) by the Mather-Gaffney criterion, so we can further assume that .
If , it suffices to replace with its complexification in the argument above, as is analytic. Therefore, such a parametrisation also exists in the real case.
Lemma 5.3**.**
Let be the plane curve from Remark 5.2. There exists a smooth -parameter deformation such that
[TABLE]
is a miniversal unfolding of .
Proof.
Let be a -basis for : by Martinet’s theorem, a miniversal unfolding for is given by the expression
[TABLE]
A simple computation shows that
[TABLE]
Using Equation (12), we may assume that and for . Setting , Equation (11) becomes
[TABLE]
as claimed. ∎
Remark 5.4**.**
Let be a smooth map-germ and be the unfolding from Lemma 5.3. The pullback is given by
[TABLE]
where , and . As we saw in the proof of Lemma 5.3,
[TABLE]
where can be assumed to be a polynomial function (due to Remark 5.2). Therefore, the component functions of are elements of , the algebra of polynomials on with coefficients in .
Theorem 5.5**.**
If has a miniversal -parameter unfolding , there is an immersion with the following properties:
- (1)
* is a frontal unfolding of ;* 2. (2)
if is frontal for any other , is equivalent as an unfolding to a pullback of .
Therefore, is a frontal miniversal unfolding.
We shall denote as and call it a frontal reduction of .
Proof.
Let be the unfolding from Lemma 5.3 and . We first want to show that there is an immersion making a frontal map germ; to do so, we shall derive a system of equations that determines whether a given pullback yields a frontal unfolding.
Let . By Remark 5.4, , so we can write . Since is a corank map germ, Corollary 2.7 states that it is frontal if and only if either or ; in particular, we can assume that , allowing us to impose the condition to .
If for some , there will exist such that . Therefore, the identity is equivalent to
[TABLE]
for . For , we may solve for to get the expression
[TABLE]
The remaining terms define an immersion germ given by which verifies Equation (13) by construction. This proves Item 1.
Let be a frontal unfolding of : versality of implies that is equivalent to for some . Let be a one-to-one representative of , be the projection
[TABLE]
and be a representative of . Since is frontal, verifies Equation (13) and thus by construction. Given , there exists a unique such that
[TABLE]
and thus . ∎
Example 5.6**.**
Consider Arnol’d’s singularity, . A versal unfolding of this curve is given by
[TABLE]
The frontal reduction of this unfolding may now be computed using Equation (13), which can be written in matrix form as
[TABLE]
Since this system has five equations and only three unknowns, we can now solve for , yielding and .
Remark 5.7**.**
While the method of frontal reductions successfully turns -versal unfoldings into -versal unfoldings, the same does not hold for stable unfoldings. For example, given the plane curve , , a stable unfolding of is given by . However, the only pullback that can turn into a frontal map germ is , giving us , which is not stable by hypothesis.
A more general method to compute stable unfoldings will be given in §6.
Corollary 5.8**.**
Given ,
[TABLE]
Consequently, if is the zero locus of some analytic ,
[TABLE]
Proof.
In the proof of Theorem 5.5, we see that , where and . Since is a miniversal -parameter unfolding, , giving the first identity.
Now assume : Milnor’s formula [17] states that the delta invariant and the Milnor number of are related via the identity , since is a mono-germ. On the other hand, a result in [8] states that , being the Tjurina number, hence yielding the expression
[TABLE]
In particular, the order of is equal to (see [5] Corollary 5.1.6).
For , simply note that , and , where is the complexification of . ∎
Example 5.9**.**
Let be the singularity, with normalisation . Direct computations show that
[TABLE]
from which follows that its -codimension is and its -codimension is . Therefore, we have , as expected.
The image of is given as the zero locus of the function . Using the second expression for the frontal codimension, we have
[TABLE]
as expected, since both the Tjurina and Milnor numbers of are .
In [22] §5, we introduced the notion of frontal Milnor number for a frontal multi-germ . This analytic invariant was defined in a similar fashion to Mond’s image Milnor number [19], only changing smooth stabilisations for frontal ones. We then conjectured that verified an adapted version of Mond’s conjecture, which we called Mond’s frontal conjecture.
Applying [22], Proposition 5.10 to Corollary 5.8, we can now prove Mond’s frontal conjecture in dimension .
Corollary 5.10**.**
Given a plane curve , , with equality if is quasi-homogeneous.
Proof.
Let be a non-constant analytic plane curve. By the Curve Selection Lemma [2], has an isolated singularity at the origin, so it is -finite and
[TABLE]
with equality if is quasi-homogeneous (see [19]). By Corollary 5.8, is -finite and . Using [22] Proposition 5.10 and Conservation of Multiplicity (see e.g. [20], Corollary E.4), , as stated above. Therefore,
[TABLE]
with equality if is quasi-homogeneous. ∎
Now let be a corank frontal map germ with isolated frontal instability. We can choose coordinates in the source and target such that
[TABLE]
for some . We then set as the projection on the coordinate of and consider the generic slice of , given by . Since has isolated frontal instabilities, is -finite (see Proposition 4.1 above) and we may consider a versal unfolding of with frontal reduction
[TABLE]
It is not true in general that the sum of two frontal mappings is frontal (e.g. and ), but we can still construct a frontal sum operator that yields a frontal mapping given two frontal mappings with corank at most . Let such that
[TABLE]
we define the frontal sum of and as , where
[TABLE]
This map germ constitutes an unfolding of both and by construction. Versality of then implies that is also versal, and thus stable. Therefore, frontal sums allow us to construct stable frontal unfoldings that are not necessarily versal.
Example 5.11** (Frontalised fold surfaces).**
Let be a frontal fold surface given in the form
[TABLE]
wherein we assume . The function has order , so can be seen as a smooth -parameter unfolding of the curve
[TABLE]
A frontal miniversal unfolding for is given by
[TABLE]
and we can recover by setting . Taking gives the stable unfolding
[TABLE]
Remark 5.12**.**
The frontal sum defined on (14) can be used to show that is linear when has corank at most : first, since is a corank frontal, we take coordinates in the source and target such that
[TABLE]
and consider the generic slice .
Let with respective integral -curves , . Since and are unfoldings of , they may also be regarded as unfoldings of . We then consider the frontal sum of and , and set . Note that the image of is simply the intersection of the image of with the hypersurface of equation , so is frontal.
Using the chain rule and Leibniz’s integral rule, we see that
[TABLE]
and thus .
6. Stability of frontal map germs
In §5, we described a method to generate -versal unfoldings of analytic plane curves using pullbacks. Nonetheless, as pointed out in Remark 5.7, the pullback of a stable unfolding is generally not stable as a frontal.
In this section, we describe a technique to generate stable frontal unfoldings, not too dissimilar to the method Mather used to generate all stable map germs. We also give a classification of all -stable proper frontal map germs of corank in §6.2, aided by Hefez and Hernandes’ Normal Form Theorem for plane curves [9, 10].
Let be a frontal map germ and . By definition of , is given by a frontal -parameter unfolding of ; this is, verifies that
[TABLE]
for some . If we now consider the vector field germ with , is given by the -parameter unfolding . This unfolding is frontal if and only if
[TABLE]
for some . Expanding on both sides of the equality and rearranging, we see that Equation (15) is equivalent to
[TABLE]
Therefore, the ring acts on via the usual action. In particular, , so is an -module via the action .
If we assume that has integral corank (so that is a -vector space), we can define the -vector spaces
[TABLE]
We also define the frontal -codimension of as the dimension of in , and will say that is -finite if .
Remark 6.1**.**
The space is not generally a -module via the usual action: consider the plane curve given by . Using Remark 3.13, we see that , but .
Recall that the Kodaira-Spencer map is defined as the mapping sending onto , where is such that . Since is frontal, the image of is contained within , and the target space becomes . Similarly, the kernel of this becomes
[TABLE]
since no element in has a preimage.
Lemma 6.2**.**
The map germ is -stable if and only if is surjective.
Proof.
Assume is -stable and let : there exist and such that . Setting , it follows that , and surjectivity of follows.
Conversely, assume is surjective: we have the identity
[TABLE]
Set and denote by the quotient projection. We may then write Equation (16) as
[TABLE]
Since is finitely generated over , so is . This implies that is finitely generated over , so is finitely generated over by Weierstrass’ Preparation Theorem. Since is a local ring, Nakayama’s lemma implies that , which is equivalent to , and frontal stability follows. ∎
Theorem 6.3**.**
A frontal with branches is -stable if and only if are -stable and the vector subspaces meet in general position.
Proof.
Let be either or one of its branches. By Lemma 6.2, is -stable if and only if is surjective; this is,
[TABLE]
Let , the ring isomorphism induces a module isomorpism , which in turn induces an isomorphism
[TABLE]
On the other hand, the spaces meet in general position if and only if the canonical map
[TABLE]
is surjective. The statement then follows from (17 - 19). ∎
We now use Ephraim’s theorem to give a geometric interpretation to , . Recall that the isosingular locus of a complex space at is defined as the germ at of the set of points such that is diffeomorphic to . Ephraim [6] showed that is a germ of smooth submanifold of and its tangent space at is given by the evaluation at of the elements in the space
[TABLE]
where is the ideal of map germs vanishing on . We shall now use this result to give a geometric interpretation to the space .
Proposition 6.4**.**
Let be a finite, frontal map germ with integral corank . If is -stable and , is the tangent space at [math] of .
To prove this result, we shall make use of the following
Lemma 6.5** (cf. [20]).**
Let be a finite, frontal map germ with integral corank and . If is -finite and ,
[TABLE]
Proof of Proposition 6.4.
By Ephraim’s theorem [6], the tangent space to at [math] is given by the evaluation at [math] of the elements in . Using Lemma 6.5, is the space of elements in that are liftable via . Therefore, we only need to show that the evaluation of [math] of this space coincides with .
Let : there exists a such that , so . Conversely, if verifies that , there exist , such that
[TABLE]
for some . Since is -stable, , which implies that
[TABLE]
Therefore, there exist and such that
[TABLE]
and . In particular, if , , thus finishing the proof. ∎
6.1. Generating stable frontal unfoldings
The generation of stable unfoldings in Thom-Mather’s theory of smooth deformations is done by computing the -tangent space of a smooth map germ of rank [math]. If is generated over by the classes of , Martinet’s theorem ([20], Theorem 7.2) states that the map germ
[TABLE]
is a stable unfolding of . While such a result fails to yield frontal unfoldings of frontal map germs, if has corank , we can still make use of the frontal sum operation defined on §5 to formulate a frontal version of Martinet’s theorem.
Lemma 6.6**.**
Let be a frontal map germ of integral corank with frontal unfolding , and be local coordinates on . There is an -linear isomorphism
[TABLE]
induced by the -linear epimorphism sending onto for and onto for .
Proof.
In [20], Lemma 5.5, it is shown that induces a -linear isomorphism . In particular, we can consider as a -epimorphism via . Note that for any frontal map germ with integral corank , so it suffices to show that sends onto .
Let with integral -curve : the integral -curve for is given by
[TABLE]
In particular, if is a frontal, is also frontal, since the image of is embedded within the image of . Conversely, given a frontal unfolding of , the map is a frontal unfolding of with , hence . ∎
As a consequence of Lemma 6.6, if is a stable frontal map germ, it is either the versal unfolding of some frontal map germ of rank [math] or a prism (i.e. a trivial unfolding) thereof.
Theorem 6.7**.**
Let be the plane curve from Remark 5.2, and
[TABLE]
If , then
[TABLE]
Proof.
Let : by Remark 3.13, if and only if , which in turn is equivalent to assuming that for some . Therefore,
[TABLE]
A simple computation shows that , hence for . However, , giving the first monomorphism. For the second monomorphism, first note that is finitely determined, so there exists a such that . If , there exist and such that . Using Equation (20), we see that
[TABLE]
Similarly, for all . ∎
If we now consider the -parameter unfolding ,
[TABLE]
and is frontal due to Corollary 2.7. Similarly, if we set with ,
[TABLE]
Since is a unit, and is also frontal.
If for some , we consider the -parameter frontal unfolding
[TABLE]
where denotes the frontal sum operation defined on Equation (14).
Example 6.8**.**
Let be the plane curve , which verifies that . We then consider the -parameter unfoldings
[TABLE]
whose frontal sum is
[TABLE]
This unfolding is -equivalent to the singularity from [14], Example 4.2.
Theorem 6.9**.**
The map germ defined on Equation (21) is stable as a frontal. Moreover, if the -codimension of over is , every other stable frontal unfolding of must have at least parameters.
Proof.
It is clear by definition of that
[TABLE]
so is -stable if and only if . By Lemma 6.6, this is equivalent to
[TABLE]
It follows from the definition of frontal sum that
[TABLE]
and thus is stable. ∎
6.2. Corank stable frontal map germs in dimension
By Theorem 6.3, a frontal multigerm is -stable if and only if its branches are -stable and meet in general position. Therefore, we only need to classify the stable monogerms.
By Lemma 6.6, every -stable monogerm with corank is a versal unfolding of an irreducible analytic plane curve with -codimension at most . In particular, if is the zero locus of some analytic , due to Corollary 5.8. A consequence of Theorem 6.7 is that , meaning that must be at most .
If , it follows from a result by Zariski [30] that . For , this yields an -stable plane curve; for , we can unfold into
[TABLE]
which is stable.
The cases and will be examined using Hefez and Hernandes’ classification of analytic plane curves from [10]. Every analytic plane curve has an associated invariant , known as the semigroup of values. If the curve is irreducible, its delta invariant is equal to
[TABLE]
regardless of its analytic family. Therefore, the expression only depends on .
For , is given by with , so . If , , so is either or . The case with implies that , which is impossible.
For , can be either or . If , is coprime with , so and we have two possible values for :
- (1)
if , , which implies that ; 2. (2)
if with ,
[TABLE]
Since , it follows that , giving us .
If , and , which implies that and . Using
[TABLE]
it follows that . Since we are only interested in the case , we can ignore this case.
For the remaining cases, the possible values for fall into one the following categories:
[TABLE]
for and . If , then , which is not possible.
Theorem 6.10**.**
Table 1 shows all stable proper frontal map germs of corank together with the plane curves of which they are versal unfoldings. All stable frontal multigerms are obtained by transverse self-intersections of these mono-germs, as shown in Theorem 6.3.
Proof.
The discussion conducted throughout this subsection shows that the only plane curves of frontal codimension less than or equal to 2 are , , , , and .
The curve is easily checked to be stable as a frontal. The family of curves for unfolds into , which is -equivalent to the folded Whitney umbrella ,which is stable as a frontal ([22, 23]).
The curves and unfold into the swallowtail and butterfly singularities ( and in Table 1), both of which are stable wave fronts ([27]). The singularity unfolds into Ishikawa’s singularity [14]. ∎
Conjecture 6.11**.**
The stable proper frontal map germs of corank are given by Ishikawa’s singularities, where
[TABLE]
where square brackets denote the floor function. All stable frontal multigerms are obtained by transverse self-intersections of these mono-germs, as shown in Theorem 6.3.
The algebra was introduced by Ishikawa in [14] in order to give a characterisation of Legendrian stability
7. Acknowledgements
We would like to thank M. E. Hernandes for his helpful contributions to §6.2.
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