Twist maps as energy minimisers in homotopy classes: symmetrisation and the coarea formula
Charles Morris, Ali Taheri

TL;DR
This paper studies twist maps as energy minimisers within specific homotopy classes in an annular domain, using symmetrisation and the coarea formula to establish minimality and local minimality results, especially in two dimensions.
Contribution
It demonstrates the minimality of twist maps as extremisers of a specific energy functional in their homotopy classes, employing symmetrisation and coarea techniques, with extensions to higher dimensions.
Findings
Twist maps are extremisers of the energy functional in their homotopy classes.
Twist maps are proven to be local minimisers of the energy in 2D.
Extensions to higher dimensions and related functionals are discussed.
Abstract
Let with fixed be an open annulus and consider the energy functional, \begin{equation*} {\mathbb F} [u; \X] = \frac{1}{2} \int_\X \frac{|\nabla u|^2}{|u|^2} \, dx, \end{equation*} over the space of admissible incompressible Sobolev maps \begin{equation*} {\mathcal A}_\phi(\X) = \bigg\{ u \in W^{1,2}(\X, \R^n) : \det \nabla u = 1 \text{ {\it a.e.} in and } \bigg\}, \end{equation*} where is the identity map of . Motivated by the earlier works \cite{TA2, TA3} in this paper we examine the {\it twist} maps as extremisers of over and investigate their minimality properties by invoking the coarea formula and a symmetrisation argument. In the case where is a union of infinitely many disjoint homotopy classes we…
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Taxonomy
TopicsGeometric Analysis and Curvature Flows · Nonlinear Partial Differential Equations · Geometric and Algebraic Topology
Abstract
Let with fixed be an open annulus and consider the energy functional,
[TABLE]
over the space of admissible incompressible Sobolev maps
[TABLE]
where is the identity map of . Motivated by the earlier works [15, 16] in this paper we examine the twist maps as extremisers of over and investigate their minimality properties by invoking the coarea formula and a symmetrisation argument. In the case where is a union of infinitely many disjoint homotopy classes we establish the minimality of these extremising twists in their respective homotopy classes a result that then leads to the latter twists being -local minimisers of in . We discuss variants and extensions to higher dimensions as well as to related energy functionals.
1 Introduction and preliminaries
Let with fixed be an open annulus in and consider the energy functional
[TABLE]
over the space of incompressible Sobolev maps,
[TABLE]
Here and in future denotes the identity map of and so the last condition in (1.2) means that on in the sense of traces.
By a twist map on we mean a continuous self-map of onto itself which agrees with the identity map on the boundary and has the specific spherical polar representation (see [16]-[18] for background and further results)
[TABLE]
Here lies in and sits on with satisfying . Therefore forms a closed loop in based at and for this in sequel we refer to as the twist loop associated with . Also note that (1.3) in cartesian form can be written as
[TABLE]
Next subject to a differentiability assumption on the twist loop it can be verified that with its energy simplifying to
[TABLE]
where the last equality uses . Now as the primary task here is to search for extremising twist maps we first look at the Euler-Lagrange equation associated with the loop energy defined by the last integral in (1) over the loop space . Indeed this can be shown to take the form (see below for justification)
[TABLE]
with solutions , where , is skew-symmetric and is described for by
[TABLE]
Now to justify (1.6) fix and for set and . Then and
[TABLE]
and so the arbitrariness of with an orthogonality argument gives (1.6).
Returning to (1.1) it is not difficult to see that the Euler-Lagrange equation associated with over is given by the system (cf. Section 4)
[TABLE]
where is a suitable Lagrange multiplier. Here a further analysis reveals that out of the solutions to (1.6) just described only those twist loops in the form
[TABLE]
when is even and () when is odd can grant extremising twist maps for the original energy (1.1). For clarification denotes the matrix of rotation by angle :
[TABLE]
Indeed direct computations give the angle of rotation to be
[TABLE]
when and
[TABLE]
when even. (See also [13], [16], [18] for complementing and further results.)
Our point of departure is (1.4)-(1.9) and the aim is to study the minimising properties the twist maps calculated above. Of particular interest is the case where the space admits multiple homotopy classes . Here direct minimisation of the energy over these classes gives rise to a scale of associated minimisers . Using a symmetrisation argument and the coarea formula we show that the twist maps with twist angle as presented in (1.10) are indeed energy minimisers in and as a result also local minimisers of over . We discuss variants and extensions including a larger scale of energies where similar techniques can be applied to establish minimality properties in homotopy classes.
2 The homotopy structure of the space of self-maps
The rich homotopy structure of the space of continuous self-maps of the annulus will prove useful later on in constructing local energy minimisers. For this reason here we give a quick outline of the main tools and results and refer the reader to [15] for further details and proofs. To this end set {\mathfrak{A}}={\mathfrak{A}}({\mathbb{X}})=\{f\in{\bf C}(\overline{{\mathbb{X}}},\overline{{\mathbb{X}}}):f=\phi\mbox{ on \partial{\mathbb{X}}}\} equipped with the uniform topology. A pair of maps are homotopic iff there exists such that, firstly, for all , secondly, for all and finally for all , . The equivalence class consisting of all homotopic to a given is referred to as the homotopy class of and is denoted by . Now the homotopy classes can be characterised as follows depending on whether or .
- •
() Using polar coordinates, for and for (fixed), the -valued curve defined by
[TABLE]
has a well-defined index or winding number about the origin. Furthermore, due to continuity of , this index is independent of the particular choice of . This assignment of an integer (or index) to a map will be denoted by
[TABLE]
Note firstly that this integer also agrees with the Brouwer degree of the map resulting from identifying , justified as a result of and secondly that for a differentiable curve (taking advantage of the embedding ) we have the explicit formulation
[TABLE]
Proposition 2.1**.**
. The map is bijective. Moreover, for any pair of maps , we have
[TABLE]
- •
() Using the identification where for ease of notation we have set it is plain that for the map 111Here as usual denotes the identity map of the -sphere and is the path-connected component of containing .
[TABLE]
uniquely defines an element of the fundamental group . By considering the action of on – viewed as its group of orientation preserving isometries, i.e., through the assignment,
[TABLE]
where
[TABLE]
it can be proved that the latter assignment induces a group isomorphism on the level of the fundamental groups, namely,
[TABLE]
Thus, summarising, we are naturally lead to the assignment of an integer mod to any which will be denoted by
[TABLE]
Proposition 2.2**.**
* The degree mod map is bijective. Moreover, for a pair of maps , we have*
[TABLE]
3 A countable family of local minimisers of when
When by Lebesgue monotonicity and degree theory (see [15] as well as [9],[11],[14],[19]) every map in has a representative (again denoted ) in . As a consequence we can introduce the components – hereafter called the homotopy classes,
[TABLE]
Evidently are pairwise disjoint and their union (over all ) gives . Furthermore it can be seen without difficulty that each is -sequentially weakly closed and that for and there exists with
[TABLE]
Here , that is, the -ball in centred at . Indeed for the sequential weak closedness fix and pick so that in . Then by a classical result of Y. Reshetnyak
[TABLE]
(as measures) and so while uniformly on gives by Proposition 2.1 that . For the second assertion arguing indirectly and assuming the contrary there exist , and in such that and while . However by passing to a subsequence (not re-labeled) in and as above uniformly on . Hence again by Proposition 2.1, for large enough which is a contradiction.
Now in view of the sequential weak lower semicontinuity of in (see below) an application of the direct methods of the calculus of variations leads to the following existence and multiplicity result.
Theorem 3.1**.**
Local minimisers Let and for consider the homotopy classes as defined by . Then there exists such that
[TABLE]
Furthermore for each such minimiser there exists such that
[TABLE]
for all satisfying .
*Proof. *Fix and pick an infimizing sequence: . Then as and for it follows that by passing to a subsequence (not re-labeled) in and uniformly in where by the above discussion . Now
[TABLE]
as together with
[TABLE]
gives the desired lower semicontinuity of the energy on as claimed, i.e.,
[TABLE]
As a result and so is a minimiser as required. To justify the second assertion fix and as above and with pick as in the discussion prior to the theorem. Then any satisfying also satisfies (3.5) [otherwise implying that and hence in view of being a minimiser, which is a contradiction.]
4 Twist maps and the Euler-Lagrange equation associated with
The purpose of this section is to formally derive the Euler-Lagrange equation associated with over . Note that can in principle be infinite if is too small or zero, however, for twist maps or more generally -integrable maps in , is bounded away from zero as is a self-map of onto itself. Moreover is -integrable for the latter maps but not in general for maps of Sobolev class (with ).
Now the derivation uses the Lagrange multiplier method and proceeds formally by considering the unstrained functional
[TABLE]
for suitable where evidently when . We can calculate the first variation of this energy by setting , where is sufficiently regular and satisfies in , for all and sufficiently small, hence obtaining,
[TABLE]
As this is true for every compactly supported as above an application of the fundamental lemma of the calculus of variation results in the Euler-Lagrange system for in :
[TABLE]
where the divergence operator is taken row-wise. Proceeding further an application of the Piola identity on the cofactor term gives (with )
[TABLE]
Next expanding the differentiation further allows us to write
[TABLE]
Finally transferring back into vector notation and invoking the incompressibilty condition it follows in turn that
[TABLE]
and subsequently
[TABLE]
Thus the Euler-Lagrange system (4.2) is equivalent to (4.6) that in particular asks for the nonlinear term on the left of (4.6) to be a gradient field in . Recall from earlier discussion that restricting to the class of twist maps results in the Euler-Lagrange equation (1.6) where the solution as explicitly computed is the twist loop associated with the map
[TABLE]
with , , skew-symmetric (). The boundary condition on gives, 222The function was introduced earlier in Section 1.
[TABLE]
Therefore it must be that and . Now as lies in it must be conjugate to a matrix in the Lie algebra of the standard maximal torus of orthogonal -plane rotations in . This means that there exists such that for some as described and so where , that is, is the lattice in the Lie subalgebra consisting of matrices sent by the exponential map to the identity of . Hence . Next upon noting that the derivatives of are given by
[TABLE]
we can write
[TABLE]
Now, moving forward, a set of straightforward calculations show that for a twist map with a twice continuously differentiable twist loop we have the differential relations
[TABLE]
and likewise
[TABLE]
Thus for the particular choice of a twist map with twist loop arising from a solution to (1.6) the above quantities can be explicitly described by the relations
[TABLE]
and likewise
[TABLE]
For the ease of notation we shall hereafter write . Proceeding now with the calculations and using - we have
[TABLE]
and in a similar way
[TABLE]
where the last identity here uses and along with for skew-symmetric . Hence putting together and gives
[TABLE]
which when combined with results in
[TABLE]
Noting with skew-symmetric and the last set of equations give
[TABLE]
Therefore to see if admits twist solutions it suffices to verify if the quantity described by is a gradient field in . Towards this end recall that here we have where as seen . Thus a basic calculation gives
[TABLE]
and likewise by substitution we have
[TABLE]
Hence using the above we can proceed by writing the Euler-Lagrange equation upon substitution as,
[TABLE]
Now as for a fixed skew-symmetric matrix by basic differentiation we have
[TABLE]
it is evident that we can write
[TABLE]
In particular with being skew-symmetric, can be written in the form
[TABLE]
Therefore it is plain that is a gradient field in provided that the term on the right and subsequently the middle term, that is, the expression
[TABLE]
is a gradient field in . By direct calculations (cf. [12]) this is seen to be the case iff all the eigenvalues of the skew-symmetric matrix are equal. (Note that in odd dimensions this requirement leads to .) As a result here would be a gradient (indeed ) and so the Euler-Lagrange system is satisfied by the twist .
Now using the representation for some and writing where, is the block diagonal matrix: when is odd and when is even, i.e.,
[TABLE]
it is required that . But invoking the lattice structure of this can happen iff
[TABLE]
and thus
[TABLE]
Noticing that here we have
[TABLE]
for and
[TABLE]
for even respectively we obtain the representation
[TABLE]
where we have set and the angle of twist function is given by (1.10) for and (1.11) for even respectively. For odd as shown and so the only twist solution to (4.6) is the trivial solution .
5 Symmetrisation as a means of energy reduction on when
Recall that the space of admissible maps consists of maps satisfying the incompressibility condition a.e. in and . Also as mentioned earlier due to a Lebesgue-type monotonicity every such map is continuous on the closed annulus and using degree theory the image of the closed annulus is again the closed annulus itself; hence, the ”embedding”
[TABLE]
where the components here are as defined by (3.1). For the sake of future calculations it is useful to write (2.2) as
[TABLE]
where . (Note that we adopt the convention that in two dimensions the cross product is a scalar and not a vector.) When is a twist map, specifically, the integral reduces to where as before is the angle of rotation function. We now proceed by reformulating the energy of an admissible map in a more suggestive way. Indeed switching to polar co-ordinates it is seen that
[TABLE]
where
[TABLE]
Next we note that
[TABLE]
Hence the gradient term on the left in (5.3) can be expressed as
[TABLE]
From this we therefore obtain the energy as
[TABLE]
Let us first state the following useful identity that will be employed in obtaining a fragment of the lower bound on the energy: For and ,
[TABLE]
The proof of this identity is postponed until later on in Section 7 (cf. Proposition 7.3). Now assuming this for the moment an application of Jensen’s inequality gives, again for ,
[TABLE]
Hence it is plain that
[TABLE]
Therefore we have the following lower bound on the energy of an admissible map :
[TABLE]
Interestingly here we have equality only for twist maps and so outside this class the inequality is strict (for more on questions of uniqueness see [10]). The next task is to show that by using a basic ”symmetrisation” in we can reduce the energy which will then be the main ingredient in the proof of the result.
Proposition 5.1**.**
Symmetrisation Let be an admissible map and associated with define the angle of rotation function by setting
[TABLE]
Then the twist map defined by with has a smaller energy than the original map , that is,
[TABLE]
Furthermore if then the symmetrised twist map satisfies . Thus the homotopy classes are invariant under symmetrisation.
Proof.
Clearly the symmetrised twist map is in the same homotopy class as since by definition satisfies and
[TABLE]
Therefore as a result of (5.2). Next the energy of satisfies the bound
[TABLE]
where the last line is a result of Jensen’s inequality. Therefore by referring to (5.9) all that is left is to justify the inequality
[TABLE]
Towards this end we use the isoperimetric inequality in the context of sets of finite perimeter and the coarea formula in the context of Sobolev spaces: For real-valued and non-negative Borel :
[TABLE]
(See, e.g., [3, 8].) Then upon taking and this gives
[TABLE]
Now since the level sets and enclose the same area due to a.e. (we can consider as extended by identity inside ) an application of the isoperimetric inequality gives for (cf., e.g., [3, 4]). Thus substituting in (5.16) results in the lower bound
[TABLE]
Finally we arrive at the conclusion by noting that and have the same distribution function, that is, again as a result of the pointwise constraint a.e. in : and therefore
[TABLE]
Now putting all the above together, a final application of Hölder inequality gives,
[TABLE]
and thus eventually we have
[TABLE]
and so the conclusion follows. ∎
6 The energy and connection with the distortion function
In this section we delve into the relationship between the energy functional in (1.1) and the notions of distortion function and energy of geometric function theory. In particular we show that in two dimensions twist maps have minimum distortion among all incompressible Sobolev homeomorphisms of the annulus with identity boundary values in any given homotopy class. To fix notation and terminology let be open sets and . Then is said to have finite outer distortion iff there exists measurable function with such that
[TABLE]
The smallest such is called the outer distortion of and denoted by . Note that here is the Hilbert-Schmidt norm of the matrix . Naturally and it measures the deviation of from being conformal. We also speak of the inner distortion function defined by the quotient
[TABLE]
when and otherwise. We define the distortion energy associated to the inner distortion (6.2) by the integral
[TABLE]
Related energies and more have been considered in [6] with close links to the work in [2]. The connection between the energy and the distortion energy (6.3) is implicit in the following result of T. Iwaniec, G. Martin, J. Onninen and K. Astala [2]. (See also [1], [6] and [7].)
Theorem 6.1**.**
Suppose is a homeomorphism with finite outer distortion. Assume is -integrable over . Then the inverse map lies in the Sobolev space . Furthermore
[TABLE]
*Proof. *The first assertion is Theorem 10.4 pp. 22 of [2]. For the second assertion using definitions we have
[TABLE]
and the conclusion follows upon dividing by and integrating using the area formula.
Now let {\mathcal{A}}^{n}_{\phi}({\mathbb{X}})=\{u\in W^{1,n}({\mathbb{X}};{\mathbb{R}}^{n}):\det\nabla u=1\mbox{ {\it a.e.} in {\mathbb{X}}u|_{\partial{\mathbb{X}}}=\phi}\}. As in Section 2 each in admits a representative in . Now restricting to homeomorphisms the above theorem gives and so by the incompressibility constraint
[TABLE]
In the planar case this allows us to relate the distortion energy of a homeomorphism , say, in to the energy of the inverse map in through
[TABLE]
Therefore by showing that twist maps minimise the energy within their homotopy classes we have implicitly shown that twist maps minimise the distortion energy within their respective homotopy classes of homeomorphisms (as the inverse of a twist map is a twist map in opposite direction and clearly twist maps are homeomorphisms of annuli onto themselves).
Theorem 6.2**.**
The distortion energy has a minimiser ($$k\in{\mathbb{Z}}$$) among all homeomorphisms within . The minimiser is a twist map of the form where . In particular the minimum energy is given by,
[TABLE]
*Proof. *That minimises amongst homeomorphisms in is a result of minimising over (Proposition 5.1) and (6.6). Indeed arguing indirectly assume there is a homeomorphism : . Then by (6.6), and this is a contradiction as , while . We are thus left with the calculation of the energy of . To this end put :
[TABLE]
and so a further reference to (6.6) completes the proof.
In the higher dimensions, i.e. , from Theorem 6.1 we can get an analogous identity to (6.6) for homeomorphisms in . Indeed, with
[TABLE]
where the energies and are given by,
[TABLE]
Therefore again to find minimisers of among homeomorphisms in one can follows the lead of and consider the energy over . It is straightforward to see that we have equality in (6.9) for twist maps with the distortion energy of given by
[TABLE]
Now restricting to the particular case of the twist map being (cf. [13])
[TABLE]
with is as in Section 4 and the angle of rotation describing the twist. The corresponding distortion energy is
[TABLE]
Note that in higher dimensions (i.e., ) as discussed earlier there are only two homotopy classes in . A twist map lies in the non-trivial homotopy class of iff the twist loop based at lifts to a non-closed path connecting in (see [17] for more.) 333Note that is the universal cover of and is the fibre over under the covering map.
Likewise a twist of the form (6.12) lies in the non-trivial homotopy class of iff the angle of rotation function satisfies for some odd. When is even the twist map lies in the trivial homotopy class of . 444The identity boundary conditions on dictates that the angle of rotation function must satisfy for some .
7 Other variants of the Dirichlet energy
The goal of this section is to establish various energy bounds and identities, when , by invoking the regularity and the measure preserving constraints satisfied by the elements of . These inequalities will ultimately lead to useful results for extremisers and minimisers of variants of the Dirichlet energy in homotopy classes of . We begin with the following identity.
Proposition 7.1**.**
For the integral identity
[TABLE]
holds for all .
Proof.
Denoting by the distribution function of we can write using basic considerations and invoking the standard properties of distribution functions
[TABLE]
which is the required conclusion. ∎
We now collect a few more results which will be needed for the proof of our main theorem at the end of this section.
Proposition 7.2**.**
Let and pick . Consider the continuous closed curve where is fixed. Then the integral identity
[TABLE]
holds for almost every , where .
*Proof. *We shall justify the assertion first when is a sufficiently smooth diffeomorphism and then pass on to the general case by invoking a suitable approximation argument. Towards this end consider first the case where is a smooth diffeomorphism with on . [Here need not satisfy the incompressibility condition in .] Let denote the -form
[TABLE]
Then by a rudimentary calculation the pull-back of under the curve is given by
[TABLE]
Hence contour integration and basic considerations lead to the integral identity
[TABLE]
Note that the curve here is diffeomorphic to and as such by the Jordan-Schöenflies theorem is the boundary of some bounded region diffeomorphic to the unit ball . In particular due to the boundary conditions on we have that when and so as a result with boundaries of and . Hence application of Stoke’s theorem gives
[TABLE]
for all . Next again by a rudimentary calculation we obtain that the pull-back of is,
[TABLE]
Hence from (7.7) and (7.8) it follows that for all ,
[TABLE]
Now pick an arbitrary in . By approximation, e.g., using Theorem 1.1 in [5] there is a sequence of diffeomorphisms so that with uniformly on and strongly in . Hence,
[TABLE]
a.e. in . Note that , for some and so and by virtue of in and dominated convergence, for each and , we have
[TABLE]
In a similar spirit we have (suppressing the arguments of for brevity)
[TABLE]
a.e. in . Again since , for some we have and so by dominated convergence
[TABLE]
Now combining (7.9) and (7.11) together with the fact that on it follows that
[TABLE]
Moreover (7.13) and a final application of dominated convergence gives
[TABLE]
Therefore the result follows by recalling that in and applying the Lebsegue differentiation theorem, i.e., dividing by and letting .
Note that we can write the conclusion of the above proposition, namely, the integral identity (7.3) in a shorter and somewhat more suggestive form
[TABLE]
where for . With this result and formulation at our disposal we can now prove the earlier relation as a specific proposition.
Proposition 7.3**.**
Taking in the above gives the integral identity
[TABLE]
Proof.
When it can be easily seen that and therefore Proposition 7.2 gives that,
[TABLE]
Then recalling that on , i.e. when , it can be seen that the integral over the inner boundary is and hence from (7.16) this implies that,
[TABLE]
which completes the proof. ∎
Proposition 7.4**.**
Suppose such that is a monotone increasing function. Then for almost every we have that
[TABLE]
Proof.
First we note that by Proposition 7.2 we have for a.e. that
[TABLE]
As is monotone increasing and and share the same distribution function we have that,
[TABLE]
In the above . Now since,
[TABLE]
by Proposition 7.1 we obtain upon using (7.20) in (7.21) that,
[TABLE]
Therefore,
[TABLE]
but from the identity boundary conditions on we know that,
[TABLE]
and therefore,
[TABLE]
The result then follows from an application of Jensen’s inequality. ∎
With the aid of these bounds we can now move on to the main goal of the section, namely, formulating and proving minimality for twist maps in homotopy classes of for a larger class of energies than those considered earlier.
Theorem 7.5**.**
Let and let denote the energy functional,
[TABLE]
where lies in and with such that is monotone increasing. Then for any ($$k\in{\mathbb{Z}}$$) there exists a twist map defined by the same symmetrisation as in such that,
[TABLE]
whilst . 555Note that taking , i.e., , gives .
Proof.
As the first step in the proof we wish to prove the inequality
[TABLE]
In order to do this we again need to apply the isoperimetric inequality, the coarea formula for Sobolev functions as in the proof of Proposition 5.1 and then the integral identity . Thus we proceed by writing
[TABLE]
Therefore it follows from basic considerations that
[TABLE]
and so rearranging gives the desired inequality (7.28), namely,
[TABLE]
Next we proceed by writing
[TABLE]
As it follows upon noting Proposition 7.4 that we have
[TABLE]
Hence by combining the above it follows that
[TABLE]
Therefore with the above at our disposal all that remains is to use the inequality
[TABLE]
whose proof proceeds similar to that of Proposition 5.1 by using the same angle of rotation function (5.10) in defining . This therefore completes the proof. ∎
8 Measure preserving self-maps and twists on solid tori
In this section we propose and study extensions of twist maps to a larger class of domains. Recalling that an -dimensions annulus takes the form the natural extension here would be domains of the product type (with , ) embedded in . Twist maps in turn will be suitable measure preserving self-maps of that agree with the identity map on the boundary (see [15, 17]). To keep the discussion tractable we confine ourselves here to the case . We proceed by first considering the solid torus embedded in as (see Fig. 1):
[TABLE]
Here and the fixed parameter is chosen to avoid self-intersection. Now let us set . Then above can be represented as
[TABLE]
From now on is the preferred choice of co-ordinates for where is unit ball in the plane. In polar co-ordinates we have , and upon noting we have as the co-ordinates of a sphere of radius :
[TABLE]
For our purposes in this section we shall write the above co-ordinate system in the following way,
[TABLE]
Now with the above notation in place we can define the desired twist maps on the solid torus as 666Note that the aim here is to seek non-trivial extremising twist maps for the energy functional over the admissible class of maps .,
[TABLE]
where the rotation matrix in takes the explicit form
[TABLE]
Here the function defines the angle of rotation as in the case for the annulus, however, in this case depends on the two variables and not just one as is the case for the annulus. There are two main reasons for this choice of representation of a twist map for , which we describe below.
- •
Firstly in order to be consistent with twist maps for the annulus we require that the rotation matrix is an isometry of the boundary
[TABLE]
with respect to the metric induced from its embedding in . (This is similar to what was done earlier in the case of an annulus). Then with this in mind the isometries of are matrices of the form,
[TABLE]
- •
Secondly we allow the angle of rotation function here to depend on the two variables instead of one to incorporate all the ”ball” variables in the product structure on . Note that collapses into in the annulus case as here one deals with an interval (a one dimensional ball).
Now in preparation for the upcoming calculations let us denote , and . Then it is easily seen that
[TABLE]
Note that the last equality results from the fact that the product is skew-symmetric and . Therefore using the above it is seen that the energy for a twist maps is given by
[TABLE]
Here we are using the fact that a change in the co-ordinates results in a Jacobian factor of in the integral, i.e.,
[TABLE]
Hence becomes,
[TABLE]
where here the additional absolute constant does not affect the variational structure of . Now to derive the Euler-Lagrange equation associated to the energy integral on the right it suffices to take variations of by some . This calculation leads to the following divergence form equation:
[TABLE]
Evidently the identity boundary condition on translates into for some fixed and all . Now suppose solves . Then by an application of the divergence theorem it is seen that the only solution to this boundary value problem is the trivial one, namely, for all . Indeed
[TABLE]
Now again as solves an application of the divergence theorem also gives
[TABLE]
Note that in obtaining the last identity we have used combined with the boundary condition satisfied by , namely, for . Hence
[TABLE]
Now since by assumption we have as and so . Hence gives and thus ; again by invoking the boundary condition on . It therefore follows that here we have no non-trivial solutions. Interestingly note that this conclusion stems from one crucial difference between the annulus and the solid torus in that has two boundary components whilst only has one. It was precisely this difference that turned crucial in the application of the divergence theorem.
Theorem 8.1**.**
There are no non-trivial twist solutions to the Euler-Lagrange equations associated with the energy functional on a solid torus .
9 Twist maps on tori with disconnected double component boundary
In contrast to what was seen above let us next move on to considering a ”thickened” torus, that is, the domain obtained topologically by taking the product of a two-dimensional torus and an interval. Note that here the boundary of the resulting domain consists of two disjoint copies of the initial torus and is in particular not connected. Now for definiteness and to fix notation let us set to be (see Fig. 1)
[TABLE]
Here are fixed and the aim is to seek non-trivial extremising twist maps for the energy functional over the admissible class of maps . Using the same co-ordinate system as in the earlier case we see that the are the co-ordinates of the two dimensional annulus centred at the origin. Additionally for similar reasons to that discussed earlier we define twist maps on as where the rotation matrix in is as (8.6).
A straightforward calculation shows that the energy of a twist maps is given by the integral
[TABLE]
Similar to what was described earlier in obtaining the second equality we have used the integral identity
[TABLE]
The Euler-Lagrange equation can be obtained in the standard way by taking variations where . This calculation again leads to the Euler-Lagrange equation given by (8.12) where we assume without loss of generality that the boundary condition on the rotation angle function is set to for and for with . Therefore solutions to (8.12) satisfy,
[TABLE]
Subsequently
[TABLE]
Hence taking into account the boundary conditions, e.g. on and on , we gain that if is a solution of then,
[TABLE]
Evidently with the stated boundary conditions has a unique solution. Indeed if are two solutions to with on and on then solves with on . Then by
[TABLE]
However in view of this gives and so invoking the boundary conditions , i.e., . As existence follows from standard arguments it follows that (8.12) has a unique smooth solution for each .
10 Euler-Lagrange analysis and twists as classical solutions
The goal of this section is to examine the solution to with the prescribed boundary conditions in relation to the Euler-Lagrange system (4.6) associated with on . To this end recall that the system takes the form
[TABLE]
For the ease of notation from now on we shall set . Hence using the identities we have
[TABLE]
Therefore from and a basic calculation we obtain
[TABLE]
Now since we have where the denotes the Laplacian with respect to the and variables we can rewrite this as
[TABLE]
Now upon recalling that the desired twist solution satisfies we have that
[TABLE]
Thus dividing both sides by and taking the negative terms to one side gives
[TABLE]
where and denotes the gradient with respect to the variable. Now since we obtain,
[TABLE]
and so as a result
[TABLE]
Next referring to the definition of basic calculation gives and , where
[TABLE]
Hence with the above notation the Euler-Lagrange associated with the twist , satisfying (8.12), simplifies to
[TABLE]
Considering the last line in the above equation it is plain that for to grant solution to the Euler-Lagrange equation it must be that
[TABLE]
or equivalently that the second term on the left is a gradient. But for this to be the case the latter term must necessarily be curl-free and so this leads to the system of equations
[TABLE]
It can be easily verified that equation is satisfied for any twist map since here we have
[TABLE]
We point out that the last line results upon noting the relations
[TABLE]
Using this we can again see that we can write and as a single equation in the following way,
[TABLE]
Therefore it is apparent that and become
[TABLE]
Now since we have the identities
[TABLE]
we obtain that simplifies further to
[TABLE]
Hence for a solution to with the prescribed boundary conditions to furnish a solution to the Euler-Lagrange system (4.6) associated with it is necessary for to satisfy
[TABLE]
We now show that (10.17) is also sufficient. Indeed assuming (10.17) the desired conclusion will follow upon showing that holds. Towards this end set to be the function,
[TABLE]
Then one can easily verify that,
[TABLE]
Furthermore using it is plain that
[TABLE]
As a result .
Theorem 10.1**.**
A twist map with the corresponding angle of rotation function satisfying and on , on with k\in{\mathbb{Z}}$$) is a solution to the Euler-Lagrange system associated with on iff it satisfies .
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