Spatial dynamics methods for solitary waves on a ferrofluid jet
Mark Groves, Dag Nilsson

TL;DR
This paper develops a mathematical framework to prove the existence of axisymmetric solitary waves on a ferrofluid jet influenced by magnetic fields, using Hamiltonian systems and dynamical systems techniques.
Contribution
It introduces a novel application of center-manifold reduction and dynamical systems methods to analyze solitary waves in ferrofluid jets with nonlinear magnetization laws.
Findings
Existence of solitary wave solutions is established.
A reduction to finite-dimensional Hamiltonian systems is achieved.
Homoclinic solutions corresponding to solitary waves are identified.
Abstract
This paper presents existence theories for several families of axisymmetric solitary waves on the surface of an otherwise cylindrical ferrofluid jet surrounding a stationary metal rod. The ferrofluid, which is governed by a general (nonlinear) magnetisation law, is subject to an azimuthal magnetic field generated by an electric current flowing along the rod. The ferrohydrodynamic problem for axisymmetric travelling waves is formulated as an infinite-dimensional Hamiltonian system in which the axial direction is the time-like variable. A centre-manifold reduction technique is employed to reduce the system to a locally equivalent Hamiltonian system with a finite number of degrees of freedom, and homoclinic solutions to the reduced system, which correspond to solitary waves, are detected by dynamical-systems methods.
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Spatial dynamics methods for solitary waves
on a ferrofluid jet
M. D. Groves Fachrichtung 6.1 - Mathematik, Universität des Saarlandes, Postfach 151150, 66041 Saarbrücken, Germany; Department of Mathematical Sciences, Loughborough University, Loughborough, LE11 3TU, UK
D. V. Nilsson111Centre for Mathematical Sciences, Lund University, PO Box 118, 22100 Lund, Sweden
Abstract
This paper presents existence theories for several families of axisymmetric solitary waves on the surface of an otherwise cylindrical ferrofluid jet surrounding a stationary metal rod. The ferrofluid, which is governed by a general (nonlinear) magnetisation law, is subject to an azimuthal magnetic field generated by an electric current flowing along the rod.
The ferrohydrodynamic problem for axisymmetric travelling waves is formulated as an infinite-dimensional Hamiltonian system in which the axial direction is the time-like variable. A centre-manifold reduction technique is employed to reduce the system to a locally equivalent Hamiltonian system with a finite number of degrees of freedom, and homoclinic solutions to the reduced system, which correspond to solitary waves, are detected by dynamical-systems methods.
1 Introduction
We consider an incompressible, inviscid ferrofluid of unit density in the region
[TABLE]
bounded by the free interface and a current-carrying wire at , where are cylindrical polar coordinates. The fluid is subject to a static magnetic field and the surrounding region
[TABLE]
is a vacuum (see Figure 1). Travelling waves move in the axial direction with constant speed and without change of shape, so that . We are interested in particular in axisymmetric solitary waves for which does not depend upon and as . Waves of this kind for ferrofluids with a linear magnetisation law have been investigated using a weakly nonlinear approximation by Rannacher & Engel [18], experimentally by Bourdin, Bacri & Falcon [4] and numerically by Blyth & Parau [3]. In this paper we present a rigorous existence theory for small-amplitude solitary waves and consider fluids with a general (nonlinear) magnetisation law.
Our starting point is a formulation of the hydrodynamic problem as a reversible Hamiltonian system
[TABLE]
in which the axial coordinate plays the role of time, is a variable related to the fluid velocity potential and , are the momenta associated with the coordinates , . The spatial Hamiltonian system (1.1) is derived from a variational principle for the governing equations in Section 3; it depends upon two dimensionless physical parameters and (see equation (2.6) for precise definitions) and the (dimensionless) magnitude of the magnetic intensity corresponding to the magnetic field in the ferrofluid.
Homoclinic solutions of (1.1) (solutions with as ) are of particular interest since they correspond to solitary waves. We detect such solutions using a technique known as the Kirchgässner reduction (Section 4), in which a centre-manifold reduction principle is used to show that all small, globally bounded solutions of a spatial (Hamiltonian) evolutionary system solve a (Hamiltonian) system of ordinary differential equations, whose solution set can in principle be determined. In this fashion we reduce (1.1) to a Hamiltonian system with finitely many degrees of freedom which can be treated by well-developed dynamical-systems methods, in particular normal-form theory. We proceed by perturbing the physical parameters , around fixed reference values , and thus introducing bifurcation parameters , . The Kirchgässner reduction delivers an -dependent reduced system which captures the small-amplitude dynamics for small values of these parameters; its dimension is the number of purely imaginary eigenvalues of the corresponding linearised system at . The reduction procedure is therefore especially helpful in detecting bifurcations which are associated with a change in the number of purely imaginary eigenvalues.
Working in the parameter plane, where , one finds that there are three critical curves , , at which the number of purely imaginary eigenvalues changes (see Figure 2(a)), together with a fourth curve at which the number of real eigenvalues changes. (In fact , and explicit formulae for and are given in Section 4.) A similar diagram arises in the study of gravity-capillary travelling water waves (see Iooss [14], Groves & Wahlén [13] and the references therein), and there the curves corresponding to , and are associated with homoclinic bifurcation: homoclinic solutions of the reduced Hamiltonian system (corresponding to solitary water waves) bifurcate from the trivial solution. Figure 2(a) illustrates the parameter regions I, II and III adjacent to , and in which the existence of homoclinic solutions is to be expected. In Section 5 we study these regions using the Kirchgässner reduction; the basic types of solitary wave found there are sketched in Figures 2(b)–(d).
In Section 5.1 we examine region I, choosing , so that , and writing with . According to the Kirchgässner reduction small-amplitude solitary waves are given by
[TABLE]
where is a homoclinic solution of the reversible Hamiltonian system
[TABLE]
with . This system admits a homoclinic solution which corresponds to a monotonically decaying, symmetric solitary wave of elevation for and depression for . For close to the critical value we write with and find that small-amplitude solitary waves are given by
[TABLE]
where is a homoclinic solution of the reversible Hamiltonian system
[TABLE]
with . For this system admits a pair of homoclinic solutions which correspond to monotonically decaying, symmetric solitary waves; one is a wave of depression, the other a wave of elevation. Note that in the limit or the variable solves a travelling-wave version of the (generalised) Korteweg-de Vries equation.
In Section 5.2 we apply the Kirchgässner reduction in region II, finding that small-amplitude solitary waves are given by
[TABLE]
where is a homoclinic solution of the reversible Hamiltonian system
[TABLE]
with ; the parameters measure the distance from respectively the point and the curve . This system admits a homoclinic solution which corresponds to a solitary wave of elevation for and depression for ; the wave is symmetric with an oscillatory decaying tail. For close to the critical value we write with and find that small-amplitude solitary waves are given by
[TABLE]
where is a homoclinic solution of the reversible Hamiltonian system
[TABLE]
with . For this system admits a a pair of homoclinic solutions which correspond to symmetric solitary waves with oscillatory decaying tails; one is a wave of depression, the other a wave of elevation. Note that in the limit or the variable solves a travelling-wave version of the (generalised) Kawahara equation.
It is instructive to interpret the above results for two well-studied magnetic intensities.
(i) The linear magnetisation law
[TABLE]
In region I we find that for (solitary waves of depression) and for (solitary waves of elevation); furthermore , so that both types of waves exist for near . This region has also been studied by Rannacher & Engel [18] using a weakly nonlinear approximation. In terms of the magnetic Bond number (corresponding to ) they derived a Korteweg-de Vries equation equivalent to (1.2), (1.3) and found solitary waves of depression for (that is, ) and of elevation for (that is, ), in agreement with our results. (Continuing their weakly nonlinear analysis to the next order in this region would lead to a cubic Korteweg-de Vries equation equivalent to (1.4), (1.5) and the prediction of both types of waves for near ). In region II we find that (solitary waves of depression).
(ii) The Langevin magnetisation law
[TABLE]
where is a dimensionless parameter. In Region I we find that for and , (solitary waves of depression), while for , (solitary waves of elevation), where is the unique solution of the equation
[TABLE]
(so that ). Furthermore , so that both types of waves exist for near (with ). In region II we find that (solitary waves of depression).
In Section 5.3 we turn to region III. Introducing a bifurcation parameter so that positive values of correspond to points on the ‘complex’ side of , one obtains the reduced (reversible) Hamiltonian system
[TABLE]
[TABLE]
where is a real polynomial which satisfies ; it contains the terms of order , …, in the Taylor expansion of . The substitution , converts the ‘truncated normal form’ obtained by neglecting the remainder term into the system
[TABLE]
(which, as evidenced by the scaling , , is at leading order equivalent to the nonlinear Schrödinger equation). Supposing that the coefficients of certain terms in have the correct sign, one finds that the latter system admits a circle of homoclinic solutions, two of which are real. The corresponding pair of homoclinic solutions to the original ‘truncated normal form’ are reversible and persist when the remainder terms are reinstated (see Iooss & Pérouème [15]). They generate symmetric solitary waves which take the form of periodic wave trains modulated by exponentially decaying envelopes; one is a wave of depression, the other a wave of elevation.
Each of the basic types of solitary waves in regions II and III is the primary member of an infinite family of multipulse solitary waves which resemble multiple copies of the primary. These waves are generated by corresponding multipulse homoclinic solutions which make several large excursions away from the origin in their four-dimensional phase space. A more precise description of the multipulse waves, together with a discussion of the relevant existence theories (which are based on variational and dynamical-systems arguments) is given in Sections 5.2 and 5.3.
Although the techniques used in the present paper are generalisations of those developed for the water-wave problem (see Iooss [14], Groves & Wahlén [13] and the references therein), we employ different methods to compute the reduced Hamiltonian systems. The spatial Hamiltonian system (1.1) is invariant under the transformation , (‘variation of potential base-level’), and the quantity is conserved. In many hydrodynamic problems it is possible to eliminate a symmetry of this kind before applying the Kirchgässner reduction (see e.g. Groves, Lloyd & Stylianou [11, §3.1] for an example in stationary ferrofluids), but here we retain it. It is inherited by the reduced systems: one of the canonical coordinates is cyclic and its conjugate is conserved. According to the classical theory, the next step is to set the conserved variable to zero, solve the resulting decoupled system for the other variables and recover the cyclic variable by quadrature; the lower-order system is typically studied using a canonical change of variables which simplifies its Hamiltonian (a ‘normal-form’ transformation). In the present context it is convenient to use a normal-form transformation before lowering the order of the system since it can be ‘absorbed’ into the changes of variable associated with the Kirchgässner reduction; this procedure greatly simplifies our later calculations. We present a general result for this purpose (Theorem 4.4), whose proof is based upon the method given by Bridges & Mielke [5, Theorem 4.3] and which may also be helpful in other applications.
2 The ferrohydrodynamic problem
We consider an incompressible, inviscid ferrofluid of unit density in the region
[TABLE]
bounded by the free interface and a current-carrying wire at , where are cylindrical polar coordinates. The fluid is subject to a static magnetic field and the surrounding region
[TABLE]
is a vacuum (see Figure 1).
We denote the magnetic and induction fields in the fluid and vacuum by respectively and , , and suppose that the relationships between them are given by the identities
[TABLE]
where is the magnetic permeability of free space and is the (prescribed) magnetic intensity of the ferrofluid. We suppose that
[TABLE]
where is a (prescribed) nonnegative function, so that in particular and are collinear. According to Maxwell’s equations the magnetic and induction fields are respectively irrotational and solenoidal, and introducing magnetic potential functions , with ,, we therefore find that
[TABLE]
in which
[TABLE]
is the magnetic permeability of the ferrofluid relative to that of free space. We suppose that the ferrofluid flow is irrotational, so that its velocity field is the gradient of a scalar velocity potential . The Euler equation for the ferrofluid is given by
[TABLE]
(Rosensweig [19, §5.1]), where is its composite pressure, and the calculations
[TABLE]
show that this equation is equivalent to
[TABLE]
where is a constant.
Next we turn to the boundary conditions at . The magnetic boundary conditions are
[TABLE]
where and denote tangent and normal vectors to the free surface; it follows that
[TABLE]
The (hydro-)dynamical boundary condition is given by
[TABLE]
(Rosensweig [19, §5.2]), in which is the coefficient of surface tension and
[TABLE]
is the mean curvature of the interface; using (2.1), we find that
[TABLE]
where
[TABLE]
Finally, the (hydro-)kinematic boundary condition is
[TABLE]
that is
[TABLE]
The relevant conditions at and in the far field are , as , so that , as , and as , so that as .
The constant is selected so that
[TABLE]
(that is , , ) is a solution to the above equations (corresponding to a uniform magnetic field and a circular cylindrical jet with radius ); we therefore set . Seeking axisymmetric waves for which and are independent of , one finds that , so that the hydrodynamic problem decouples from the magnetic problem and is given by
[TABLE]
and
[TABLE]
for .
The next step is to seek travelling wave solutions for which and depend upon and only through the combination , and to introduce dimensionless variables
[TABLE]
and functions
[TABLE]
where
[TABLE]
(note that ). Dropping the hats for notational simplicity, we find that
[TABLE]
and
[TABLE]
for , where
[TABLE]
and
[TABLE]
are dimensionless parameters. Solitary waves are nontrivial solutions of (2.2)–(2.5) with , as . Finally, note that equations (2.2), (2.4) and (2.5) follow from the formal variational principle
[TABLE]
where the variations are taken with respect to and .
3 Spatial dynamics
3.1 Formulation as a spatial Hamiltonian system
The first step is to use the ‘flattening’ transformation
[TABLE]
to map the variable domain into a fixed strip and the free interface into . Dropping the hat for notational simplicity, we find that the corresponding ‘flattened’ variable
[TABLE]
satisfies the equations
[TABLE]
with boundary conditions
[TABLE]
and
[TABLE]
Observe that equations (3.1), (3.3) and (3.4) follow from the new variational principle , where
[TABLE]
and the variations are taken in and (the functional is obtained from the variational functional for (2.2), (2.4) and (2.5) by ‘flattening’).
We exploit this variational principle by regarding as an action functional of the form
[TABLE]
in which is the integrand on the right-hand side of equation (3.5), and deriving a canonical Hamiltonian formulation of (3.1)–(3.4) by means of the Legendre transform. To this end, let us introduce new variables and by the formulae
[TABLE]
and define the Hamiltonian function by
[TABLE]
in which
[TABLE]
Writing , where are fixed, and (since is the ‘trivial’ solution of Hamilton’s equations), we find that Hamilton’s equations are given explicitly by
[TABLE]
where the superscript denotes the dependence upon , with boundary condition
[TABLE]
the second of which arises from the integration by parts necessary to compute (3.10) Note that our equations are reversible, that is invariant under the transformation , where the reverser is defined by .
To make this construction rigorous we recall the differential-geometric definitions of a Hamiltonian system and Hamilton’s equations for its associated vector field.
Definition 3.1**.**
A Hamiltonian system consists of a triple , where is a manifold, is a closed, weakly nondegenerate bilinear form (the symplectic -form) and the Hamiltonian is a smooth function on a manifold domain of (that is, a manifold which is smoothly embedded in and has the property that is densely embedded in for each ).
Its Hamiltonian vector field with domain is defined as follows. The point belongs to with if and only if
[TABLE]
for all tangent vectors (by construction admits a unique extension ). Hamilton’s equations for are the differential equations
[TABLE]
which determine the trajectories of its Hamiltonian vector field.
Definition 3.1 applies to the above formulation. Note that the identity mapping is(up to the scaling factor ) an isometry , and , where is the unit ball in and denotes the closed subspace of consisting of axisymmetric functions (see Bernardi, Dauge & Maday [2, Theorem II.2.1]). We therefore let be a neighbourhood of the origin in
[TABLE]
and with
[TABLE]
so that elements satisfy (see Bernardi, Dauge & Maday [2, Remark II.1.1]). We consider values of in a neighbourhood of the origin in and choose and small enough so that
[TABLE]
The formula
[TABLE]
defines a weakly nondegenerate bilinear form and hence a constant symplectic -form (its closure follows from the fact that it is constant), and the function given by (3.6) belongs to , so that the triple is a Hamiltonian system. Applying the criterion in the definition, one finds that
[TABLE]
and that Hamilton’s equations are given explicitly by (3.7)–(3.10).
It remains to confirm the relationship between a solution to Hamilton’s equations for and a solution to the ‘flattened’ hydrodynamic problem (3.1)–(3.4). Suppose that is a smooth solution of Hamilton’s equations. An explicit calculation shows that the variables , given by , solve (3.1)–(3.4) (see Groves & Toland [12, pp. 212-214] for a discussion of this procedure in the context of water waves).
4 Centre-manifold reduction
Our strategy in finding solutions to Hamilton’s equations (3.7)–(3.10) for consists in applying a reduction principle which asserts that is locally equivalent to a finite-dimensional Hamiltonian system. The key result is the following theorem, which is a parametrised, Hamiltonian version of a reduction principle for quasilinear evolutionary equations presented by Mielke [17, Theorem 4.1] (see Buffoni, Groves & Toland [8, Theorem 4.1]).
Theorem 4.1**.**
Consider the differential equation
[TABLE]
which represents Hamilton’s equations for the reversible Hamiltonian system . Here belongs to a Hilbert space , is a parameter and is a densely defined, closed linear operator. Regarding as a Hilbert space equipped with the graph norm, suppose that [math] is an equilibrium point of (4.1) when and that
- (H1)
The part of the spectrum of which lies on the imaginary axis consists of a finite number of eigenvalues of finite multiplicity and is separated from the rest of in the sense of Kato, so that admits the decomposition , where , and is the spectral projection corresponding the purely imaginary part of . 2. (H2)
The operator satisfies the estimate
[TABLE]
for some constant that is independent of . 3. (H3)
There exists a natural number and neighbourhoods of [math] and of [math] such that is times continuously differentiable on , its derivatives are bounded and uniformly continuous on and , .
Under these hypotheses there exist neighbourhoods of [math] and , of [math] and a reduction function with the following properties. The reduction function is times continuously differentiable on , its derivatives are bounded and uniformly continuous on and , . The graph is a Hamiltonian centre manifold for (4.1), so that
- (i)
* is a locally invariant manifold of (4.1): through every point in there passes a unique solution of (4.1) that remains on as long as it remains in .*
- (ii)
Every small bounded solution , of (4.1) that satisfies lies completely in .
- (iii)
Every solution of the reduced equation
[TABLE]
generates a solution
[TABLE]
of the full equation (4.1).
- (iv)
* is a symplectic submanifold of and the flow determined by the Hamiltonian system , where the tilde denotes restriction to , coincides with the flow on determined by . The reduced equation (4.2) is reversible and represents Hamilton’s equations for .*
Mielke’s theorem cannot be applied directly to (3.7)–(3.10) because of the nonlinear boundary condition (3.11) in the domain of the Hamiltonian vector field (the right-hand sides of (3.7)–(3.10) define a smooth mapping with for any ). We overcome this difficulty using the change of variable , where
[TABLE]
which transforms the boundary condition in into
[TABLE]
Lemma 4.2**.**
For each the mapping is a smooth diffeomorphism from the neighbourhood of the origin in onto a neighbourhood of the origin in , and from onto . The diffeomorphisms and their inverses depend smoothly upon .
Proof. These results follow from the explicit formulae (4.4) and
[TABLE]
where
[TABLE]
for and its inverse .∎
A simple calculation shows that the diffeomorphism transforms
[TABLE]
into
[TABLE]
where is the smooth vector field defined by
[TABLE]
Formula (4.5) represents Hamilton’s equations for the Hamiltonian system , where
[TABLE]
and
[TABLE]
The domain of the Hamiltonian vector field is
[TABLE]
and for any .
The next step is to verify that (4.5) satisfies the hypotheses of Theorem 4.1 (with ), so that we obtain a finite-dimensional reduced Hamiltonian system . We write (4.5) as
[TABLE]
in which and verify the spectral hypotheses on by considering the operator , where
[TABLE]
and
[TABLE]
(the formal linearisation of at the origin); the formula shows that the spectral properties of and are identical. It follows from Lemma 4.3 below that satisfies hypotheses (H1) and (H2); hypothesis (H3) is clearly satisfied for an arbitrary value of . Part (i) of Lemma 4.3 is proved using the elementary theory of ordinary differential equations, while part (ii) is established using arguments similar to those employed for other problems treated using centre-manifold reduction (e.g. see Buffoni, Groves & Toland [8, Proposition 3.2] or Groves & Wahlén [13, Lemma 3.4]).
Lemma 4.3**.**
- (i)
The spectrum of consists entirely of isolated eigenvalues of finite algebraic multiplicity. A complex number is an eigenvalue of if and only if
[TABLE]
where . (In particular, [math] is an eigenvalue of and is a finite set.)
- (ii)
There exist real constants , such that
[TABLE]
for each real number with .
According to Lemma 4.3(i), a purely imaginary number is an eigenvalue of if and only if
[TABLE]
Straightforward computations show that there are three critical curves
[TABLE]
and
[TABLE]
in the parameter plane at which purely imaginary eigenvalues of collide, together with a fourth curve
[TABLE]
at which real eigenvalues collide (see Figure 3). Here , , …and , , …denote respectively the Bessel functions and modified Bessel functions of the first kind, and is the smallest zero of . Furthermore, has a geometrically simple zero eigenvalue whose algebraic multiplicity is two for , four for , and and six for .
The centre manifold is equipped with the single coordinate chart and coordinate map defined by . It is however more convenient to use an alternative coordinate map for calculations. We define the function with (which in general has components in and ) by the formula
[TABLE]
where , , and equip with the coordinate map given by , so that
[TABLE]
as . Furthermore, using a parameter-dependent version of Darboux’s theorem (e.g. see Buffoni & Groves [7, Theorem 4]), we may assume that the remainder term in (4.8) vanishes identically.
We proceed by choosing a symplectic basis for the centre subspace of (so that for and the symplectic product of any other combination of these vectors is zero); here either or is the eigenvector corresponding to the zero eigenvalue of . Using coordinates , …, , , …, , where
[TABLE]
we find that is the canonical -form. Note that equations (3.7)–(3.11) are invariant under the transformation , , and the quantity is conserved. This symmetry is inherited by the reduced system: one of the variables , is cyclic (that is, and do not depend upon it), so that the other is conserved.
According to the classical theory, the next step is to lower the dimension of the reduced system by two by setting the conserved variable to zero, solving the resulting decoupled system for , …, , , …, and recovering the cyclic variable by quadrature; the lower-order system is typically studied using a canonical change of variables which simplifies its Hamiltonian (a ‘normal-form’ transformation). For our purposes it is convenient to use a normal-form transformation before lowering the order of the system since it can be ‘absorbed’ into in the same way as the Darboux transformation; this procedure greatly simplifies our later calculations. The following general result (whose proof is based upon the method given by Bridges & Mielke [5, Theorem 4.3]) shows that this procedure is possible; we assume for definiteness that is cyclic and use the construction by Elphick [10] as our ‘usual’ normal form. The result is applied to the specific parameter regimes shown in Figure 2(a) in Section 5 below, where we denote the nonlinear part of the reduced Hamiltonian vector field by .
Theorem 4.4**.**
Consider the -degree-of-freedom Hamiltonian system
[TABLE]
where and is cyclic (so that is conserved).
There exists a near-identity canonical change of variables with the properties that is cyclic, and the lower-order Hamiltonian system
[TABLE]
adopts its usual normal form. (Here, with a slight abuse of notation, we denote the transformed Hamiltonian by .)
Proof. Consider the -degree of freedom Hamiltonian system
[TABLE]
in which and are parameters. The standard theory asserts the existence of a canonical change of variables
[TABLE]
with
[TABLE]
which converts (4.11) into its parameter-dependent normal form; note that
[TABLE]
where
[TABLE]
and this condition may also be written as
[TABLE]
We seek a change of variable for (4.9), (4.10) of the form
[TABLE]
the new function
[TABLE]
is subject to the requirement that
[TABLE]
where
[TABLE]
and this condition may be written as
[TABLE]
It is possible to find satisfying these conditions since the compatibility condition for (4.14), (4.15) is the derivative of (4.13) with respect to , and (4.13) is automatically satisfied because of (4.12).∎
5 The reduced Hamiltonian systems
5.1 Homoclinic bifurcation at
At each point of the curve in Figure 3 two real eigenvalues become purely imaginary by colliding at the origin and increasing the algebraic multiplicity of the zero eigenvalue from two to four. This resonance is associated with the bifurcation of a branch of homoclinic solutions into the region with real eigenvalues (the parameter regime marked I in Figure 2. Let us therefore fix reference values , so that , , and introduce a bifurcation parameter by choosing , where .
The four-dimensional centre subspace of is spanned by the generalised eigenvectors
[TABLE]
where has been chosen so that , for ,
[TABLE]
and the symplectic product of any other combination of the vectors , … is zero. Writing
[TABLE]
we therefore find that , , and are canonical coordinates for the reduced Hamiltonian system, which has the cyclic variable and reverser ; with a slight abuse of notation we abbreviate to .
The usual normal-form theory for the two-dimensional system with Hamiltonian asserts that, after a canonical change of variables,
[TABLE]
where is a polynomial of order in with
[TABLE]
It follows that, after a canonical change of variables,
[TABLE]
with
[TABLE]
here is a polynomial of order with
[TABLE]
and , and is an affine function of its first argument which satisfies
[TABLE]
Note that
[TABLE]
Writing
[TABLE]
where denotes the part of the Taylor expansion of which is homogeneous of order in and in , one finds that
[TABLE]
(see Appendix (i)). Setting and introducing scaled variables
[TABLE]
yields
[TABLE]
where
[TABLE]
and the lower-order Hamiltonian system
[TABLE]
which is reversible with reverser . Suppose . In the limit equations (5.1), (5.2) are equivalent to the single equation
[TABLE]
for the variable .
Let us now suppose that is close to the critical value and introduce a second bifurcation parameter by setting
[TABLE]
and observing that
[TABLE]
(with a slight change of notation). Writing
[TABLE]
where denotes the part of the Taylor expansion of which is homogeneous of order in , in and in , one finds that
[TABLE]
(see Appendix (ii)). Setting , introducing scaled variables
[TABLE]
and writing
[TABLE]
thus yields
[TABLE]
where
[TABLE]
and the lower-order Hamiltonian system
[TABLE]
which is of course reversible with reverser . Suppose that . In the limit equations (5.3), (5.4) are equivalent to the single equation
[TABLE]
for the variable .
The phase portrait of the equation
[TABLE]
for a fixed natural number (which is a travelling-wave version of the generalised Korteweg-de Vries equation) is readily obtained by elementary calculations and is sketched in Figure 5; the homoclinic orbits are of particular interest.
Lemma 5.1**.**
**
- (i)
Suppose that is even. Equation (5.5) has precisely one homoclinic solution (up to translations). This solution is positive and symmetric, and monotone increasing to the left, monotone decreasing to the right of its point of symmetry.
- (ii)
Suppose that is odd. Equation (5.5) has precisely two homoclinic solutions , where is symmetric, and monotone increasing to the left, monotone decreasing to the right of its point of symmetry.
In both cases the homoclinic solutions intersect the symmetric section in the two-dimensional phase space transversally.
A familiar argument shows that Lemma 5.1(i) also applies to (5.1), (5.2) for small, positive values of , while Lemma 5.1(ii) applies to (5.3), (5.4) for small, positive values of and small, values of (that is, small values of ); the qualitative statements apply to the variable or . The homoclinic orbits at (and ) intersect the symmetric section transversally, and these orbits therefore persist (as small, uniform perturbations of their limits) for small, positive values of (and small values of ).
Altogether we have established the existence of a symmetric, monotonically decaying solitary wave of depression for and elevation for ; the corresponding ferrofluid surface is obtained from the homoclinic solution of (5.1), (5.2) by the formula
[TABLE]
Furthermore, a pair of symmetric, monotonically decaying solitary waves exists for small values of provided that ; one is a wave of depression, the other a wave of elevation. The corresponding ferrofluid surface is obtained from a homoclinic solution of (5.3), (5.4) by the formula
[TABLE]
(A more detailed analysis of a codimension-two bifurcation of this kind was given by Kirrmann [16, §4] in the context of two-layer fluid flow.) Figure 5 shows a sketch of the ferrofluid surface corresponding to solitary waves of the present type.
5.2 Homoclinic bifurcation at
At each point of the curve in Figure 3 two pairs of real eigenvalues become complex by colliding at non-zero points on the real axis. Of particular interest here is the local part of near the point (which is given by , for ) since we can access this curve using the centre-manifold technique. To this end we choose , and
[TABLE]
Notice that indicates the distance in parameter space from the point , while plays the role of a bifurcation parameter (varying through zero from above we cross the critical curve from above); the parameter regime marked II in Figure 2 corresponds to small, positive values of and .
The six-dimensional centre subspace of is spanned by the generalised eigenvectors
[TABLE]
[TABLE]
where , for ,
[TABLE]
and the symplectic product of any other combination of the vectors , … is zero. Writing
[TABLE]
we therefore find that , , , , and are canonical coordinates for the reduced Hamiltonian system, which has the cyclic variable and reverser S:(q_{0},q_{1},q_{2},p_{0},p_{1},p_{2})\mapsto$$(-q_{0},-q_{1},-q_{2},p_{0},p_{1},p_{2}); with a slight abuse of notation we abbreviate to .
The usual normal-form theory for the four-dimensional system with Hamiltonian , where , asserts that, after a canonical change of variables,
[TABLE]
where is a polynomial of order which depends upon , , , through the combinations
[TABLE]
and satisfies
[TABLE]
It follows that, after a canonical change of variables,
[TABLE]
with
[TABLE]
here is a polynomial of order which depends upon , , , through the above combinations and satisfies
[TABLE]
and , and is an affine function of its first two arguments which satisfies
[TABLE]
Note that
[TABLE]
Writing
[TABLE]
where denotes the part of the Taylor expansion of which is homogeneous of order in , in and in , one finds that
[TABLE]
(see Appendix (iii)). Setting , choosing , according to (5.6) and introducing the scaled variables
[TABLE]
thus yields
[TABLE]
and the lower-order Hamiltonian system
[TABLE]
which is reversible with reverser . Suppose . In the limit equations (5.7)–(5.10) are equivalent to the single fourth-order ordinary differential equation
[TABLE]
for the variable .
Let us now suppose that is close to the critical value and introduce a further bifurcation parameter by setting
[TABLE]
and observing that
[TABLE]
(with a slight change of notation). Writing
[TABLE]
where denotes the part of the Taylor expansion of which is homogeneous of order in , in , in and in , one finds that
[TABLE]
(see Appendix (iv)). Setting , choosing , according to (5.6), introducing the scaled variables
[TABLE]
and writing
[TABLE]
thus yields
[TABLE]
and the lower-order Hamiltonian system
[TABLE]
which is of course reversible with reverser . Suppose . In the limit equations (5.11)–(5.14) are equivalent to the single fourth-order ordinary differential equation
[TABLE]
for the variable .
Existence theories for homoclinic solutions to the equation
[TABLE]
for a fixed natural number (which is a travelling-wave version of the generalised Kawahara equation) are given in Theorems 5.2 and 5.3 below. These theorems are generalisations of results given by Buffoni, Champneys & Toland [6] (see also Devaney [9]) for the special case ; a full discussion of their generalisation to is given by Ahmad [1].
Theorem 5.2**.**
Suppose that .
- (i)
Suppose that is even. Equation (5.15) has precisely one homoclinic solution (up to translations). This solution is positive and symmetric, and monotone increasing to the left, monotone decreasing to the right of its point of symmetry.
- (ii)
Suppose that is odd. Equation (5.15) has precisely two homoclinic solutions , where is symmetric, and monotone increasing to the left, monotone decreasing to the right of its point of symmetry.
In both cases the homoclinic solutions are transverse, that is, the stable and unstable manifolds of the zero equilibrium intersect transversally with respect to the zero level surface of the Hamiltonian at their point of symmetry.
Theorem 5.3**.**
The primary homoclinic solutions found in the previous theorem persist (as small, uniform perturbations of their limits at ) for small, negative values of .
Furthermore, each primary homoclinic solution in the region generates a family of transverse multipulse homoclinic solutions which resemble multiple copies of ‘glued’ together with small oscillations in between. More precisely, for each all natural numbers with there exists a homoclinic solution associated with which
- (i)
has local extrema at , …, ,
- (ii)
oscillates times and has extrema in each interval ,
- (iii)
oscillates infinitely often in the intervals and .
Theorem 5.2(i) also applies to (5.7)–(5.10) for small, positive values of , while Theorem 5.2(ii) applies to (5.11)–(5.14) for small, positive values of and small, values of (that is, small values of ); the qualitative statements apply to the variable or . The homoclinic orbits at (and ) are transverse and therefore persist (as small, uniform perturbations of their limits) for small, positive values of (and small values of ). Similarly, Theorem 5.3 applies to any of these persistent primary homoclinic orbits.
Altogether we have established the existence of a primary and accompanying multipulse family of solitary waves of depression for and elevation for ; the corresponding ferrofluid surface is obtained from the homoclinic solution of (5.1), (5.2) by the formula
[TABLE]
Furthermore, two multipulse families of solitary waves exist for small values of provided that ; one consists of waves of depression, the other of waves of elevation. The corresponding ferrofluid surface is obtained from a homoclinic solution of (5.3), (5.4) by the formula
[TABLE]
5.3 Homoclinic bifurcation at
At each point of the curve in Figure 3 two pairs of purely imaginary eigenvalues become complex by colliding at non-zero points on the imaginary axis and forming two Jordan chains of length 2. This resonance is associated with the bifurcation of a branch of homoclinic solutions into the region with complex eigenvalues (the parameter regime marked III in Figure 2). Let us therefore choose
[TABLE]
(so that and introduce a bifurcation parameter by writing , where .
The six-dimensional centre subspace of is spanned by the generalised eigenvectors
[TABLE]
where
[TABLE]
and
[TABLE]
note that , , , ,
[TABLE]
and the symplectic product of any other combination of the vectors , , , , is zero. Writing
[TABLE]
where
[TABLE]
we therefore find that , , and are canonical coordinates for the reduced Hamiltonian system, which has the cyclic variable and reverser ; with a slight abuse of notation we abbreviate to .
The usual normal-form theory for the two-dimensional system with Hamiltonian asserts that, after a canonical change of variables,
[TABLE]
where is a real polynomial function of its arguments which satisfies
[TABLE]
It follows that, after a canonical change of variables,
[TABLE]
with
[TABLE]
here is a real polynomial function of its arguments which satisfies
[TABLE]
and , and is an affine function of its first four arguments which satisfies
[TABLE]
Note that
[TABLE]
Writing
[TABLE]
where denotes the part of the Taylor expansion of which is homogeneous of order in and in , one finds that
[TABLE]
where
[TABLE]
(see Appendix (v)).
The lower-order Hamiltonian system
[TABLE]
has been examined in detail by Iooss & Pérouème [15]. The ‘truncated normal form’ obtained by ignoring the remainder terms in is conveniently handled using the substitution , , which converts it into the system
[TABLE]
Supposing that the coefficients and are respectively negative and positive, one finds that (5.19), (5.20) admits a real, reversible homoclinic solution , which evidently generates a circle of further homoclinic solutions, two of which (those with and ) are reversible. The corresponding pair of homoclinic solutions to the original ‘truncated normal form’ are reversible and persist when the remainder terms are reinstated. A theory of multipulse homoclinic solutions to (5.17), (5.18) has also been given by Buffoni & Groves [7] (under the same hypotheses on the normal-form coefficients).
Theorem 5.4**.**
**
- (i)
(Iooss & Pérouème) For each sufficiently small, positive value of the two-degree-of-freedom Hamiltonian system (5.17), (5.18) has two distinct symmetric homoclinic solutions.
- (ii)
(Buffoni & Groves) For each sufficiently small, positive value of the two-degree-of-freedom Hamiltonian system (5.17), (5.18) has an infinite number of geometrically distinct homoclinic solutions which generically resemble multiple copies of one of the homoclinic solutions in part (i).
The homoclinic solutions identified above correspond to envelope solitary waves whose amplitude is and which decay exponentially as ; they are sketched in Figure 8.
Appendix: Calculation of the normal-form coefficients
The coefficients in the reduced Hamiltonian are determined using the equations
[TABLE]
to compute the Taylor series of and systematically in powers of or . Here and are the linear and nonlinear parts of (with this slight abuse of notation is given by the explicit formula (4.6)), and , are the linear and nonlinear parts of the boundary-value operator defined by the left-hand side of (3.11). Throughout these calculations we also make use of the identity
[TABLE]
in which . We denote the parts of , , which are homogeneous of order in and in by , , , and the part of which is homogeneous of order in and in by ; the notation is modified in the natural fashion when is replaced by a more specific parameterisation. Finally, arbitrary constants arising from solving differential equations are denoted by .
Homoclinic bifurcation at
(i) Write
[TABLE]
and consider the and components of (A.1), (A.2), namely
[TABLE]
Using these equations we find that
[TABLE]
which implies that
[TABLE]
and
[TABLE]
which implies that
[TABLE]
(ii) Write
[TABLE]
and consider the component of (A.1), (A.2), namely
[TABLE]
The coefficient can be expressed as
[TABLE]
where
[TABLE]
and we find from the boundary condition in (A.4) that the sum inside the parentheses vanishes. From (A.3) we find that
[TABLE]
and it follows from (A.5) that
[TABLE]
Homoclinic bifurcation at
(iii) Write
[TABLE]
and consider the , and components of (A.1), (A.2), namely
[TABLE]
Using the method described in part (i) above, we find from these equations that
[TABLE]
Combining
[TABLE]
with
[TABLE]
which is obtained from (A.7), one finds by the usual argument that
[TABLE]
Similarly, combining
[TABLE]
with
[TABLE]
which is obtained from (A.8), yields
[TABLE]
so that .
(iv) Write
[TABLE]
and note that
[TABLE]
Since
[TABLE]
where we have used
[TABLE]
it follows that
[TABLE]
In order to compute it is therefore necessary to compute and .
From (A.6) one finds that
[TABLE]
and
[TABLE]
yields
[TABLE]
Furthermore,
[TABLE]
and
[TABLE]
yield
[TABLE]
and using these results we find that the solvability condition for
[TABLE]
is . Inserting these expressions for and into (A.10), we obtain
[TABLE]
Homoclinic bifurcation at
(v) Here we write
[TABLE]
The coefficient is found from
[TABLE]
Noting that
[TABLE]
we find from (A.11) that
[TABLE]
Finally, to compute we consider
[TABLE]
Taking the symplectic product with and simplifying in the usual fashion, we find that
[TABLE]
where and are obtained from
[TABLE]
and
[TABLE]
where
[TABLE]
because of
[TABLE]
(note that is determined up to addition of ). Altogether (A.12) shows that
[TABLE]
and the result of this calculation is given in equation (5.16).
The reference list from the paper itself. Each links out to its DOI / PubMed record.
- 1[1] Ahmad, R. 2016 Homokline Lösungen zu einer Modellgleichung für Wasserwellen . Bachelor thesis: Universität des Saarlandes.
- 2[2] Bernardi, C., Dauge, M. & Maday, Y. 1999 Spectral methods for axisymmetric domains . Series in Applied Mathematics. Paris, Amsterdam: Gauthier-Villars, North Holland.
- 3[3] Blyth, M. & Parau, E. 2014 Solitary waves on a ferrofluid jet. J. Fluid Mech. 750 , 401–420.
- 4[4] Bourdin, E., Bacri, J.-C. & Falcon, E. 2010 Observation of axisymmetric solitary waves on the surface of a ferrofluid. Phys. Rev. Lett. 104 , 094502.
- 5[5] Bridges, T. J. & Mielke, A. 1995 A proof of the Benjamin-Feir instability. Arch. Rat. Mech. Anal. 133 , 145–198.
- 6[6] Buffoni, B., Champneys, A. R. & Toland, J. F. 1996 Bifurcation and coalescence of a plethora of homoclinic orbits for a Hamiltonian system. J. Dyn. Diff. Eqns. 8 , 221–279.
- 7[7] Buffoni, B. & Groves, M. D. 1999 A multiplicity result for solitary gravity-capillary waves in deep water via critical-point theory. Arch. Rat. Mech. Anal. 146 , 183–220.
- 8[8] Buffoni, B., Groves, M. D. & Toland, J. F. 1996 A plethora of solitary gravity-capillary water waves with nearly critical Bond and Froude numbers. Phil. Trans. Roy. Soc. Lond. A 354 , 575–607.
