An Initial-Boundary Value Problem for a Modified Transitional Korteweg-de Vries Equation ()
1. Introduction
The Korteweg-de Vries equation (KdV) equation below
(1.1)
is a famous equation in mathematical physics. It was derived as a model for undirectional propagation of small-amplitude long waves in a number of physical systems, such as the evolution of shallow water waves, ion acoustic waves, long waves in shear flows [1]-[5]. The KdV equation is a soliton equation with Hamiltonian structures and an infinitely number of independent motion constants in involution [6]-[8]. The existence of a unique global solution and well-posedness for the KdV equation with smooth initial data can be found in [9]-[14].
The Korteweg-de Vries equation (KdV) equation has a cousin, namely the modified KdV equation (mKdV)
(1.2)
also has been a subject of prolific study [15]-[23]. This equation has infinitely many conserved quantities. The famous Miura transformation establishes the connection between KdV and mKdV equations: namely, a solution of the mKdV equation
yields a solution of the KdV equation
. For the Cauchy problem of the mKdV Equation (1.2), there exists a unique global classical solution. For the following generalized mKdV equation
(1.3)
where
is a positive integer, it is found to be integrable only in two cases:
(KdV) and
(mKdV) [24].
We notice that most of these studies are focused on pure initial value problems. However, in many cases of physical interest, the mathematical model leads precisely to a mixed initial-boundary value problem. For example, the KdV equation can describe long waves. In order to assess the performance of the KdV equation as a model for waves in a particular system, sometimes it is not quite convenient to consider the pure initial value problem since there may be difficulty associated with determing the entire wave profile accurately at a given time. One way to obtain undirectional waves to test the appurtenance of KdV, is to generate waves at one end of a homogeneous stretch of the medium in question and to allow them to propagate into the initial undisturbed medium beyond the wavemaker (see [25]-[27] for details). This leads to the following inhomogeneous initial-boundary value problem in which global existence and well-posedness were established [28] [29]:
(1.4)
Meanwhile, for the famous n-dimensional nonlinear Schrödinger equation (NLS) (
)
(1.5)
under initial and inhomogeneous boundary conditions
,
(with compact support), there exists a global solution
for
[30]. The PDE is understood in the sense of distribution while the boundary condition is understood as
for a.e.
. Furthermore, if
, this solution is unique.
Another example is the following initial and inhomogeneous boundary value problem for an n-dimensional Ginzburg-Landau equation which describes nonlinear amplitude evolution of wave propagation:
(1.6)
where
and
are smooth functions. If
,
,
,
(compatibility condition), then (1.6) has an unique global solution in
, for some
,
, for a.e.
[31].
For the following initial and inhomogeneous boundary value problem of a modified KdV:
(1.7)
where
is an even integer,
. The existence of a unique global classical solution
is proved in [32] provided that
,
.
As we know, transitional KdV equation arises in the study of long solitary waves in lakes and estuaries. It propagates on the thermocline separating two layers of fluids of almost equal densities (see [33] for example). Global well-posedness for the Cauchy problem of the following transitional KdV equation was obtained in [34]:
(1.8)
where
,
,
.
This research is the continuation of an earlier paper [35] about the following modified transitional KdV equation posed in the quarter plane (
):
(1.9)
We proved a unique global classical solution
for (1.9) under the conditions either (i)
,
or (ii)
where
.
In this paper, we will study a more generalized version of modified transitional KdV equation under initial and inhomogeneous boundary conditions
(1.10)
where
is an even integer. We prove the global existence and uniqueness theorem under similar conditions.
2. Local and Global Existence-Uniqueness Theorems
We first define
and subsitute this in (1.10) to get
(2.1)
where
,
. Let
be a subspace of
with standard Sobolev norm, then (2.1) is converted to a quasi-linear equation of evolution
(2.2)
where
(2.3)
Let
,
,
,
, then
is continuously and densely embedded in
with usual norms. Since
where
, the leading term
in
is the generator of a contraction semi-group in
, skew-adjoint with
. The perturbing term
is quasi-accretive and relatively bounded with respect to
. We consider the solution for (2.2) on any time interval
. Since
as
,
is a first-order differential operator with a smooth coefficient
. We have the following estimate
(2.4)
provided that
,
and
. Since
and
are locally bounded functions, we see that
is
-Lipschitz continuous for each
. Similar to the results on abstract quasi-linear equation of evolution in [36] [37], we have the following existence theorem.
Theorem 2.1. (Local Existence and Uniqueness) For the modified transitional Korteweg-de Vries Equation (2.2) posed in the quarter plane, there exists a unique classical solution
for some
if
. Thus there is a unique local classical solution
for (1.10) with inhomogeneous boundary data provided that
,
and
.
To prove global existence, we need to estimate the
norm for any solution
and show it’s bounded on any finite interval
. Write
,
,
. Differentiate both
and
with respect to
variable and substitute them in (1.10) to get
(2.5)
(2.6)
Now we differentiate
with respect to
variable to get
(2.7)
By adding (2.5)-(2.7) we obtain:
(2.8)
To prove global existence, we need to show that
is bounded on any
. First we consider the case (i)
. From (2.8) we see that for any
(2.9)
for some positive number
which depends on
and
which in turn depend on
and
. By integrating (2.9) in
variable and noting that
we obtain
(2.10)
which implies that
is bounded on any
.
Next we turn to case (ii)
where
with no restriction on
. Again, from (2.8) we get
(2.11)
for some positive
depending on
and
which in turn depend on
and
. By integrating (2.11) in
variable and noting that
we obtain
(2.12)
for some positive number
which depends on
and
. By Gronwall’s
lemma,
is bounded on any
, so is
. From
Gagliardo-Nirenburg estimate [38], we see that
for some
, therefore
is bounded on any
.
Now consider the Cauchy problem for the linear equation
(2.13)
in a Banach space
and if one assumes that
generates an analytical semigroup then the solution of (1.10) can be written as
(2.14)
where
is defined as the family of operators such that
is the solution of the homogeneous differential equation
with the initial value
. For the nonlinear case in a Banach space
:
(2.15)
we consider the linear equation
,
for certain functions
. If this equation has a solution
then define a mapping
and seek a fixed point of
which will be a solution of (2.15). We note that (2.15) is similar to (2.2) as we take boundary data
into consideration and switch
and
variables. We now can adopt arguments in [39], thinking
, and write the following as the solution to (2.2)
(2.16)
where
is continuous and bounded operator. Recall from (2.10) and (2.12) that
is bounded under
and
norms, thus
is also bounded under
and
norms on any given interval of time
. Take
norm on both side of (2.16) one obtains the following inequality
(2.17)
Apply the Grownwall lemma on (2.17) one conclude that
is bounded under
norm on any given interval of time
. Therefore,
is a global classical solution to the inhomogeneous initial-boundary value problem for the modified transitional KdV Equation (1.10). Therefore we have proved the following global existence theorem.
Theorem 2.2. (Global Existence) For the initial-boundary value problem of modified transitional KdV (1.10),
,
, there exists a unique global classical solution
under the conditions either (i)
,
or (ii)
where
.
3. Conclusion
The inhomogeneous boundary value problems for the modified transitional KdV are relatively new, and this paper is our initial attempt to study the existence and uniqueness of the global solution. A lot more could be done. For example, the well-posedness of the problem (i.e. continuous dependency on initial and boundary data), decay estimates, and numerical simulations. We plan to continue our study on mTKdV in the near future.
Funding
This research was supported by the William R. Kenan Jr. Professorship and Wellesley College Faculty Awards.