Abstract
In the present article we consider a capillary compressible system introduced by C. Rohde after works of Bandon, Lin and Rogers, called the order-parameter model, and whose aim is to reduce the numerical difficulties generated by the classical local Korteweg system (involving derivatives of order three) or the non-local system (also introduced by Rohde after works of Van der Waals, and which involves a convolution operator). We prove that this system has a unique global solution for initial data close to an equilibrium and we obtain the convergence of this solution towards the local Korteweg model as well as a convergence rate with respect to the order parameter, in accordance to what conjectured C. Rohde. As a by-product, the a priori estimates we obtain allow to provide global existence results in the
Keywords
Introduction
Presentation of the systems
In the mathematical study of liquid-vapour mixture, Gibbs first modelled phase transitions thanks to the minimization of an energy functional with a nonconvex energy density (see [16]). The phases are separated by an hypersurface and there are mainly two ways to describe it: either we consider that the interface behaves like a discontinuity for the fluid parameters (this is the Sharp Interface model), either we consider that between the phases lies a thin region of continuous transition (this is the Diffuse Interface approach, where the phase changes are seen through the variations of the density and which is much simpler numerically). Unfortunately the basic models provide an infinite number of solutions (few of them being physically relevant) and this is why authors tried to penalize the high variations of the density (with capillary terms related to surface tension) in order to select the physically correct solutions.
In the present paper, we are interested in the local and non-local Korteweg systems (in the diffuse interface model). These systems are based upon the compressible Navier–Stokes system with a Van der Waals state law for ideal fluids, and endowed with a capillary tensor.
Let us recall that the local model was introduced by Korteweg and renewed by Dunn and Serrin (see [15]) and the non-local model was introduced by Van der Waals and renewed by F. Coquel, D. Diehl, C. Merkle and C. Rohde. For an in-depth presentation of the capillary models, we refer to [11,17–19,25,28]).
Let ρ and u denote the density and the velocity of a compressible viscous fluid (ρ is a non-negative function and u is a vector-valued function defined on
Comparing the Fourier transform of the capillary terms, we have
Using energy methods, we proved in [7] that this system has a unique global strong solution for initial data close to an equilibrium state. The functional setting are classical and hybrid Besov spaces (taylored to the capillary term). We also obtained that when the small parameter ε goes to zero, the solution tends to the corresponding solution of the local Korteweg system and we obtained a rate of convergence in terms of ε. In [9], we provided by Lagrangian methods more precise a priori estimates giving a better understanding of the convergence and the hybrid Besov setting in terms of the linear Fourier structures.
Though, these models are not completely satisfying. On one hand, recalling the results from [2,12] (compressible Navier–Stokes system), [8,14] (local Korteweg model), and [7,19] (non-local Korteweg model), we observe that the density in the local capillary model is far more regular than in the non-local model where it shares the same frequency structure as in the compressible Navier–Stokes model (heat regularization in low frequencies and only a damping in high frequencies).
On the other hand, from a numerical point of view the local model is difficult to handle because the capillary term contains third-order derivatives. The non-local model also presents difficulties in numerical studies: even if the capillary term only contains derivatives of order one, it involves a convolution operator, whose numerical difficulty is comparable.
For this reason, C. Rohde presented in [30] a new model, called the order-parameter model, and inspired by the work of D. Brandon, T. Lin and R.C. Rogers in [5].
This new system consists in introducing in the capillary term
As explained in [30] another numerical interest is that when α is large enough, the momentum equations can be rewritten with the new pressure
In [30], C. Rohde proves (for
Assume that the initial data
In this paper, C. Rohde also conjectures that when the coupling constant α goes to infinity, these solutions converge to the solution of the local Korteweg model.
Statement of the results
In the present article, following what we did in the whole space for the non-local system (see [7]) and using Lagrangian methods from [9], we will prove that under smallness conditions, and with less regular initial data, the system has global strong solutions in the following critical spaces (we refer to the Appendix for more details on Besov spaces and hybrid spaces). We also prove the above conjectured convergence and give an explicit rate of convergence with respect to α.
The space
Let
The following result deals with the convergence in α: when the initial data are small enough (so that we have global solutions for (NSK) and
With the same assumptions as before, if
As the order parameter
Thanks to Besov injections into
Let us end this section with the following important remark: As explained in [9], the high-frequency part in the a priori estimates that we obtain in the present article (see Theorem 4) allow us perform the same method as in [6] and provide global existence results for the order parameter model in the
The article is structured in the following way: Section 2 is devoted to the proof of Theorem 2. We first introduce an interaction potential
In Section 3 we prove the convergence result from Theorem 3 and in the Appendix, we first recall basic properties of Besov spaces, then we provide estimates for the flow of a smooth vectorfield. The last part of the Appendix is devoted to Bessel functions that are needed for the expression of our new interaction potential.
We wish to emphasize that as we follow our method from [9], we will skip details and only focus on what is different: the difficulty comes from the potential
Proof of Theorem 2
Interaction potential
As announced in the introduction, we first rewrite the system in a non-local shape. Let us focus on the last equation, we can write that (for more clarity we drop the subscripts with α):
Another way to understand the limitation on the dimension consists in observing in the integral (6), that if we roughly approximate the Bessel function by
In fact (7) is also valid for dimensions
We are now able to write the system into a non-local form:
From the previous computations, we immediately get that
As we consider initial data close to an equilibrium state
The space
Due to obvious simplifications we slightly changed the notations for
We will now follow the tracks of [7] and [9] to prove the results. Classically in the study in critical spaces of compressible Navier–Stokes-type systems (see [6,12,20]), the proofs of Theorems 2 and 3 (see [7], Section 2) rely on key a priori estimates on the following advected linear system (
Let
The coefficient
Up to the necessary changes due to the Fourier expression of the potential, we use the very same methods as is [9] so we will skip details and only state the linear estimates and precise the matrix and eigenvalues for the convenience of the reader.
As in [6] and [9] the first step to prove Theorem 4 is to obtain estimates for the following linearized system:
Let
This is an adaptation of the arguments in the proof of Proposition 2 from [9]. We refer the reader to Section 2 therein and we will only point out the differences coming from the eigenvalues and eigenvectors: as in [12] or [6] we first introduce the Helmholtz decomposition of u. Defining the pseudo-differential operator Λ by
The difficulties and methods exposed here are the same as in [9], so we will roughly explain them and focus on what is new.
In order to prove Theorem 4, a natural idea is to use Proposition 1 and put the advection terms as external forces. Unfortunately, there are some obstacles: the main problem is that in
A direct use of the linear estimates will be useful only for the low frequencies (
For all
Low frequencies
For the low frequencies, we obtain (see [9], Section 3.1 for details) that there exists a nonnegative summable sequence whose sum is 1, denoted by As pointed out in [9] (Remark 29) using the linear estimates for the low frequency case, allows us to get rid of another difficulty introduced by the change of variables: in low frequencies some of the additional external force terms have too much regularity to be absorbed by the left-hand side, and not enough regularity to be controlled with a view to apply the Gronwall lemma. The only way to control them would be to use interpolation arguments that would introduce linear time dependant coefficients, and prevent us to get global in time results.
As explained, in order to get rid of the advection terms involved in system
([13]).
There exists a sequence
In order to perform the change of variable we define
Let us now perform the Lagrangian change of variable, for a function h, we define
Precisions on the capillary term
As explained, we will skip detail for what is close to the study in [9] and only point out what is different. Let us first go back to the convolution term written in (22): for a function f,
For any suitable function f and any
Thanks to the monotonicity of function In the
This section is devoted to giving estimates on the capillary term introduced in (21). As
Let As a by-product we obtain that under the previous assumptions, if t is small enough,
We refer to [9] for details and here we will only focus on what changes. The first step is to obtain pointwise estimates and then We emphasize here that the previous quotient is well defined near zero and we refer to Section 2.2. We have to face the same problem as in [9]: as we want to estimate the For this, we simply write Under the previous assumptions, there exist a positive constant To prove this result we will successively prove the following lemmas:
There exists a constant C only depending on the dimension d such that for all
For all
A direct estimate gives:
Under the same assumptions, for all
As in [9] every term is close to 1 when t is small and we obtain the result by carefully estimating the differences between these terms. For this we write:
Under the general previous assumptions, for all
Using the upper and lower bounds for ϕ given by Proposition 7, we can write that for a fixed As
Under the same assumptions, there exists a nonnegative summable sequence of summation 1, that we will also denote by
It appears then clearly that both integrals are bounded by:
As this part is strictly the same as in [9] (Section 3.5) we will not give details (in particular we refer to [6] or [9] for estimates on
Proof of Theorem 2
Existence and uniqueness, uniform estimates
As explained in the Introduction, once we have defined the interaction potential
Let us just recall some details for the global existence: using estimate (10) with When for example
As already explained (see Remark 6), we have
Rate of convergence (Theorem 3)
In this section we prove that the solution of
We recall that, due to endpoints in the Littlewood–Paley remainder term estimates, as in [7] we have the condition
If η is so small that
For small viscosities, in the case
To estimate the remainder in the case If If
We conclude that:
Footnotes
Acknowledgements
The author wishes to thank Raphaël Danchin, Nicolas Fournier, and François Vigneron for useful discussions.
The first part is devoted to a quick presentation of the Littlewood–Paley theory and specific properties for hybrid Besov norms used in this paper. The second section to general considerations on flows.
