On well-posedness of the Muskat problem with surface tension
Huy Q. Nguyen

TL;DR
This paper establishes the local well-posedness of the Muskat problem with surface tension for large initial data across all subcritical Sobolev spaces, covering various boundary conditions and dimensions, using a paradifferential approach.
Contribution
It provides the first large-data well-posedness result for all subcritical Sobolev spaces in the Muskat problem with surface tension, including unbounded curvature and non-square integrable interfaces.
Findings
Proves local well-posedness for large data in all subcritical Sobolev spaces.
Handles interfaces with unbounded curvature and non-square integrable initial data.
Reformulates the problem using Dirichlet-Neumann operators and paradifferential calculus.
Abstract
We consider the Muskat problem with surface tension for one fluid or two fluids, with or without viscosity jump, with infinite depth or Lipschitz rigid boundaries, and in arbitrary dimension of the interface. The problem is nonlocal, quasilinear, and to leading order, is scaling invariant in the Sobolev space with . We prove local well-posedness for large data in all subcritical Sobolev spaces , , allowing for initial interfaces whose curvatures are unbounded and, furthermore when , not square integrable. To the best of our knowledge, this is the first large-data well-posedness result that covers all subcritical Sobolve spaces for the Muskat problem with surface tension. We reformulate the problem in terms of the Dirichlet-Neumann operator and use a paradifferential approach to reduce the problem to an explicit…
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On well-posedness of the Muskat problem with surface tension
Huy Q. Nguyen
Department of Mathematics, Brown University, Providence, RI 02912
(Date: today)
Abstract.
We consider the Muskat problem with surface tension for one fluid or two fluids, with or without viscosity jump, with infinite depth or Lipschitz rigid boundaries, and in arbitrary dimension of the interface. The problem is nonlocal, quasilinear, and to leading order, is scaling invariant in the Sobolev space with . We prove local well-posedness for large data in all subcritical Sobolev spaces , , allowing for initial interfaces whose curvatures are unbounded and, furthermore when , not locally square integrable. To the best of our knowledge, this is the first large-data well-posedness result that covers all subcritical Sobolev spaces for the Muskat problem with surface tension. We reformulate the problem in terms of the Dirichlet-Neumann operator and use a paradifferential approach to reduce the problem to an explicit parabolic equation, which is of independent interest.
Key words and phrases:
Muskat, Surface tension, Free boundary problems, Regularity, Paradifferential calculus.
- MSC Classification: 35R35, 35Q35, 35S10, 35S50, 76B03.*
1. Introduction
1.1. The Muskat problem
The Muskat problem ([49]) of practical importance in geoscience describes the dynamics of two immiscible fluids in a porous medium with different densities and different viscosities . Let us denote the interface between the two fluids by and assume that it is the graph of a time-dependent function
[TABLE]
where is the horizontal dimension. The associated time-dependent fluid domains are then given by
[TABLE]
where are the parametrizations of the rigid boundaries
[TABLE]
Here is the horizontal variable and is the vertical variable.
The incompressible fluid velocity in each region is governed by Darcy’s law
[TABLE]
where is the acceleration due to gravity and is the th vector of the canonical basis of .
At the interface , the normal velocity is continuous
[TABLE]
where is the upward pointing unit normal to . Then, the interface moves with the fluid
[TABLE]
According to the Young-Laplace equation, the pressure jump at the interface is proportional to the mean curvature
[TABLE]
where denotes the surface tension coefficient.
Finally, at the two rigid boundaries, the no-penetration boundary conditions are imposed
[TABLE]
where denotes the outward pointing unit normal to . We will also consider the case that at least one of is empty (infinite depth) in which case the velocity vanishes at infinity.
We shall refer to the system (1.5)-(1.9) as the two-phase Muskat problem. When the top phase corresponds to vacuum, i.e. , the two-phase Muskat problem reduces to the one-phase Muskat problem and (1.8) becomes
[TABLE]
We note that the Muskat problem is mathematically analogous to the vertical Hele-Shaw problem with gravity [40, 41].
1.2. Reformulation and main results
Our reformulation for the Muskat problem involves the Dirichlet-Neumann operators associated to . For a given function , letting solve
[TABLE]
we define
[TABLE]
Proposition 1.1** **(Reformulation).
* If solve the one-phase Muskat problem then obeys the equation*
[TABLE]
Conversely, if is a solution of (1.13) then the one-phase Muskat problem has a solution which admits as the free surface.
* If is a solution of the two-phase Muskat problem then*
[TABLE]
where satisfy
[TABLE]
Conversely, if is a solution of (1.14) where solve (1.15) then the two-phase Muskat problem has a solution which admits as the free interface.
We postpone the proof of Proposition 1.1 to Appendix B. The above reformulation contains as a special case the reformulation obtained in [51] in the absence of surface tension, i.e. . In this work, we are interested in the case that is a fixed positive constant. To leading order, since , equation (1.13) behaves like
[TABLE]
It can be easily checked that in the case of no bottoms , if solves (1.16) then so is
[TABLE]
and thus the (-based) Sobolev space is scaling invariant. Interestingly, the Muskat problem without surface tension (and without bottoms) also admits as the scaling invariant Sobolev space ([51]). The presence of bottoms alters the behavior of solutions at low frequencies. Our main results state that the Muskat problem with surface tension is locally well-posed for large data in all subcritical Sobolev spaces , , either for one fluid or two fluids, with or without viscosity jump, with infinite depth or with Lipschitz rigid boundaries, and in arbitrary dimension. Here well-posedness is obtained in the sense of Hadamard: existence, uniqueness and Lipschitz dependence on initial data.
Introducing the spaces
[TABLE]
we state our main results in the following theorems.
Theorem 1.2** **(Well-posedness for the one-phase problem).
Let , and . Let be a real number with . Consider either or . Let satisfy
[TABLE]
Then there exist , depending only on and , and a unique solution to (1.13) such that and
[TABLE]
Moreover, if and are two solutions of (1.13) then the stability estimate
[TABLE]
holds for some function depending only on .
Theorem 1.3** **(Well-posedness for the two-phase problem).
Let , and . Let be a real number with . Consider any combination of and . Let satisfy
[TABLE]
Then there exist , depending only on and , and a unique solution to (1.14)-(1.15) such that and
[TABLE]
Moreover, if and are two solutions of (1.14)-(1.15) then the stability estimate
[TABLE]
holds for some function depending only on .
To the best of our knowledge, Theorems 1.2 and 1.3 are the first large-data well-posedness results that cover all subcritical Sobolev spaces for the Muskat problem with surface tension. The corresponding results in the absence of surface tension were obtained in the recent work [51]; see Subsection 1.3 for a discussion on prior results. In particular, Theorems 1.2 and 1.3 allow for initial interfaces whose curvatures are unbounded for and not locally square integrable for .
Using results on paralinearization of the Dirichlet-Neumann operator obtained in [2, 51] we shall reduce both the one-phase and two-phase Muskat problems with surface tension to the following explicit parabolic paradifferential equation
[TABLE]
where satisfies
[TABLE]
provided that
[TABLE]
We refer to Propositions 3.1 and 4.4 for the precise statements and to Appendix A for notation of paradifferential operators. Here and , defined by (2.12) and (3.2), are respectively the principal symbol of the Dirichlet-Neumann operator and the mean curvature operator ; moreover they are elliptic and of first and second order respectively. Consequently, is an elliptic paradifferential operator of third order and thus the solution to (1.19) gains derivatives when measured in . The estimate (1.20) then shows that for any subcritical data , the right-hand side is smoothing which in turn allows one to close the energy estimate in . The stability estimate is more delicate, especially for the two-phase problem.
The reduction (1.19)-(1.20) is of independent interest. It is worth remarking that unlike the case of zero surface tension [51], this reduction does not involve the trace of velocity on the interface.
This work emphasizes the virtue of the paradifferential calculus approach in establishing (almost) sharp large-date well-posedness for free boundary problems in fluid dynamics. In the context of water waves, this approach was initiated in [1, 2, 3] with inspiration from [4, 43]. In the context of Muskat, this approach was independently employed in [5, 51] for the case without surface tension. In this work, by taking advantage of the strong dissipation mechanism of the Muskat problem with surface tension, we obtain well-posedness results that allow for curvature singularity of initial data. Such a result for the water waves problem with surface tension remains open in view of the recent works [1, 30, 31, 50].
Remark 1.4**.**
Theorems 1.2 and 1.3 still hold in the following situations:
- •
Gravity is neglected (), as usually assumed for the Hele-Shaw problem.
- •
Periodic data for any .
Since , the rigid boundaries can be unbounded. The proof of Theorem 1.3 (see (4.3)) also gives that
[TABLE]
For quasilinear PDEs, stability estimates for solutions are usually obtained in rougher topology compared to initial data, e.g. [1, 2, 51]. Theorems 1.2 and 1.3 however provide stability estimates for solutions in the same topology as initial data.
Remark 1.5**.**
It is well known that the smoothing effect of surface tension bypasses the Rayleigh-Taylor stability condition required for well-posedness of free boundary problems in the absence of surface tension. In particular, Theorem 1.3 does not require that the less dense fluid is above the denser one, i.e. . We refer to [16, 18, 43, 51, 54, 55] for in-depth discussions on the Rayleigh-Taylor stability condition for Muskat and water waves.
Remark 1.6**.**
For simplicity let us consider the infinite-depth case and restrict ourselves to the graph formulation. As a consequence of the fact that the existence time in Theorems 1.2 and 1.3 depends only on the norm of initial data, if remains uniformly bounded in up to time then the solution can be continued past . It is possible that by combining the techniques in the present paper with mixed Hölder-Sobolev estimates for the Dirichlet-Neumann operator in the spirit of [3, 30], one can prove that controlling for any small would suffice.
It is an open problem for the Muskat problem (with or without surface tension) whether the control of the maximal slope implies the continuation of the solution. Any continuation criterion in terms of scaling invariant quantities should be interesting. For the 2D Muskat problem without surface tension and constant viscosity, it is known from [21] that the solution remains regular so long as the slope remains bounded and uniformly continuous.
Remark 1.7**.**
The time interval in Theorems 1.2 and 1.3 shrinks to [math] as the surface tension coefficient vanishes. The question of zero surface tension limit is interesting but is not be pursued in the present paper. We refer to [9, 10, 34] for results in this direction.
1.3. Priori results
The Muskat problem and its mathematical analog – the Hele-Shaw problem have recently been the subject of intense study in analysis of PDEs and numerical analysis. The literature is vast and we will mostly discuss the topic of well-posedness. We refer to the recent surveys [35, 38] for discussions on other topics, and in particular [15, 16, 36] for interesting results on finite-time singularity formation.
Taking advantage of the parabolic nature of the Muskat problem, global strong solutions for small data have been considered in a large number of studies. We refer to [14, 17, 18, 19, 20, 21, 22, 25, 27, 52] for data in subcritical -based and -based Sobolev spaces, and to [37] for data in the critical Wiener space . We note in particular that [18, 37] allow for viscosity jump and [27] allows for interfaces with large slopes. In the case of constant viscosity, by using maximum principles for the slope, global weak solutions were constructed in [20, 28].
We discuss in detail the issue of local well-posedness for large data. In the context of the Musat problem, the case without surface tension is better understood. Early results on local well-posedness for large data in Sobolev spaces date back to [17, 32, 56, 7, 8]. Córdoba and Gancedo [25] introduced the contour dynamics formulation for the Muskat problem without viscosity jump and with infinite depth, and proved local well-posedness in and when the interface is a graph. In [23, 24], Córdoba, Córdoba and Gancedo extended this result to the case of viscosity jump and nongraph interfaces satisfying the arc-chord and the Rayleigh-Taylor conditions. One of the main difficulties is to invert a highly nonlocal equation to express the vorticity amplitude in terms of the interface. Using an “arbitrary Lagrangian-Eulerian” approach, Cheng, Granero and Shkoller [18] (see also [39]) proved local well-posedness for the one-phase problem with flat bottoms when the initial surface , allowing for unbounded curvatures. This result was then extended by Matioc [46] to the case of viscosity jump (but infinite depth). For the case of constant viscosity, using nonlinear lower bounds, a technique developed for critical SQG, the authors in [21] obtained local well-posedness for for all . The space is scaling invariant yet requires more derivative compared to . Matioc [45] sharpened the local well-posedness theory to for the case of constant viscosity and infinite depth. This is the first result that covers all subcritical (-based) Sobolev spaces for the given one-dimensional setting. By paralinearizing the nonlinearity in the contour dynamics formulation, Alazard and Lazar [5] gave a different proof and extended the result in [45] to homogeneous Sobolev spaces, allowing non- solutions. In the recent joint work [51] of the author, we reformulated the Muskat problem in terms of the Dirichlet-Neumann operator for the general setting: one fluid or two fluids, with or without viscosity jump, with or without rigid boundaries and in arbitrary dimension. Then employing a paradifferential calculus approach we proved local well-posedness for large data in all subcritical Sobolev spaces. In [6], a similar result was independently obtained for the case of one fluid and without bottom.
Next we discuss results on large-data well-posedness for the Muskat and Hele-Shaw problems with surface tension, which is the problem considered in the present paper. Early results for the 2D case date back to Duchon and Robert [29], Chen [17] and Escher-Simonett [32] where the initial interface is smooth enough so that its curvature is at least bounded. In [9], the zero surface tension limit is established for the 2D Muskat problem with smooth ) Sobolev data. The issue of low regularity well-posedness has been recently addressed for constant viscosity and viscosity jump respectively in [45] and [46] in which the initial one-dimensional interface is taken in with . These results are -derivative above scaling, i.e. versus , yet allows for unbounded curvatures. The same result for the periodic case was obtained in [47]. Our Theorems 1.2 and 1.3 appear to be the first large-data well-posedness results that cover all subcritical Sobolev spaces for the Muskat problem with surface tension in a general setting.
The paper is organized as follows. In Section 2, we recall results on the continuity, paralinearization and contraction estimates for the Dirichlet-Neumann operator, most of which are taken from [2] and [51] . Sections 3 and 4 are devoted to the proofs of Theorems 1.2 and 1.3. Appendix A provides a review of the paradifferential calculus machinery. Finally, we prove Proposition 1.1 in Appendix B.
Notation 1.8**.**
Throughout this paper we use to denote a continuous increasing positive nonlinear function which may change from line to line but its dependency on relevant parameters will be indicated.
2. Results on the Dirichlet-Neumann operator
We consider the Dirichlet-Neumann problem associated to the fluid domain defined by (1.3) with the time variable being frozen. We shall always assume that at least . Regarding the bottom , we assume either or , where satisfying . Consider the elliptic problem
[TABLE]
where in the case of infinite depth (), the Neumann condition is replaced by the decay condition
[TABLE]
The Dirichlet-Neuman operator associated to is formally defined by
[TABLE]
where we recall that is the upward-pointing unit normal to . Similarly, if solves the elliptic problem (2.1) with replaced by then we define
[TABLE]
Note that is inward-pointing for , making a skew-adjoint operator, whereas is self-adjoint. In the rest of this section, we only state results for since corresponding results for are completely parallel.
The Dirichlet data for (2.1) will be taken in the following screened fractional Sobolev space (see [44])
[TABLE]
where is a given lower semi-continuous function. For the bottom domain , we will choose
[TABLE]
Since , we have
[TABLE]
We also define the slightly-homogeneous Sobolev spaces
[TABLE]
The continuous embeddings
[TABLE]
hold (see [51]). Here the embedding is due to the lower bound (2.5). In addition, if then according to Theorem 3.13 [44], we have . However, we have only assumed that to accommodate unbounded bottoms. Nevertheless, Proposition 3.2 [51] implies that for any two surfaces and in satisfying , the screened Sobolev space , given by (2.4), is independent of . This justifies the following notation.
Notation 2.1**.**
We denote
[TABLE]
where is defined similarly to with replaced by . For , we set
[TABLE]
It was proved in [44, 53] that there exist unique continuous trace operators
[TABLE]
with norm depending only on and . The Sobolev spaces are homogeneous and tailored to the boundaries . This is crucial for the two-phase Muskat problem since the traces obtained by solving (1.15) are only determined up to additive constants. Employing the lifting results in [44, 53] for homogeneous Sobolev spaces, it was proved in [51] that for each , there exists a unique variational solution to (2.1). This in turn implies that provided that . For continuity estimates in higher Sobolev norms, we shall appeal to the following theorem.
Theorem 2.2** ([2, 51]).**
Let , and . Consider and with . Then we have and
[TABLE]
for some depending only on and .
Since the bottoms are fixed in , we shall omit the dependence on in the remainder of this paper.
It is well known that for smooth domains, the Dirichlet-Neumann operator is a first-order pseudo-differential operator whose principal symbol is given by
[TABLE]
The one-dimensional case is special since is -independent. The following result provides error estimates when paralinearizing by , which will be the key tool for paralinearizing the Muskat problem with surface tension.
Theorem 2.3** ([2, 51]).**
Let , and . Fix a real number \delta\in\big{(}0,s-1-\frac{d}{2}\big{)}, . If and with then
[TABLE]
for some depending only on .
Theorems 2.2 and 2.3 were first obtained in [2] (see Theorem 3.12 and Proposition 3.13 therein) when , and extended to as a special case of Theorem 3.18 in [51]. It surprisingly turns out that the case with surface tension requires a less precise paralinearization compared to the one needed in [51] for the case without surface tension. This is in contrast with the water waves problem [1, 2].
Finally, we will need contraction estimates for the Dirichlet-Neumann operator in order to obtain uniqueness and stability of solutions.
Theorem 2.4** ([51, Proposition 3.31]).**
Let with . Consider and , with for . Then there exists depending only on such that
[TABLE]
3. Proof of Theorem 1.2
3.1. Paradifferential reduction
We assume that with is a solution of (1.13) and satisfies
[TABLE]
The next proposition shows that equation (1.13) can be reduced to an explicit third-order parabolic equation with a smoothing right-hand side.
Proposition 3.1**.**
Set
[TABLE]
For and , there exists depending only on such that
[TABLE]
Proof.
Let us rewrite (1.13) as
[TABLE]
Theorem 2.2 applied with gives
[TABLE]
Regarding , we apply Theorem 2.3 with and (A.11) with to have
[TABLE]
with
[TABLE]
The rest of the proof is devoted to control the main term . We paralinearize the mean-curvature operator by means of Theorem A.9 with , :
[TABLE]
where Id is the identity matrix and satisfies
[TABLE]
Consequently,
[TABLE]
where we note that . To estimate we use (A.8) and the fact that
[TABLE]
yielding
[TABLE]
We thus obtain
[TABLE]
Since (see Lemma C.1), Theorem A.4 (ii) yields that is of order and that
[TABLE]
Putting together the above considerations we arrive at
[TABLE]
which combined with (3.6) and (3.5) concludes the proof. ∎
Remark 3.2**.**
In view of (2.12) and (3.2) we have
[TABLE]
which shows that is elliptic so long as .
3.2. A priori estimates
Using the reduction in Proposition 3.1 and the symbolic calculus for paradifferential operators, we derive a closed a priori estimate for in :
Proposition 3.3**.**
Let . Assume that is a solution of (1.13) such that (3.1) is satisfied. There exists depending only on such that
[TABLE]
Proof.
Denote and . Commuting equation (3.3) with we obtain
[TABLE]
which yields
[TABLE]
In view of (3.4),
[TABLE]
In light of Theorem A.4 (ii) and Lemma C.1, is of order and that
[TABLE]
whence
[TABLE]
Next we write
[TABLE]
Applying Theorem A.4 (ii), (iii) and Lemma C.1, we find that and are respectively of order and and that
[TABLE]
Consequently,
[TABLE]
As for we first note that the lower bound (3.11) implies (see Lemma C.1). Theorem A.4 (i) and (ii) then gives that is of order ( given by (A.3)) and that
[TABLE]
It follows that
[TABLE]
and hence,
[TABLE]
Combining (3.16), (3.17) and (3.18) leads to
[TABLE]
for some depending only on . From this, (3.13), (3.14) and (3.15) we arrive at
[TABLE]
where depends only on . The gain of derivative in the second term allows one to interpolate
[TABLE]
where depends only on . We then use Young’s inequality to hide , leading to
[TABLE]
Finally, a Grönwall argument finishes the proof. ∎
As the function in (3.12) depends on the distance between the surface and the bottom, we need an a priori estimate for this quantity.
Lemma 3.4**.**
Under the assumptions of Proposition 3.3, there exist and depending only on such that
[TABLE]
Proof.
Using equation (1.13), Theorem 2.2 and the fact that , we have
[TABLE]
Fixing and using interpolation yields
[TABLE]
for some . Then in view of the embedding , this implies (3.20). ∎
3.3. Contraction estimates
Our goal in this subsection is to prove the following contraction estimate for solutions of (1.13).
Theorem 3.5**.**
Let . Assume that and are two solutions of (1.13) in that satisfy (3.1). There exists depending only on such that
[TABLE]
We first prove a contraction estimate for the remainder in the paralinearization .
Lemma 3.6**.**
Set
[TABLE]
where is defined in terms of as in (3.2). For and , there exists depending only on such that
[TABLE]
Proof.
We denote the Gâteaux derivative of a function at in the direction by
[TABLE]
By virtue of the mean-value theorem for Gâteaux derivative, it suffices to prove that
[TABLE]
Setting for , we write . Since , where is given by (3.7), it follows that
[TABLE]
Using Bony’s decomposition and the fact that , we obtain
[TABLE]
where ,
[TABLE]
Since
[TABLE]
(A.9) implies
[TABLE]
By means of (3.8) and (A.8) we get
[TABLE]
for and .
Finally, for we note that where is homogeneous of order in . Hence,
[TABLE]
and thus applying Theorem A.4 (i) gives
[TABLE]
Putting together the above estimates we arrive at (3.23) which completes the proof. ∎
Proof of Theorem 3.5
Setting we have
[TABLE]
According to Theorem 2.2,
[TABLE]
On the other hand, Theorem 2.4 applied with gives
[TABLE]
where depends only on and we denoted
[TABLE]
Consequently,
[TABLE]
Next we claim that for some depending only on ,
[TABLE]
To this end, let us fix and . Applying Theorem 2.3 with we obtain
[TABLE]
In addition, Theorem A.8 together with the embedding implies
[TABLE]
whence
[TABLE]
Next we write
[TABLE]
By Theorem A.4 (i) and Lemma 3.6,
[TABLE]
Since
[TABLE]
(see Lemma C.1), Theorem A.4 (i) gives
[TABLE]
Finally, Theorem A.4 (ii) yields that is of order and
[TABLE]
The above estimates together imply
[TABLE]
Therefore, we arrive at (3.28)-(3.29) with .
Now it follows from equations (3.24), (3.28) and the estimates (3.27), (3.29) that
[TABLE]
where satisfies
[TABLE]
where depends only on . An energy estimate for (3.32) yields
[TABLE]
The argument leading to (3.19) gives
[TABLE]
Combining (3.34), (3.35) and (3.33) we obtain
[TABLE]
for some function depending only on . By interpolation and Young’s inequality we have
[TABLE]
It follows that
[TABLE]
for some depending only on . Finally, since
[TABLE]
a simple Grönwall argument leads to (3.21).
3.4. Proof of Theorem 1.2
Consider an initial datum , , satisfying . We construct the sequence of approximate solutions , , that solve the ODE
[TABLE]
where denotes the usual mollifier that cut off frequencies of size greater than . Each exists on some maximal time interval in light of the Cauchy-Lipschitz theorem and Theorems 2.2 and 2.4 for the Dirichlet-Neumann operator. It is easy to check that the a priori estimates in Proposition 3.3 and Lemma 3.4 remain valid for . Consequently, a continuity argument guarantees the existence of a positive time such that for all and that on the uniform estimates
[TABLE]
hold for some depending only on . Theorem 3.5 also holds for , giving that the sequence is Cauchy in and thus converges to some . By virtue of Theorems 2.11 and 2.4 we can pass to the limit and obtain that is a solution of (1.13) with initial data . Finally, uniqueness and stability follow at once from Theorem 3.5.
4. Proof of Theorem 1.3
4.1. Regularity of
We first recall the well-posedness of variational solutions to (1.15).
Proposition 4.1** ([51, Proposition 4.8 and Remark 4.9]).**
Let satisfy . Then there exists a unique variational solution to the system (1.15). Moreover, satisfy
[TABLE]
where the constant depends only on .
It follows from (4.1) and Theorem A.7 that
[TABLE]
for some function depending only on . Using the variational estimate (4.2) and the paralinearization Theorem 2.3, we prove that higher Sobolev regularity for can be transferred from .
Proposition 4.2**.**
Let be the solution of (1.15) as given by Proposition 4.1. If with then and
[TABLE]
for all , where depends only on .
Proof.
Fix and . First, we claim that for , if then there exists depending only on such that
[TABLE]
Indeed, according to Theorem 2.3 there exists depending only on such that
[TABLE]
Then using the system (1.15) we obtain after rearranging terms that
[TABLE]
which together with Theorem A.4 (i) and the bound
[TABLE]
proves the claim (4.4). Note that .
We now bootstrap the regularity for using (4.4) and the inequality
[TABLE]
Let us first prove (4.6). By virtue of Theorem A.4 (ii) and Remark A.5, we have for ,
[TABLE]
where the cut-off removing the low frequency part is defined by (A.3). On the other hand, for we have
[TABLE]
which combined with (4.7) yields (4.6). Now applying (4.6) with , and invoking (4.2) and (4.4) we deduce that
[TABLE]
where depends only on . We have thus bootstrapped the regularity of from to by using (4.4) with . Since (4.4) holds for , an induction argument leads to
[TABLE]
for all . In conjunction with (4.2) and the definition (2.9) of , this yields (4.3). ∎
Remark 4.3**.**
The estimate (4.3) shows that behave like .
4.2. Paradifferential reduction and a priori estimates
Assume that with solves (1.14) and satisfies
[TABLE]
Moreover, let be the solution of (1.15) as given by Propositions 4.1 and 4.2.
Proposition 4.4**.**
For \delta\in\big{(}0,s-1-\frac{d}{2}\big{)}, , there exists depending only on such that
[TABLE]
Proof.
We rewrite (4.5) as
[TABLE]
where by virtue of Theorem 2.3 and Proposition 4.2,
[TABLE]
Using (3.9) and Theorem A.4 (i) (ii), we can bound
[TABLE]
We thus obtain
[TABLE]
for some depending only on . Plugging this into the paralinearization
[TABLE]
and using (4.11) and (1.14) we conclude the proof. ∎
It follows from (4.10) that
[TABLE]
We have thus reduced the two-phase Muskat problem to the paradifferential parabolic equation (4.9) which is of the same form as equation (3.3) for the one-phase problem. Therefore, the proofs of Proposition 3.3 and Lemma 3.4 yield the following a priori estimates.
Proposition 4.5**.**
There exist depending only on and depending only on such that
[TABLE]
and
[TABLE]
4.3. Contraction estimates
Considering two solutions and in of (1.14) that satisfy condition (4.8), we prove a contraction estimate in for the difference .
Theorem 4.6**.**
There exists depending only on such that
[TABLE]
4.3.1. Contraction estimates for
For let solve
[TABLE]
We set , , , where the subscript only signifies the difference. We also recall the notation (3.26)
[TABLE]
Lemma 4.7**.**
Let and .
1) For each , there exists depending only on such that
[TABLE]
2) For each , there exists depending only on such that
[TABLE]
with satisfying
[TABLE]
Proof.
Taking the difference of the second equation in (4.16) for and we find that
[TABLE]
Since and , this gives
[TABLE]
where
[TABLE]
Theorems A.4 (i) and A.8 together imply that for ,
[TABLE]
In light of Theorem 2.3 we have that for ,
[TABLE]
Finally, a combination of Theorem 2.15 and Proposition 4.2 yields
[TABLE]
Consequently, for we have
[TABLE]
and
[TABLE]
Invoking the relation leads to the same bound for and thus
[TABLE]
for . Now we can apply (4.6) and use the definition of (see (2.9)) to have
[TABLE]
for . Next we note that by using the variational form of (1.15) derived in Proposition 4.8 [51] it can be proved that the following contraction estimate holds
[TABLE]
By virtue of Theorem A.8 and the embedding , we have
[TABLE]
It follows that
[TABLE]
Then combining (4.22), (4.24) and an induction argument we arrive at
[TABLE]
for all . This proves (4.17). Finally, (4.18)-(4.19) follow from (4.20), (4.21) and (4.25). ∎
4.3.2. Proof of Theorem 4.6
From equation (1.14) we see that satisfies
[TABLE]
According to Theorem 2.15,
[TABLE]
Applying Theorem 2.3 and the estimate (4.17) for (with ) yields where
[TABLE]
Thus, for some depending only on we have
[TABLE]
By virtue of (4.18)-(4.19) with ,
[TABLE]
Clearly,
[TABLE]
Then in view of (3.31) we deduce that
[TABLE]
where depends only on . This reduction is of the same form as (3.32)-(3.33) in the proof of Theorem 3.5. Thus, we can conclude similarly.
4.4. Proof of Theorem 1.3
Let be an initial datum satisfying . For each , let solve the ODE
[TABLE]
where solve
[TABLE]
Note that the solvability and regularity of are guaranteed by Propositions 4.1 and 4.2. Since the a priori estimates in Proposition 4.5 and the contraction estimate in Theorem 4.6 remain true for , the existence, uniqueness and stability of solutions to (1.14)-(1.15) can be deduced as in the proof of Theorem 1.2.
Appendix A A review of paradifferential calculus
We provide a review of basic features of Bony’s paradifferential calculus (see e.g. [11, 13, 42, 48]).
Definition A.1**.**
1. (Symbols) Given and , denotes the space of locally bounded functions on , which are with respect to for and such that, for all and all , the function belongs to and there exists a constant such that,
[TABLE]
Let , we define the semi-norm
[TABLE]
2. (Paradifferential operators) Given a symbol , we define the paradifferential operator by
[TABLE]
where is the Fourier transform of with respect to the first variable; and are two fixed functions such that:
[TABLE]
and satisfies, for small enough,
[TABLE]
and such that
[TABLE]
Remark A.2**.**
The cut-off can be appropriately chosen so that when , the paradifferential operator becomes the usual paraproduct.
Definition A.3**.**
Let . An operator is said to be of order if, for all , it is bounded from to .
Symbolic calculus for paradifferential operators is summarized in the following theorem.
Theorem A.4**.**
*(Symbolic calculus) Let and .
If , then is of order . Moreover, for all there exists a constant such that*
[TABLE]
* If then is of order . where*
[TABLE]
Moreover, for all there exists a constant such that
[TABLE]
* Let . Denote by the adjoint operator of and by the complex conjugate of . Then is of order where*
[TABLE]
Moreover, for all there exists a constant such that
[TABLE]
Remark A.5**.**
In the definition (A.2) of paradifferential operators, the cut-off removes the low frequency part of . Consequently, when we have
[TABLE]
The same remark applies to Theorem A.4 (ii) and (iii).
Next we recall several useful product and paraproduct rules.
Theorem A.6**.**
Let , and be real numbers.
- (1)
For any ,
[TABLE] 2. (2)
If and , then
[TABLE] 3. (3)
If , and then
[TABLE] 4. (4)
If , , and then
[TABLE]
Theorem A.7** ([11, Theorem 2.89]).**
Consider such that . For , there exists a non-decreasing function such that, for any ,
[TABLE]
Theorem A.8** ([11, Corollary 2.90]).**
Consider such that . For , there exists a non-decreasing function such that, for any ,
[TABLE]
Theorem A.9** ([11, Theorem 2.92] and [48, Theorem 5.2.4]).**
(Paralinearization for nonlinear functions) Let be positive real numbers and let be a scalar function satisfying . If with then we have
[TABLE]
Appendix B Proof of Proposition 1.1
Setting we deduce from the Darcy law (1.5) that
[TABLE]
The one-phase problem. Then boundary condition (1.10) gives . Consequently, by the definition of we have
[TABLE]
which in conjunction with (B.1) yields
[TABLE]
Combing this and the kinematic boundary condition (1.7) we obtain equation (1.13).
The two-phase problem. Set . In view of the pressure jump condition (1.8) we have
[TABLE]
which gives the first equation in (1.15). On the other hand, since
[TABLE]
(B.1) implies that
[TABLE]
The second equation in (1.15) thus follows from (B.2) and the continuity (1.6) of . Finally, (1.14) is a consequence of (1.7) and (B.2).
Appendix C Estimates for paradifferential symbols
We prove estimates for the symbols defined in terms of and (see (2.12) and (3.2)) that are used in the proof of the main results.
Lemma C.1**.**
Let and . Then, there exists such that
[TABLE]
for all (see definition (2.6)).
Proof.
To prove (C.1) for , we rewrite as
[TABLE]
Note that and for all . Applying Theorem A.7 and the Sobolev embedding we get
[TABLE]
It follows that
[TABLE]
for all and . In view of the definition (A.1) of , we obtain (C.1). As for , we rewrite (3.2) as
[TABLE]
and argue similarly. Note that and the gradient of with respect to the first argument vanishes at . This finishes the proof of (C.1). Since , the estimates in (C.2) follow from (C.1) for , the chain rule and calculus inequalities.
Regarding (C.3), we apply Theorem A.8 and the embedding to have
[TABLE]
for all . Then, (C.3) follows as above. ∎
Acknowledgment. The work of HQN was partially supported by NSF grant DMS-1907776. The author thanks B. Pausader and F. Gancedo for many discussions on the Muskat problem. We would like to thank the reviewer for his/her positive comment and detailed reading.
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