Global well-posedness for the 2D Muskat problem with slope less than 1
Stephen Cameron

TL;DR
This paper establishes the global existence and decay of smooth solutions for the 2D Muskat problem under a slope condition less than 1, extending techniques from quasi-geostrophic equations.
Contribution
It proves global well-posedness for the 2D Muskat problem in the stable regime with slope product less than 1, using a novel modulus of continuity approach.
Findings
Solutions decay to flatness as time progresses.
Unique solutions exist for initial data with $C^{1, ext{epsilon}}$ regularity.
The slope condition ensures global regularity and stability.
Abstract
We prove the existence of global, smooth solutions to the 2D Muskat problem in the stable regime whenever the product of the maximal and minimal slopes is strictly less than 1. The curvature of these solutions solutions decays to 0 as goes to infinity, and they are unique when the initial data is . We do this by constructing a modulus of continuity generated by the equation, just as Kiselev, Nazarov, and Volberg did in their proof of the global well-posedness for the quasi-geostraphic equation.
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Global well-posedness for the 2D Muskat problem with slope less than 1.
Stephen Cameron
Department of Mathematics, University of Chicago, 5734 S. University Ave., Chicago, IL 60637
Abstract.
We prove the existence of global, smooth solutions to the 2D Muskat problem in the stable regime whenever the product of the maximal and minimal slope is less than 1. The curvature of these solutions solutions decays to 0 as goes to infinity, and they are unique when the initial data is . We do this by getting a priori estimates using a nonlinear maximum principle first introduced in [11], where the authors proved global well-posedness for the surface quasi-geostraphic equation.
1. Introduction
The Muskat problem was originally introduced by Muskat in [12] in order to model the interface between water and oil in tar sands. In general, it describes the interface between two incompressible, immiscible fluids of different constant densities in a porous media. The fluids evolve according to Darcy’s law, giving an evolution of the interface (see [5] for derivation of equations), and in 2D is analogous to the two phase Hele-Shaw cell (see [14]). In the case that the two fluids are of equal viscosity and the interface is given by the graph with the denser fluid on bottom (i.e. the stable regime), the function satisfies
[TABLE]
after the appropriate renormalization. By making a change of variables, (see the proof of Lemma 5.1 of [6]) we get the equivalent system
[TABLE]
which will be more useful for our purposes. Since the function is Lipschitz, the above integral can be viewed as a nonlinear perturbation of the half Laplacian. In fact, it is easy to see that linearizing around a flat solution gives
[TABLE]
demonstrating the natural parabolicity of the problem.
The Muskat problem is known to be locally well-posed in for with solutions satisfying and maximum principles, but neither imply any gain of derivatives (see [6], [3]).
Under the assumption , there have been a number of positive results. In [3] the authors prove an maximal principle for the slope along with the existence of global weak Lipschitz solutions using a regularized system. Recently, [9] improved the energy estimate of [3] (which holds for any solution) to one analogous with the energy estimate from the linear equation under this assumption on the slope. When the initial data with less than some explicit constant (which implies slope less than 1), [2] proves that a unique global strong solution exists. In this case [13] proves optimal decay estimates on the norms , matching the estimates for the linear equation.
Recently, [8] was also able to prove the existence of global weak solutions for arbitrarily large monotonic initial data. They did this using the regularized system from [3] to prove that both and still obey the maximum principle under this monotonicity assumption.
Because solutions to (1.2) have the natural scaling , we see that or sign bounds on the slope are scale invariant properties. We fit these two types of assumptions into the same framework by showing that the critical quantity is in fact the product of the maximal and minimal slopes,
[TABLE]
As we shall see in section 3, the derivative obeys the equation
[TABLE]
where and the kernel is uniformly elliptic of order 1 whenever . Thus we naturally get regularizing effects from the equation whenever the initial data satisfies this bound. It’s clear that implies , and for bounded monotonic data we get that since either or . Thus this provides a natural interpolation between these two types of assumptions.
In contrast to the positive results, [1] shows that there is an open subset of initial data in such that the Rayleigh-Taylor condition breaks down in finite time. That is, for some time , after which the interface between the fluids can no longer be described by a graph.
The authors of [4] made great progress towards proving global regularity. They proved that if the initial data , then the solution will exist and remain in so long as the slope remains bounded and uniformly continuous. Thus the natural next step is to prove the generation of a modulus of continuity for , hence
Theorem 1.1**.**
Let with
[TABLE]
Then there exists a classical solution
[TABLE]
to (1.2) with satisfying both the maximum principle and
[TABLE]
for some Lipschitz modulus of continuity depending solely on ,. In the case that for some , then the solution is unique with .
The uniqueness statement follows essentially from the uniqueness theorem of [4]. We note in the appendix the few small changes needed to their proof in order to apply it here.
The most vital part of Theorem 1.1 is the spontaneous generation of the modulus , as everything else will follow from that. The spontaneous generation/propogation of a general modulus of continuity has old roots as classical Holder estimates, but its only recently that the idea to tailor make moduli for specific equations emerged. The technique first appeared in [11], where the authors used it to prove global well-posedness for the surface quasi-geostraphic equation. It has had great success at proving regularity for a number of active scalar equations, that is equations of the form
[TABLE]
where is a flow depending on and is some diffusive operator. See [10], [7] for a good overview of results using this method.
To date, these tailor made moduli have only been applied to cases where all the nonlinearity has been in the flow velocity , and the diffusive term has been rather nice (typically , or at least a Fourier multiplier). We will be applying this method to , which solves the active scalar equation (1.5). Note that in this equation, the kernel defined in (3.4) is a highly nonlinear function of . Thus this is the first time the method has been applied in a fully nonlinear equation.
We prove Theorem 1.1 by deriving a priori estimates for smooth solutions to (1.2) with initial data depending primarily on . We prove enough estimates that by approximating in with smooth compactly supported initial data, we get solutions which will converge along subsequences in to a solution solving (1.2) for arbitrary initial data with .
The rest of the paper is organized as follows. We begin by repeating the breakthrough argument of [11] in Section 2. In Section 3, we differentiate (1.2) to derive the equation for , showing that it satisfies the maximum principle when . In Section 4, we state how a modulus of continuity interacts with the equation in our main technical lemma. In Sections 5 and 6 we then derive the bounds on the drift and diffusion terms necessary to prove that lemma. In Section 7, we apply our main technical lemma to a specific modulus of continuity, and finally in Section 8 we complete the proof of (1.8) by choosing the correct modulus . In Section 9, we then use (1.8) to prove a few estimates on regularity in time, guaranteeing enough compactness to prove that there are classical solutions for rough initial data. Finally in the appendix, we give a quick outline for how to modify the uniqueness proof of [4] to work for initial data with .
2. Breakthrough Scenario
Assume that with , so that there exists a solution for arbitrarily large and some by [6]. Note that under the assumption that , we will show that the maximum principle holds (see Section 3 Proposition 3.1) and hence is uniformly bounded. Fix a Lipschitz modulus which we will define later. For sufficiently small times, will have modulus since it is smooth and bounded. It then follows by the main theorem of [4] that as long as continues to have modulus , the solution will exist with .
So, we proceed as in [11]’s proof for quasi-geostraphic equation. Suppose that satisfies (1.8) for all . Then by continuity,
[TABLE]
We first prove that if we have the strict inequality , then will have modulus for .
Lemma 2.1**.**
Let , and . Suppose that satisfies
[TABLE]
for some Lipschitz modulus of continuity with . Then
[TABLE]
for all sufficiently small.
Proof.
To begin, note that for any compact compact subset ,
[TABLE]
for sufficiently small by uniform continuity. So, we only need to focus on pairs that are either close to the diagonal, or that are large.
To handle near the diagonal, we start by noting that and . Thus for every we get that
[TABLE]
Since , as . Thus we can take the point where is achieved to get that
[TABLE]
By continuity of , we thus have for sufficiently small. Hence,
[TABLE]
for sufficiently small.
Now let be such that
[TABLE]
and that implies
[TABLE]
for sufficiently small. Taking , it’s easy to check that implies that
[TABLE]
Finally, taking , we’re done.
∎
Thus by the lemma, if was to lose its modulus after time , we must have that there exist with
[TABLE]
We will show for a smooth solution of (1.2) and the correct choice of that in this case
[TABLE]
contradicting the fact that had modulus for time .
Thus we just need to prove (2.12) to complete the proof of the generation of modulus of continuity (1.8) of Theorem 1.1.
3. Equation for
So, we just need to prove (2.12). To begin, we need to examine the equation that solves. Since everything we will be doing is for some fixed time , we will suppress the time variable from now on. Differentiating (1.2), we see that solves
[TABLE]
To simplify notation, we reparametrize (3.1) by taking , and letting
[TABLE]
we get
[TABLE]
Note that
[TABLE]
for , and
[TABLE]
for .
With that in mind, define
[TABLE]
and
[TABLE]
Then integrating (3.2) by parts, we have that solves the equation
[TABLE]
As
[TABLE]
we see that
[TABLE]
and hence
[TABLE]
Thus in the case that , we then have that the kernel is a nonnegative, from which we get immediately
Proposition 3.1**.**
(Maximum Principle)
Let be a sufficiently smooth solution to (3.5) with . Then for any , we have that
[TABLE]
In particular, since the maximum principle tells us that
[TABLE]
Thus we get that
[TABLE]
where
[TABLE]
Thus is comparable to the kernel for , so solves the uniformly elliptic equation (3.5). Note that the sole reason we require is to ensure this ellipticity of .
4. Moduli Estimates
Our goal is to show that if has modulus and equality is achieved at two points (2.11), then (2.12) must hold, contradicting the assumptions of the breakthrough argument (see section 2). To that end, we first need to understand how a modulus of continuity interacts with the equation for (3.5). Hence,
Lemma 4.1**.**
Let be a bounded smooth solution to (1.2) with , and be some fixed modulus of continuity. Assume that at some fixed time that
[TABLE]
for all , and for some . Then
[TABLE]
for any , where depends only on and are as in (3.11).
This is the main technical lemma that we need. Since solutions to (1.2) are closed under translation and sign change, it suffices to consider the above situation for our proof of (2.12).
Note that (4.2) holds for any value of the parameter . Later in Lemma 6.1, we will essentially use two different values of depending on the size of . In the small regime we can simply take , but in the large regime we will need to take to be a sufficiently large constant depending only on initial data (but not on exact size of ) in order to control the size of the error term .
The proof for Lemma 4.1 is essentially a nondivergence form argument; our function is touched from above at by our modulus , and its touched from below at by . Specifically,
[TABLE]
From (4.3), we want to derive as much information as we can and bound . To that end, by dividing (4.3) through by and taking the limit as , we then get that
[TABLE]
Hence by our equation for (3.5), we have that
[TABLE]
for any . The first two terms of the RHS of (4.5) act as a drift, giving rise to the first two error terms of (4.2). The latter two terms of (4.5) act as a diffusion, giving rise to both the helpful (negative) terms in (4.2), as well as additional error terms (the middle terms of (4.2)) arising from the difference in the kernels, .
5. Bounds on Drift terms
We begin proving Lemma 4.1 by bounding the drift terms of (4.5), starting with
Lemma 5.1**.**
Under the assumptions of Lemma 4.1,
[TABLE]
Proof.
We want to bound (5.1) by symmetrizing the kernels for , and and then using the continuity in the first variable for . To that end,
[TABLE]
We bound the first integral using
[TABLE]
Thus get that for ,
[TABLE]
and hence
[TABLE]
For , we bound and
[TABLE]
in order to get
[TABLE]
Putting (5.5) and (5.7) together, we thus have
[TABLE]
∎
That leaves us with the second drift term of (4.5),
Lemma 5.2**.**
Under the assumptions of Lemma 4.1, for any
[TABLE]
Proof.
To begin, we note
[TABLE]
Recall the definition of , (3.4),
[TABLE]
So, to control (5.10) we first need to bound for , and for . For the first, using the bounds (5.3) we see that
[TABLE]
For the second, using (5.3), (5.6), and (4.1) we get that
[TABLE]
So using (5.12) and (5.13), we can first bound
[TABLE]
For the rest of (5.10), we use (5.13) again to also bound
[TABLE]
∎
6. Bounds on Diffusive Terms
Now we move on to proving an upper bound for the diffusive terms of (4.5). We can rewrite them as
[TABLE]
We begin by bounding the last term, which is an error term.
Lemma 6.1**.**
Under the assumptions of Lemma 4.1,
[TABLE]
Proof.
Using the fact that has modulus and the bounds 5.13, it follows that
[TABLE]
∎
For the other two terms in (6.1), we bound them in two stages.
Lemma 6.2**.**
Under the assumptions of Lemma 4.1,
[TABLE]
Proof.
We can bound the second term of (6.4) rather easily. Since
[TABLE]
by the uniform ellipticity of ,
[TABLE]
To bound the first term, we first define
[TABLE]
Note that since is concave and touches from above (see (4.3)), it follows that
[TABLE]
Thus for , by the uniform ellipticity of we have the bound
[TABLE]
That just leaves us with the case to analyze. Note that we can write in two distinct ways:
[TABLE]
By (6.8), for all . Thus if , then
[TABLE]
On the other hand, since
[TABLE]
for , we see that
[TABLE]
Putting these two together, we get that
[TABLE]
for . A similar argument can be made in the case that .
Putting this all together,
[TABLE]
∎
It’s clear that we can bound \displaystyle\int\limits_{\xi<|h|<M\xi}\bigg{|}h\left[K(\xi/2,h)-K(-\xi/2,h)\right]\bigg{|}dh as in (5.15). Thus the only thing remaining to prove (4.2) is
Lemma 6.3**.**
Under the assumptions of Lemma 4.1,
[TABLE]
Proof.
To see this, note that formally we should have
[TABLE]
Thus in order to get an upper bound on (6.17), we should be taking an upper bound on when and a lower bound when . Note by (4.3) that
[TABLE]
In particular, using the upper bounds bounds on for and the lower bounds for for give the result. To rigorously justify this though, we will bound
[TABLE]
from above. Taking , we’ll get
[TABLE]
The bound for follows from identical arguments.
So, fix some . By splitting the integral into a several pieces and reparameterizing, we get that
[TABLE]
In the first integral of the second line, since we have that . So applying the upper bound in (6.18) gives an upper bound on the integral,
[TABLE]
By reparametrizing back, we get that
[TABLE]
Hence combining (6.20),(6.21), and (6.22) gives us
[TABLE]
Now for , we have that , and thus
[TABLE]
Taking the limit as , we then get
[TABLE]
∎
7. Modulus Inequality
Combining all the estimates from the previous two sections, we get a proof of Lemma 4.1. Thus under the assumptions (4.1), we have that
[TABLE]
for any , where is a constant depending only on .
In [11], the authors showed that the modulus
[TABLE]
satisfies
[TABLE]
for all so long as are sufficiently small.
With that in mind, we will show that
Lemma 7.1**.**
Under the assumptions of Lemma 4.1 for the modulus defined in (7.2),
[TABLE]
as long as are taken sufficiently small depending on .
Proof.
By the Lemma 4.1 and (7.3) which was proven in [11], it suffices to show
[TABLE]
for the correct choices of , and sufficiently small.
We proceed very similarly to [11]. To begin, for we take . Then we just need to show that
[TABLE]
In this regime, note that we have the bounds
[TABLE]
Putting this all together, we get that
[TABLE]
assuming that is sufficiently small.
Now assume that . Then what we need to show is
[TABLE]
We first bound our new error terms. Using the definition of and integrating by parts, we see that
[TABLE]
assuming .
In order to bound our other new error term, we will be taking sufficiently large and then sufficiently small depending on . Noting that , we can bound our other new error term by integrating by parts
[TABLE]
assuming that
[TABLE]
and then is sufficiently small so that
[TABLE]
Note that this is where we set a value for , and that is taken sufficiently small depending on . Now that the value for is fixed, we can also control the value by taking sufficiently small that
[TABLE]
Hence,
[TABLE]
Using the same integration by parts tricks, we can also show
[TABLE]
for sufficiently small.
So combining these together, we get that
[TABLE]
Since , we finally get that
[TABLE]
if is taken sufficiently small. ∎
8. Our choice for the modulus
We’ve now shown that for the modulus defined in (7.2) that if the assumptions (4.1) hold that
[TABLE]
We claim that in fact (8.1) will hold for any rescaling as well. To see this, fix some , and suppose that satisfies the conditions of Lemma 4.1 for at time and distance . Take , which is also a solution of (1.2). Then is a solution of (3.5) with , , and satisfying the conditions of Lemma 4.1 for at time and distance . Hence by Lemma 7.1
[TABLE]
So, (8.1) will hold for any rescaling . Also note that for to hold, we must necessarily have . Thus taking
[TABLE]
we see that
[TABLE]
for all relevant . Define
[TABLE]
so that
[TABLE]
for all .
Now, suppose that at time , satisfies the assumptions (4.1) for . Then since is a rescaling of , we have that
[TABLE]
Thus we’ve constructed a modulus which satisfies (2.12), completing the proof of the generation of a Lipschitz modulus of continuity (1.8) in our main theorem.
9. Regularity in Time
With the construction of the modulus , we get universal Lipschitz bounds in space for . By the structure of (1.2), we also get regularity in space for .
Proposition 9.1**.**
Let be a classical solution to (1.2) with bounded and . Then is Log-Lipschitz in space with
[TABLE]
Proof.
For , we have that
[TABLE]
For , you can similarly show , proving the first bound.
For regularity in space, we see that
[TABLE]
For , we can bound similarly to before to get that
[TABLE]
For midsize , we have that
[TABLE]
Thus
[TABLE]
Finally, we use bounds on to get that
[TABLE]
Putting this all together, we thus have that
[TABLE]
∎
Recall that in section 2, we assumed that our initial data so that by the local existence results of [6], there is a unique solution for arbitrarily large and some . We were then able to prove the existence of the modulus as in Theorem 1.1 depending only on , and hence with the solution existing for all time by the main theorem of [4]. For an arbitrary with , the same result holds true by compactness. Let be a smooth mollifier, and be a smooth cutoff function. For with , take . Then in , with respectively as . Thus for sufficiently small, and the results of the previous section hold for the solution to the mollified problem . The bound on proven above along with the maximum principle for is enough to ensure that there a subsequence converging in to a Lipschitz (weak) solution to the original problem. In order to get a classical solution, we need regularity estimates for in both time and space. The modulus and Proposition 9.1 give the regularity in space that we need for . All that leaves is to prove regularity in time.
Proposition 9.2**.**
Let be a sufficiently smooth solution to (1.2) with . Then with
[TABLE]
where , and depends only on .
Proof.
We have that solves
[TABLE]
where is uniformly elliptic with ellipticity constants depending on . Rewriting this, we have that satisfies
[TABLE]
Let denote the righthand side of (9.11). Then is locally bounded with controlled by . Then since is a symmetric uniformly elliptic kernel, it follows that we have local bounds for for some depending on ellipticity constants (see [15]).
So, all we have to do is give bounds on depending only on . Similar to proof of Lemma 5.1,
[TABLE]
Also similar to the proof of Lemma 5.2 (specifically (5.12)), we have that
[TABLE]
so
[TABLE]
Thus since we’ve bounded the right hand side of (9.11) depending only on , we have our local bounds for for all sufficiently small. A bound that is uniform in for then gives a log estimate for , similar to the proof for regularity in space in Proposition 9.1. Thus we have estimates for both .
∎
Appendix A Uniqueness
We now prove that if our initial data with , then the solution given by Theorem 1.1 is unique with . As mentioned before, this essentially follows from the uniqueness theorem given in [4], which under our assumptions simplifies to
Theorem A.1**.**
(Constantin et al) Let be a classical, solution to (1.2) with initial data . Assume that , and that there is some modulus of continuity such that
[TABLE]
Then the solution is unique.
The authors of [4] note that the uniform continuity assumption should be the only real assumption; the decay is assumed for convenience in their proof. So, we start by proving that if , then the solution . To begin, suppose that . Then necessarily has modulus for some sufficiently small. The same proof for the instantaneous generation of the modulus will give that has modulus . Hence has modulus for all .
If , we can make the same essential argument by changing the definition of , . You can repeat the arguments of section 7 and 8 for the modulus
[TABLE]
All the error terms for are of order , while the diffusion term is of the order , so there are no problems as long as is sufficiently small. The argument for is identical to the original. Taking to be some suitable rescaling of , we then have that if has modulus , then will have modulus .
Thus if , then the solution given by Theorem 1.1 will satisfy the main uniform continuity assumption of Theorem A.1. Our solution will not decay as , but that assumption isn’t truly necessary.
Let be two uniformly continuous, classical solutions to (1.2) with the same initial data, and let . With the decay assumption, the authors of [4] are able to assume that for almost every , there is a point such that
[TABLE]
They then bound using equation , , and bounds.
Without the decay assumption, you instead use that
[TABLE]
where is arbitrary. When you go to bound , you then get new error terms which can be bounded by
[TABLE]
Since is bounded and has modulus , it then follows that
[TABLE]
Thus by taking sufficiently small depending on , we can guarantee that the new error terms . Then the original proof of [4] goes through.
Acknowledgements
I would like to thank my advisor Luis Silvestre for suggesting the problem, pointing me towards good resources, and just giving good advice in general.
The reference list from the paper itself. Each links out to its DOI / PubMed record.
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