In this paper we analyze a singular heat equation of the form . The singular term gives rise to very fast diffusion effects. The equation is settled in a smooth bounded domain and complemented with a general dynamic boundary condition of the form , where is the Laplace–Beltrami operator and α and β are non-negative coefficients (in particular, the homogeneous Neumann case given by is included). For this problem, we first introduce a suitable weak formulation and prove a related existence result. For more regular initial data, we show that there exists at least one weak solution satisfying instantaneous regularization effects which are uniform with respect to the time variable. In this improved regularity class, uniqueness is also shown to hold.
In this paper we address a singular heat equation having the expression
where f is an external force. The equation is settled in a smooth bounded domain , where the restriction to the three-dimensional setting is motivated by physical applications, and is complemented with dynamic boundary conditions of the form
where is the Laplace–Beltrami operator and (in particular they may both be 0, so that the homogeneous Neumann problem is included). Equation (1.1) can be viewed in the framework of non-linear diffusion problems, i.e., of equations of the form
with . When , Eq. (1.3) is the well-known porous medium equation [21] (heat equation when ); for , Eq. (1.3) lies in the class of fast diffusion equations (ultra fast when ) analyzed in several papers (see, e.g., the pioneering work [15]). In this regime very fast diffusion occurs in the regions where ϑ is small. Moreover, one can distinguish two sub-regimes, depending on the so-called first critical fast diffusion exponent (d is the dimension) which acts as a threshold between the good parameter range and its complementary range . More precisely, when and the initial condition is non-negative and locally integrable, then Eq. (1.3) (with ) on the whole space has a unique weak solution which is globally defined, positive and smooth. Moreover, solutions emanating from initial data lying in (), or even in the Marcinkiewicz space , immediately become bounded. The scenario when is drastically different for at least two reasons (we refer to [5] for further remarks). First of all, solutions may in general be unbounded and may also be non-smooth. As an example, when , one can consider, for arbitrary , the function (see [20])
which solves (1.1) with and initial condition for any . In particular, Θ is an unbounded function and for , at least until it vanishes for . In this range of m, the boundedness of the solutions is tied to the summability of the initial condition and to the value of m. More precisely, solutions are bounded whenever with (see [5]). Note that, when and (as in our case (1.1)), . A second notable feature of the fast diffusion regime, which is already evident in example (1.4), is the possible occurrence of extinction in finite time. This means that a solution may become identically zero after some finite time T which depends on the initial conditions. Consequently, positivity is lost. The ultra fast diffusion regime presents further difficulties linked to the mere question of existence (see [19] and [12]). In particular, for (non-zero) data in with one may face a phenomenon called “immediate extinction” meaning that solutions obtained as limits of reasonable approximation schemes can be identically zero for any . Note that the immediate extinction can occur also for boundary value problems with zero Dirichlet conditions. Finally, the case , , deserves a particular attention, as observed in the papers [2] and [4] dealing with the asymptotics as (the extinction time). Note that we always have and, for , we have , exactly as in our Eq. (1.1).
In this paper, we are interested in the analysis of Eq. (1.1) with the dynamic boundary condition (1.2) in the case when the source term f has zero spatial mean. Then, a straightforward computation permits us to see that conservation of mass occurs. For instance, in the case , we have for any , which manifestly excludes both immediate extinction and extinction in finite time. It is worth pointing out that Neumann (or related) boundary problems are poorly studied in the literature, even in the simpler case of the porous medium equation. In this regard, well-posedness and asymptotic results have been established in [1]. More recently, these results have been improved in [14] by means of an approach similar to ours based on Moser iteration techniques.
Our interest is twofold. From the one hand, we aim at proving existence of at least one solution under weak conditions on the initial data. To explain what we mean for “weak”, and considering for simplicity the case , we note that, thanks to the monotone structure of (1.1)–(1.2), the system admits several Lyapunov functionals. In particular, on account of physical considerations (see below for details), we may identify a natural energy functional , which is defined in (2.12) below. Mathematically, the finiteness of seems to be a minimal regularity condition on the initial datum that allows to define a rigorous concept of weak solution (cf. Definition 2.1 below). Indeed (in the simpler Neumann case ), finiteness of the energy corresponds to asking that . Hence, we have some control on the -norm of the solution (permitting to use -arguments in the analysis) and also a positivity condition. Weak solutions emanating from initial data with finite energy will be called “energy” solutions. Actually, our first result (see Theorem 5.1 below) states that, if the initial data have finite energy and f has zero mean value and satisfies suitable summability conditions, then at least one global energy solution exists; moreover, the energy remains bounded uniformly in time.
Once existence is established, we study boundedness and positivity properties of energy solutions. Assuming the (sole) energy regularity of initial data, we can prove (see Theorem 5.1) that becomes instantaneously bounded from below, namely, for we have , where the constant depends only on the initial energy and may vanish as . If, in addition, is (in space dimension ) in some -space with (), then (see Theorem 5.3) we prove an analogous bound from above ( for ). These bounds also entail further regularity properties of the solutions, which hold uniformly for large values of the time variable. Indeed, does not vanish, and does not explode, for . The main tool in our regularity proof is a suitably modified Moser iteration scheme. Note that the required extra regularity of the initial datum is in complete agreement with the above discussion on the case and with the explicit solution (1.4). However, since the choice of dynamic boundary conditions (1.2) precludes the occurrence both of immediate and of finite time extinction, it remains an open challenging question to understand whether the restriction is still optimal in the present setting. Mathematically, the main difficulties we encountered in the analysis of this problem come from the choice of the boundary conditions (1.2) which does not allow us to perform some otherwise standard a priori estimates. Actually, we have a sort of “asymmetry” of diffusion effects between the equation in the interior domain (where the Laplacian acts on ) and that on the boundary (where the Laplace–Beltrami operator acts on (the trace of) ϑ). Moreover, as the precise statements of our results show, in some situations we cannot allow α, or β, to be 0. Note, however, that the situation when both α and β vanish is always permitted because it corresponds to the simpler case of no-flux conditions, already studied in the literature.
A natural application of Eq. (1.1) comes from the so-called phase change models of Penrose–Fife type [16]. In this physical context, the unknown ϑ represents the absolute temperature of a material liable to a phase transition, while the source f can also take into account the effects of the phase variable on the temperature evolution. More precisely, in the Penrose–Fife model, Eq. (1.1) is coupled with a parabolic equation of Allen–Cahn or Cahn–Hilliard type describing the evolution of the phase variable χ (see, e.g., [9–11,17,18]). In this framework, the choice of considering a zero-mean-valued forcing function f in (1.1) can be motivated by the need of replicating in our situation some inner cancellation effects that appear in the energy estimates for the full model. An application of the present results to the Penrose–Fife system with boundary conditions of the type (1.2) (which has never been studied in the literature, at least up to our knowledge) will be given in a forthcoming paper. Besides the Penrose–Fife model, Eq. (1.1) (or, more generally, Eq. (1.3) with ) comes naturally into play in other physical contexts (see [3] and [8]). For example, it appears [13] in the study of the long-range Van der Waals interactions in thin films that diffuse on a solid surface.
The plan of the paper is as follows. In the next Section 2, we present our assumptions and state a rigorous definition of weak solution. Section 3 is devoted to proving the main technical lemmas constituting the core of our existence proof. In particular, using Moser iteration arguments, we show that, under suitable conditions on data, both ϑ and satisfy instantaneous regularization properties. Then, in Section 4 we prove that (global) existence holds for smooth and bounded initial data. Finally, in Section 5 we prove our main results. Namely, we show that existence holds for initial data enjoying the sole “energy” regularity. Moreover, we investigate regularization properties, and (under additional conditions) uniqueness of weak solutions.
Notation and hypotheses
Let Ω be a smooth bounded domain of (of course, everything could be easily extended to the one and two-dimensional cases, where, actually, better results are expected to hold). Let also so that for all , . Let , endowed with the standard scalar product and norm . Let also . We note by the norm in the generic Banach space X and by the duality between and X. We will also write for and for , for simplicity. Next, we set and and denote by the scalar product in , by the corresponding norm, and by the duality between and . We also denote by the tangential gradient on Γ and by the Laplace–Beltrami operator. We can thus set
The spaces and are endowed with the natural norms, respectively denoted by and . For instance, for , we may set , whereas for we put . Unless specified otherwise, in the sequel we shall make the following convention: when we write , h will be interpreted as a pair of functions belonging, respectively, to H and to , and both denoted by the same letter. On the other hand, when we consider (or even ), the symbol v will be intended, depending on the context, either as a function defined on Ω, or as a pair formed by a function of Ω and its trace on Γ.
For any function, or functional z, defined on Ω, we can then set
where the integral is substituted with the duality in case, e.g., . Given , we also define the measure , given by
where v represents a generic function in . Here and below, integrals over Γ are to be intended with respect to the standard surface measure. With some abuse of notation, we will also write
i.e., the “mean value” of v w.r.t. the measure . Here represents the surface measure of Γ. In case , it is intended that . For and X a Banach space, we introduce the space
which is a Banach space as it is endowed with the graph norm. Assuming be a suitable source term and letting , we can introduce the system
Our basic assumptions on the initial data are the following:
This very natural condition corresponds to asking that the initial data have finite energy, where the energy functional is defined as
In the sequel, we will simply write, with some abuse of language, , in place of . Moreover, we will note as the energy of initial data, namely
The source term is assumed to satisfy for some given
The first regularity condition seems to be necessary for controlling the energy uniformly in time. The second condition, where we require more summability in space, but allow for a locally uniform (rather than uniform) summability in time, is used for the purpose of Moser iterations. The assumption is taken because we need a uniform estimate for the spatial mean both of ϑ and of u, which may not hold for general f. Actually, integrating (2.6) in Ω, (2.7) on Γ and taking the sum, one can see that the “total mass” is conserved in time. It is also worth observing that it may be possible to extend our results by considering more general conditions on data (and, particularly, on f). However we believe that the assumptions provided above are very natural, especially in relation with the energy estimate, and may allow us to give simpler proofs.
In the sequel we will note as Problem (P) the initial-value problem for system (1.1)–(1.2). In particular, we can introduce a suitable concept of weak solution as follows:
A (global) weak solution (or “energy solution”) to Problem (P) is a triplet satisfying, for all , the regularity properties
and fulfilling, for any test function
and for all times , the relation
It is worth giving some explanation of relation (2.19). There, denotes the trace of u on Γ, which exists for almost every value of the time variable thanks to the first (2.17). More precisely, we have . Actually, for weak solutions we cannot simply write since the trace of ϑ does not necessarily exist. On the other hand, when considering smoother solutions (e.g., in the approximation detailed in Section 4 below) it will happen that ϑ is more regular so that η can be intended, in fact, as the trace of ϑ.
In the case when and , the last integral on the first row of (2.21) may make no sense since (2.15)–(2.19) do not guarantee any summability property for η, whereas when we can get help from the latter (2.15). For this reason we will be able to consider the case , only for more regular solutions (and, correspondingly, under more restrictive conditions on data).
Main technical lemmas
In this section we prove some regularization estimates holding for sufficiently smooth solutions of Problem (P). In this procedure, a sufficient regularity will always be assumed in such a way that all computations we perform make sense. For this reason, we will indicate simply by ϑ, rather than by η, the boundary temperature (indeed, the “bulk” ϑ has a trace at this regularity level). As a rule, we will use the letters c and κ to denote generic positive constants, depending only on the set Ω and on the parameters α and β, with κ used in estimates from below. The dependence, or independence, of κ and c, with respect to time will be pointed out on occurrence. The values of c, κ are allowed to vary from time to time. Finally, Q will denote a generic computable function, increasingly monotone with respect to each of its parameters, taking values in .
Regularization of u
(Moser iterations for u).
Let,,,, and let, for some,Letbe a couple of sufficiently smooth functions solving, in a suitable sense, the systemover the time interval. Moreover, let us assume thatThen, for any, we have
We will just consider the case when , which is more difficult since we cannot get any help from the boundary diffusion term. In this proof, the constant(s) c are allowed to depend (monotonically) on the length of the time interval , which is finite and assigned. Indeed, in the sequel this lemma will be applied on time intervals of fixed length. Setting , we will also assume, for the sake of simplicity, that almost everywhere. Indeed, if that does not hold, then it is easy to check that in the estimates below we can simply replace z with . That said, we test (3.2) by , where will be specified later. This gives
In order to recover the full V-norm on the left-hand side, we can multiply (3.7) by p and then add to both hand sides the quantity
Hence, using continuity of the embedding and of the trace operator from V to , we get on the left-hand side of (3.7) a quantity such that
We now choose for the first iteration. Then, we can estimate the right-hand side of (3.8) as
On the other hand, still for , we can write
whence, taking σ small enough and collecting (3.8)–(3.11), (3.7) becomes
Thus, integrating over and using Grönwall’s lemma, we readily arrive at
where the function Q has no explicit dependence on T at this level. This relation is the starting point for the subsequent iterations.
To proceed, we set to be the conjugate exponent of . Rewriting (3.7) (multiplied by p) for a suitable new choice of p, we can now estimate the right-hand side as follows:
Then, adding again the term to both hand sides and integrating the result from some (to be chosen later) to T, we arrive at
where we used, in particular, that . Next, we define, for and to be chosen later,
Then, using that and that the integration domain has measure greater than 1, by elementary interpolation we obtain
where the index and the interpolation exponent are given by the system
Dividing the second equation in (3.18) by the first one, we have
whence
and it is easy to compute
From (3.20) we also infer
Being
we then obtain from the first (3.18)
where, obviously, whenever .
Taking the th power of (3.17), by convexity we obtain
We can now start the iteration argument. Let and inductively define, for , . Moreover, let (for instance), for ,
Let us now rewrite (3.15) by taking . Setting also, for brevity, and writing in place of (to be chosen below), we then obtain, thanks also to (3.25),
Let us now make precise the choice of . First of all, we set . Then, by induction, given , we take such that
where we used that . Thus, (3.27)–(3.28) give
In particular, we obtain
Thus, setting , we have
Hence, letting and , we can rewrite (3.31), for i large enough, as
where the last productory is understood to be 1 for . Then, letting , it is not difficult to obtain (3.6), which concludes the proof (see also [17] for more details). □
If u is bounded at the initial time, we can avoid all complications connected with the choice of the sequence . Indeed, a straightforward modification of the above proof permits to show the following:
Let,,,, and let, for some, (3.1) hold. Let, as before,be a couple of sufficiently smooth functions solving, in a suitable sense, system (3.2)–(3.3) over the time interval. Moreover, let us assume (3.4) together withThen, we have
Regularization of ϑ
(Uniform stability of norm).
Let,,,. Letbe a couple of sufficiently smooth functions solving in a suitable sense system (3.2)–(3.3) over. Let also the following properties hold:where the exponent p is given and is assumed to satisfyin the case whenand, and is assumed to satisfyin all the other cases. Then,where the expression of Q is independent of the final time T.
Let us consider first the case when . We test (3.2) by . This gives
Then, being , using (3.36), we can add the inequality
Then, owing also to the continuity of the trace operator from V to , we may conclude that
Here and below, the constants c and κ are assumed to be independent of p and of time. Next, we estimate the right-hand side of (3.39) as follows:
Taking σ small enough, we then arrive at the inequality
Let us now set
Then, we need to distinguish between two different cases. First, let either or both α and β be strictly positive. Then, thanks to the assumption , it follows that . Moreover, assuming for simplicity , which is of course not restrictive, (3.44) reduces to the differential inequality
Then, integrating explicitly the ODE and applying the comparison principle, it is not difficult to obtain (3.38). We observe in particular that the procedure works on time intervals of any length with no explicit dependence of Q on time. In other words, the resulting function Q depends on T only through the quantities F and L. Note also that the dissipative term on the left-hand side is essential for the purpose of getting rid of the quantity on time intervals of arbitrary length.
Second, let us consider the case when and . Then, we need to use the boundary term resulting from (3.41). This is what forces us to assume so that (hence, in fact, we are taking exactly at least as a first iteration). Under these assumptions, we still deduce a differential inequality of the form (3.46), which is integrated exactly as before.
Finally, let us remove the restriction made at the beginning. In that case, we need to iterate the procedure a finite number of times. Namely, we can first take to get an estimate of ϑ in (and of in ). Thanks to this new information, we can repeat the procedure by taking higher values of p. We omit the details and just point out that a similar argument will be carried out in the Lemmas 3.4, 3.5 below. □
(Moser iterations for ϑ).
Let,,,. Moreover, iflet also. Letbe a couple of sufficiently smooth functions solving in a suitable sense system (3.2)–(3.3) over. Moreover, let us assume that, for some,Then, for any, we have
In this proof, we work on time intervals of assigned finite length. Hence, we may assume, as in Lemma 3.1, explicit dependence of c on the length . To start with a further Moser iteration procedure, we rewrite (3.39), multiply it by p, and then add to both sides the term , which may be controlled as in (3.40). We then deduce
Then, in the case , the proof works similarly with [18, Lemma 3.5], to which we refer the reader for details. In the cases and , , the argument can be adapted just with small variants. Note in particular that, at the first iteration step, we choose so that the latter term in (3.51) can be controlled by using Lemma 3.3. □
In the case when and , we can still prove regularization of ϑ, but the argument is a bit more delicate since, as in the corresponding case in Lemma 3.3, we cannot take advantage of the boundary gradient term. So, we have to use the trace theorem as in Lemma 3.1. As before, this forces us to assume some more summability of the initial value of ϑ. Namely, we have:
(Moser iterations for ϑ, case , ).
Let,,, and. Letbe a couple of sufficiently smooth functions solving in a suitable sense system (3.2)–(3.3) over. Moreover, let us assume that, for some, (3.47)–(3.48) hold, together withThen, for any, (3.50) holds.
As before, here we allow c to depend on . We take for simplicity . The analogue of (3.51) reads now
Then, we take first . Owing to Lemma 3.3, we then get
Let us now repeat (3.53) for a new p to be chosen below. Let also , where is a number, also to be chosen below, in the range . We then obtain
Hence, integrating (3.53) over , for some (to be chosen later) and using once more continuity of the trace from V to , we arrive (compare with (3.15)) at
Now, we perform Moser iterations as in the proof of Lemma 3.1, starting from . Then, in place of (3.18), we get the system
whence one computes, similarly as before,
and, finally,
Note that, as before, H is larger than 1 since .
Then, we can follow with minor variations the proof of Lemma 3.1 up to formula (3.27). In particular, is now defined by setting
Then, the analogue of (3.28) reads
Hence, to control the right-hand side of (3.56), we also need to take the th power of the above inequality. It is readily checked that this does not affect the validity of the argument since the exponent is asymptotically close to 1. Note also that (3.61) holds provided that . As is given by (3.59), this means that we need
which is easily shown to be true for every provided that we choose so small that
Actually, also the choice works. Notice that, since we used , it follows that the regularity (3.52) is needed in order for the iteration scheme to work. From this point on, the proof proceeds once again similarly with that of Lemma 3.1, hence we can omit the details. □
As before, we have a better result in case the “initial” value of ϑ is uniformly bounded. The proof follows the preceding ones up to straightforward modifications.
Let,,,. Letbe a couple of sufficiently smooth functions solving in a suitable sense system (3.2)–(3.3) over. Let also (3.47)–(3.48) hold, together withThen, we have
The space regularity of f, stated in (2.14) with , is strongly exploited in the proofs (cf. (3.24) and (3.58)). Indeed, if one weakens it by putting , no additional summability is gained at subsequent iteration steps and the argument fails.
Further regularity of time derivatives
We now prove that, for smooth solutions of Problem (P), the boundedness of ϑ and u implies some -regularity of time derivatives at least for strictly positive times. The proof of this result is a little bit tricky in the case since the diffusion operators on Ω and on Γ act on different functions. In particular, we cannot treat the case when and because in the derivation of the estimates the contribution of the boundary term is explicitly needed.
Let,,,. If, then let. Letbe a couple of sufficiently smooth functions solving in a suitable sense system (3.2)–(3.3) over the time interval. Moreover, letfor some (given) constants,. Then, for any, we have
We just consider the case when , which is the most difficult one. For simplicity, we can then set and write
whenever v is, say, an element of . Then, we test both (3.2) and (3.3) by (note that we are always assuming the solution to be smooth enough for our purposes). Then, standard integrations by parts lead to
Of course, using (3.68), the latter term can be simply estimated as follows:
The first term on the right-hand side of (3.71) is more delicate. Actually, owing to standard interpolation inequalities, we have
Then, the last term is moved to the left-hand side and will give a positive contribution. We now estimate the first term on the right-hand side, which requires some work. Actually, we first notice that, comparing terms in Eq. (3.3), using the trace theorem and elliptic regularity results (cf., e.g., [7, Theorems 2.5.13 and 2.7.4]), for arbitrarily small but otherwise fixed , we obtain
for a suitable depending on the choice of δ. Then, using (3.2) and Young’s inequality, we obtain
Moreover, comparing once more terms in (3.3) and noting in particular that
we arrive at
Hence, the last term in (3.74) can be controlled this way:
where is small and also depends on σ. In particular, taking σ small enough both in (3.75) and in (3.78), and collecting (3.72)–(3.78), (3.71) gives
Now, thanks to (3.66), for any τ as in the statement, we can choose such that
The thesis then follows by integrating (3.79) over . □
As before, for regular “initial” data, the property holds starting from the initial time:
Let,,,. If, then let. Letbe a couple of sufficiently smooth functions solving in a suitable sense system (3.2)–(3.3) over the time interval. Moreover, let (3.66)–(3.68) hold together withfor some. Then,
Existence for smooth data
Based on the previous lemmas, we will prove here that, for sufficiently regular initial data and source term, Problem (P) has a global solution in a rather good regularity class.
Local existence of smooth solutions
We start by showing that, for regular data, a local in time smooth solution exists. For the sake of simplicity, we give the proof only in the case when both α and β are strictly positive. Actually, the other cases can be treated with differences that are mainly of technical character.
Let,. Letand letfor suitable constants. Then, there existsdepending on f and(and in particular on,), such that Problem (P) admits a solutionover the time intervalsatisfying
We only sketch it, since it follows from more or less classical arguments for quasilinear parabolic problems. The key idea is to regularize the monotone function by introducing a function with the following properties
In other words, coincides with γ over an interval that is strictly larger than the range of the initial values of the problem. Outside that interval, we substitute it by a smooth and bi-Lipschitz approximation (e.g., we can take the first order Taylor expansion and then mollify). At this point, we can solve the problem by means of a fixed point argument. We just give the highlight of this procedure and set, for simplicity, .
As a first step, we take a function ϕ in the closed ball Φ of radius 1 of the space
where is fixed but otherwise arbitrary. Then, we consider the initial-value problem
and we claim that it admits a unique solution η lying in a bounded closed ball of the space
The simpler way to obtain this property is probably to prove it directly by interpolation. Actually, the regularity (4.7) of the datum ϕ implies the regularity (4.9) of the solution η for (this is classical and can be proved easily; notice that Γ is a smooth manifold without boundary). Moreover, the solution operator is continuous for . Hence, by standard interpolation results we get continuity of the solution map for . Notice also that, for such a choice of ε, the regularity of the boundary initial datum (which is known to lie in in view of (4.2) and the trace theorem), is sufficient. Next, we observe that, again by interpolation, the space (4.9) is continuously embedded into for some depending on the choice of ε (recall that Ω is smooth and its boundary Γ is a 2-dimensional manifold). Note also that this property may fail for . Thus, we can take so small that, additionally,
As a subsequent step, we solve the problem
This is a quasilinear parabolic system with bi-Lipschitz continuous non-linearity and Dirichlet boundary conditions. Then, by standard methods one may verify that it admits a unique solution ϑ such that
For instance, the basic a priori estimate corresponding to the above regularity can be obtained testing the equation in (4.11) by the function , where denotes the harmonic extension operator, namely
where v is, say, a function in . Note that the regularity (4.9) of the trace and the -regularity of are essential for the sake of obtaining (4.13), as a direct check permits us to verify.
Then, being bi-Lipschitz, has the same -regularity as (cf. (4.13)). Hence, we may conclude that lies in a bounded closed ball of the space
Moreover, the equation in (4.11) is quasilinear and uniformly parabolic and it has uniformly bounded initial data (by (4.2)), boundary data (by (4.10)), and forcing term (by (4.1)). Thus, standard barrier arguments entail that, up to possibly taking a smaller initial time (in a way that only depends on the known norms of and f, on the regularized function , and on the truncation values , ),
Next, let us notice that, by interpolation of Sobolev spaces (cf. once more [7, Chapter 2] for details), the space in (4.15) is continuously embedded into for any . Hence, at least for , we may apply the trace theorem [7, Theorem 2.7.4]. In particular, taking , we obtain that the function lies in a bounded closed ball of the space
which, in view of the fact that , is continuously and compactly embedded into the space in (4.7). Hence, the map
is compact. Next, we prove that, for small enough, takes values into Φ. Actually, interpolating the latter two spaces in (4.15), we obtain that lies in a bounded closed ball of , whence, applying once more [7, Theorem 2.7.4], also lies in a bounded closed ball of the space . Moreover, the radius of that ball has the form . In particular, the radius is independent of in view of the fact that all the constants appearing in the estimates performed so far are also independent of since they come from parabolic regularity theorems. In other words, we do not need to use Sobolev’s embeddings (in which case the embedding constants may explode as the measure of the time interval becomes small). Hence, since and , comparing with (4.7), we can take small enough so that takes values into Φ. Finally, by a number of standard checks one may verify that is continuous. Hence, the Schauder fixed point theorem may be applied to . This provides a local solution to the system
plus the initial conditions and the boundary condition . However, thanks to (4.16) and the latter (4.5), coincides with everywhere in . Hence, is a local smooth solution to (3.2)–(3.3). This concludes the proof. □
Energy estimate
In this section we prove the basic energy estimate satisfied by solutions of Problem (P). We start by recalling a generalized version of Poincaré’s inequality (see for instance [18, Lemma 3.2] for a proof).
Assume Ω is a bounded open subset of. Supposeanda.e. in Ω. Then, setting, the following estimate holds:the positive constantsanddepending only on Ω.
(Energy estimate).
Let,and let (2.10)–(2.11) and (2.14) hold. Letbe a sufficiently smooth solution to Problem (P). Then, we have
Test (2.6) and (2.7) with . This gives
Then, using (2.14) and the Poincaré–Wirtinger inequality, we estimate the right-hand side as follows:
with c independent of time. Integrating (4.23) in time from 0 to t, we obtain
To obtain the control on the full V-norm of u, we use Lemma 4.2. Thus, taking in (4.21), we infer
Hence, squaring, integrating over , and using (4.25), we obtain
The thesis follows combining (4.27) and (4.25). □
Proof of global existence
Our next aim is to prove that, for smooth initial data, the solution constructed in Section 4.1 has, in fact, a global in time character. We can treat all cases with the exception of , . This case will be dealt with separately in Section 5.3 below.
Let,and, if, then let. Let (2.14) hold together withfor some. Then, there exists a global solution to Problem (P) satisfying, for all,Moreover, if eitherandor, then we have more precisely
Let us fix (an arbitrary) . In this proof we will allow the constants c to depend on T. Indeed, we are working on a fixed interval and are not looking for uniform estimates at this level. In order to get a local solution via Theorem 4.1 we need to construct sequences of regularized initial and source data and satisfying, for all , (4.1) and, respectively, (4.2). Moreover, we need and in proper ways. The details of the regularization procedure are sketched in Section 5.2 below, to which we refer the reader.
Then, thanks to Theorem 4.1, for all we have a solution to the n-Problem defined on some interval , with . We now deduce global in time estimates independent of n and, for the sake of simplicity, we shall directly work on the time interval rather than on . As usual, this can be justified a posteriori by means of standard extension arguments. To be more precise, one may first extend the approximate solution up to the final time T by applying the uniform estimates at fixed n. Indeed, these estimates imply that, if is the maximal existence time of the approximate solution in the regularity class of Theorem 4.1, then the approximate solution cannot explode as (because the estimates are uniform) and consequently must coincide with the reference time T. Once the approximate solutions are proved to exist over , then one may apply once more the estimates in order to let and remove the approximation.
That said, we can first apply Lemma 4.3, which gives the bound
for independent of n. Indeed, from this point on, we go back to the notation when we indicate the boundary value of . Next, we can apply Corollaries 3.2, 3.6 (with ), which give
Clearly, the same uniform boundedness properties hold also for the traces on Γ.
Next, by Corollary 3.9 (here the restriction on α and β comes into play), we have
Comparing terms in Eq. (3.2), we also obtain
Moreover, in the case when (and hence ), we observe that
the latter bound following from (4.33)–(4.34). Hence, by standard regularity results for elliptic problems with Dirichlet boundary conditions (see, e.g., [7, Theorem 3.1.5]), we obtain
Thanks to (4.33) and (4.36), we can apply the trace theorem [7, Theorem 2.7.7], which yields
Consequently, using the regularity of the boundary initial datum (4.28) we obtain
Next, we observe that
Thus, using the boundary analogue of (4.34), (4.40), and the Gagliardo–Nirenberg inequality
which gives that uniformly w.r.t. n, we readily obtain that
whence (4.38) can be improved to
and the same bound holds for thanks again to (4.34) and (4.42).
Let us now deal with the case when . Then, if it is also , we are just dealing with no-flux conditions. Hence, from (4.36) we directly deduce (4.44) and, consequently, (4.32). If, instead, and , we then have that , so that, from (4.35), (4.36), and regularity results for Neumann elliptic boundary value problems, we deduce once more (4.38). However, it does not seem possible to arrive at (4.44) since we do not have sufficient regularity of .
In all cases, standard applications of the Aubin–Lions lemma permit to take the limit and obtain (up to the extraction of a subsequence) existence of a triplet solving Problem (P) and complying with the regularity properties (4.29)–(4.31) and, possibly, (4.32). In particular, it is worth noting that, in the case there is no boundary function η. Otherwise, η coincides with the trace of ϑ thanks to the quoted regularity properties and to continuity of the trace operator. The proof is concluded. □
Weak solutions
Existence for finite-energy data
Let assumptions (2.10)–(2.11) and (2.14) hold and let us assume that, if, then. Then, Problem (P) admits at least one energy solutionsatisfying the uniform energy estimate
and the further regularity propertywhere we have set
As before, we start with the case when α and β are both strictly positive. The other cases can be treated with small variants that will be outlined at the end of the proof. In order to apply Theorem 4.4, we consider a sequence of initial data such that, as ,
The construction of such a sequence is sketched in Section 5.2 below. Notice that we do not need to approximate f. Then, for any , the assumptions of Theorem 4.4 are fulfilled and we have existence of a “smooth” solution . Moreover, thanks to the energy estimate in Lemma 4.3 (cf. in particular (4.22)), the assumptions of Lemma 3.1 are satisfied over the generic time interval . Hence, thanks to (3.6), we obtain
where it is worth noting once more that here Q does not depend on the final time T. Indeed, we are applying Lemma 3.1 on a time interval of fixed length 2. Hence, we obtain a bound which is uniform for large T.
At this point, we use -techniques in order to take the limit . To this aim, we work on the generic interval and rewrite the approximate Eq. (2.6) in the equivalent form (which is possible since has the good regularity properties (4.30))
Then, we test (5.8) with , where we choose so that , continuously. Note that, since on Γ, we do not have to take into account the contribution of the boundary. Using (4.22) and (5.7), it is a standard matter to get
Next, for any and we introduce the approximate sign function as . Then, we write the approximate Eqs (2.6) and (2.7) for the indexes m and n, take the differences and test them, respectively, by and by . Indeed, for any and , we have
since is Lipschitz. Then, we arrive at
Here, we used integration by parts to prove that
which is possible thanks to the good regularity of approximate solutions, to monotonicity of , and to (5.10). Thus, integrating (5.10) over , for a generic , we obtain
Next, we take the limit and notice that, since is monotone increasing, it turns out that almost everywhere in and almost everywhere in , where denotes the sign-like function with . Then,
Applying the Brezis–Strauss lemma (see [6, Lemma 2]), we can integrate by parts the boundary Laplacian, which gives a non-negative contribution. Thus, we arrive at
Taking the supremum for , we finally obtain
for suitable limit functions ϑ and η. Moreover, using (4.22), (5.9), and the Aubin–Lions lemma, we obtain that, up to the extraction of a subsequence,
for all , , and for some limit function u. In particular, taking a test function ξ satisfying (2.20), we can test both (2.6) and (2.7) (at the n-level) by ξ and integrate by parts. This gives the n-analogue of (2.21). Moreover, the convergence properties proved above permit to take the limit to show that (2.21) holds also at the limit level. Hence, to conclude the proof it remains to identify the functions ϑ and η in terms of u. To do this, we first observe that, combining the first (5.16) with (5.17), it follows that almost everywhere in .
Next, by (5.17) and continuity of the trace operator, we have, for all ,
with denoting the trace of u. In particular, thanks to arbitrariness of τ, pointwise convergence holds on , up to the extraction of a further subsequence. Being almost everywhere in and for all , we then deduce that
Combining this with the second (5.16), we then obtain relation (2.19). This concludes the proof of the Theorem in the case , .
Let us now consider the case and (the case is essentially already known and, in any case, it is simpler to treat). Since Lemma 3.1 does not depend on whether β is zero or not, estimate (5.7) (and consequently (5.9)) still holds when . Moreover, it is easy to check that the Cauchy argument (5.10)–(5.16) can be reproduced also when . The proof of the theorem is concluded. □
Note that, in the case when and , need not be the trace of . Thus, there is a boundary layer in the sense specified by (5.18)–(5.19). However, (2.19) still makes sense thanks to instantaneous regularization properties.
Approximation of data
In this part, we sketch the approximation of data needed in the proofs of Theorems 4.4 and 5.1. Since the procedures are rather standard, we just give the highlights without entering too much into details.
Approximation of data for Theorem4.4. We start with the initial data. Let us given such that for all (as in the statement, see (4.28)), and let be its trace on Γ. Since we want to apply Theorem 4.1 (cf., in particular, (4.2)), for any we need to have an approximate datum (with trace ) such that for all n and
in ,
for all .
To construct we then consider the elliptic problem
Then, the standard elliptic theory gives that, for any fixed n, lies in and lies in .
To prove the convergence , we test by and, correspondingly, by . Then, by integrations by parts and Young’s inequality, it is not difficult to obtain
which clearly implies the desired convergence. On the other hand, to prove uniform boundedness of , we use a maximum principle argument. We prove only the upper bound, the lower one being completely equivalent. For a generic , we test by . Integrating by parts the Laplacian and using , we then obtain
Adding to both sides the quantity , we arrive at
This clearly gives the desired inequality for all .
Concerning the source term, recalling that f satisfies (2.14), a combination of truncation and mollification techniques, together with a suitable correction of the spatial mean values permits to construct a family of functions , , such that
The details of this construction are left to the reader. Notice that (5.22)–(5.25) suffice both to apply Theorem 4.1 at the level n to get a local smooth solution and to perform the estimates of Theorem 4.4 uniformly in n in order to let .
Approximation of data for Theorem5.1. We detail such an approximation just in the case , which is a little bit trickier. So, let such that and . We need to construct in such a way that properties (5.4)–(5.5) hold. Then, we consider first the function . Using that Γ is smooth, we can first extend it (e.g., by reflection) to a neighbourhood of . It is then clear that the new function, note it as , lies in ; moreover, . Next, we truncate , setting
Finally, we regularize, setting , where is a suitable sequence of smooth and compactly supported mollifiers. Then, straightforward checks (based on the properties of convolutions and on Lebesgue’s theorem) and a standard diagonal argument permit to verify that is smooth and tends to strongly in . Moreover, based on Jensen’s inequality, it is not difficult to verify that, for some independent of n,
Finally, we pass to the boundary component. First of all, thanks to smoothness of Γ, we can find such that can be extended (e.g., constantly along directions orthogonal to Γ) to a function defined on a neighbourhood of Γ. Thanks to Fubini’s theorem, it is then clear that both and lie in . Then, we truncate (as in (5.26)) obtaining (which can be seen as a function defined on the whole of ). Next, we mollify , introducing , for supported, say, on the ball . Finally, we take a cutoff function such that is identically one on and is supported on . Then, we set in such a way that belongs to and tends to 0 in , while its trace tends to in . Moreover, as above, one can check that is uniformly controlled in in the sense of (5.27). Then, the required approximation of is obtained simply taking .
Solutions with regularizing effects for ϑ
In this last part, we extend the previous results in three directions. First, we prove that, if (and, possibly, ) enjoy higher summability properties, then there exist weak solutions whose component ϑ satisfies time-regularization properties in the spirit of Lemmas 3.4 and 3.5. Second, we demonstrate that, under the same type of conditions on the initial data, existence holds also for and (recall that we could not deal with this case for initial data, cf. Theorem 5.1). Third, we see that uniqueness holds in the class of solutions with regularizing effects. We start with analyzing regularity:
Let assumptions (2.10)–(2.11) and (2.14) hold and let in addition, for some,Moreover, ifand, letwhereas in the other cases letThen, Problem (P) admits at least one energy solutionsatisfying (5.1), (5.2), together with the regularization estimatewhere we have setthe exponentsbeing all replaced byin the case whenand. Moreover, in all cases with the exception ofand, we haveMoreover, estimates (5.31) and (5.33) are uniform for large values of t. In other words, the expression of Q is independent of t.
For the sake of simplicity, we just prove the theorem by directly working on the “limit” solutions without referring to an explicit approximation scheme. That said, we first observe that the energy estimate (4.22) still holds. Moreover, we can still rely on the conclusion of Lemma 3.1. Next, thanks to assumption (5.28), we can apply Lemma 3.3 over the generic time interval . Note that the estimates provided by Lemma 3.3 are uniform with respect to T. We then obtain
(here and below, is replaced by in case and ). Hence, for , we can apply Lemma 3.4 (or Lemma 3.5) over the generic time interval , which has fixed finite length. This gives (5.31).
Finally, in all cases with the exception of and , we can apply Lemma 3.8 over the generic time interval where , which gives (5.33).
Then, to conclude the proof, it just remains to show that, in the case when and (that we set equal to 1 for simplicity), a weak solution still exists under the above assumptions. To this aim, we consider the system
complemented with the usual initial conditions. Then, for all , there exists at least one weak solution . Moreover, thanks to (5.33) and to regularity arguments similar to those performed in Section 4.3, is smooth enough in order for the system to make sense in the above “strong” form, at least on time intervals of the form for all .
In addition to that, we still have estimates (5.1) and (5.2). Moreover, it is worth noting that (5.2) holds independently of n. Indeed, looking back at the proof of Lemma 3.1, it is immediate to check that estimate (3.6) is independent of α. Actually, when one performs the iteration argument (see (3.29)) one simply has a functional that depends on α, but the bound for such a functional remains unchanged. The same holds when applying Lemma 3.4. In conclusion, we have the uniform bound
Thus, thanks also to Lemma 3.3, for any , , we have
Moreover, since , as an additional consequence of estimate (3.39) (with ) we have
In particular, being
we have, from (5.38)–(5.39),
In particular, this fact tells us that, in the present regularity setting, can be directly seen as the trace of . More precisely, applying the trace theorem, we have
On the other hand, testing (3.2) by a generic function of unit norm and recalling (5.1) and (5.28), we obtain
Thus, using (5.41), (5.43) and the Aubin–Lions lemma, we infer
for all . Hence, by continuity of the trace operator,
Thus, writing the weak formulation (2.21) of system (5.35)–(5.36), it is immediate to check that one can take the limit therein. In particular, it can be standardly proved that
Hence, in place of (2.19), we can now directly write in the sense of traces and a.e. in . We may also notice that, thanks to the additional regularity properties coming from (5.41)–(5.42), we could even relax a bit the requirements (2.20) on the test function ξ (we omit the details). The proof is concluded. □
Finally, let us come to uniqueness:
Let (2.10)–(2.11) and (2.14) hold. Letandbe a couple of weak solutions to Problem (P) over some intervalin the sense of Definition 2.1, both satisfying (5.31) and (5.33) and emanating from the same initial datum. Thenandcoincide over.
In view of the fact that and are smooth for strictly positive times, we can proceed as in Section 5.1 testing the difference of the equations by . We then integrate over for and arrive at the analogue of (5.13), namely
Note that we cannot integrate directly over since (5.31) and (5.33) do not extend to ; in other words, we do not have sufficient regularity to use as a test function over . Hence, we first need to take the limit , obtaining
Letting and noting that energy solutions are continuous with values in (cf. (2.15)), we obtain the assertion. The proof is concluded. □
In principle, the above proof does not rely directly on hypothesis (5.30) (or (5.29)). In other words, the conditions on initial data assumed in Theorem 5.1 may suffice. However, in that case the uniqueness statement may be vacuous since we do not know whether there exist energy solutions satisfying (5.31) and (5.33). Actually, even when (5.30) (or (5.29)) holds, the proved properties does not exclude that there might exist other energy solutions of Problem (P) that do not regularize with respect to time. The same observation can also be referred to the case when and since (5.33) is not known to hold under these conditions.
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