On the lifespan of classical solutions to a non-local porous medium problem with nonlinear boundary conditions
Monica Marras, Nicola Pintus, Giuseppe Viglialoro

TL;DR
This paper investigates the lifespan of solutions to a non-local porous medium equation with nonlinear boundary conditions, providing bounds and criteria for solution blow-up and global existence based on parameters and initial data.
Contribution
It offers new bounds on the lifespan of classical solutions and establishes conditions for global existence or blow-up in a non-local porous medium problem with nonlinear boundary conditions.
Findings
Lower bounds for blow-up time in 2D and 3D when p>q.
Global existence criteria for solutions when p<q.
Analysis of solution behavior based on parameters m, p, q, and initial data.
Abstract
In this paper we analyze the porous medium equation \begin{equation}\label{ProblemAbstract} \tag{} %\begin{cases} u_t=\Delta u^m + a\io u^p-b u^q -c\lvert\nabla\sqrt{u}\rvert^2 \quad \textrm{in}\quad \Omega \times I,%\\ %u_\nu-g(u)=0 & \textrm{on}\; \partial \Omega, t>0,\\ %u({\bf x},0)=u_0({\bf x})&{\bf x} \in \Omega,\\ %\end{cases} \end{equation} where is a bounded and smooth domain of , with , and is the maximal interval of existence for . The constants are positive, proper real numbers larger than 1 and the equation is complemented with nonlinear boundary conditions involving the outward normal derivative of . Under some hypothesis on the data, including intrinsic relations between and , and assuming that for some positive and sufficiently regular function the Initial Boundary Value Problem…
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On the lifespan of classical solutions to a non-local porous medium problem with nonlinear boundary conditions
Abstract.
In this paper we analyze the porous medium equation
[TABLE]
where is a bounded and smooth domain of , with , and is the maximal interval of existence for . The constants are positive, proper real numbers larger than 1 and the equation is complemented with nonlinear boundary conditions involving the outward normal derivative of . Under some hypothesis on the data, including intrinsic relations between and , and assuming that for some positive and sufficiently regular function the Initial Boundary Value Problem (IBVP) associated to ( ‣ On the lifespan of classical solutions to a non-local porous medium problem with nonlinear boundary conditions) possesses a positive classical solution on :
when and in 2- and 3-dimensional domains, we determine a lower bound of for those becoming unbounded in at such ;
when and in -dimensional settings, we establish a global existence criterion for .
Key words and phrases:
Non-local reaction-diffusion problems, porous medium equations, global existence, blow-up.
†Corresponding author: [email protected]
2010 Mathematics Subject Classification:
35K55, 35K57, 35A01, 34B10, 74H35.
Monica Marras, Nicola Pintus Giuseppe Viglialoro*†*
Dipartimento di Matematica e Informatica
Università di Cagliari
Viale Merello 92, 09123, Cagliari (Italia)
1. Introduction, state of the art and motivations
Reaction-diffusion equations are commonly employed to model several natural phenomena appearing in various physical, chemical and biological applications. This paper is devoted to this specific reaction-diffusion problem
[TABLE]
where is defined in the cylinder , being a bounded and smooth domain of () with regular boundary , and the maximal interval of existence for the solution . Further, stands for the outward normal unit vector to the boundary and is the normal derivative of . Additionally, and are appropriate and sufficiently smooth functions of, respectively, and , arbitrarily positive constants, whilst are proper reals related one to the other.
Beyond problems arising in the mathematical models for gas or fluid flow in porous media (see [3] and [30]), the formulation in (1) also describes (see [9] and [29]) the evolution of some biological population (cells, bacteria, etc.) at some time and position which lives in a certain domain and whose growth is induced by the law (positive addends essentially represent sources which increase the energy of the system and stimulate the occurrence of an uncontrolled increasing of through the time, whereas negative ones have a damping/absorption effect, absorb the energy and, so, contrast the power of the source terms); precisely, the term idealizes the spread of the population, the parameter indicating the speed of propagation/displacement, the non-local term the births of the species and counts, respectively, its natural and the accidental deaths. Moreover, the assumption on the boundary virtually models an incoming flux of the population ; in a particular way, since realistically to a low (high) concentration of on the boundary corresponds a low (high) incoming flux, will be taken from a set including increasing functions. (For interested readers, we mention the contributions [1, 17, 18, 31, 32, 33, 34], where reactions terms similar to that in (1) have been also employed in chemotaxis models.)
Coming back to the mathematical analysis of our problem, some general results concerning existence of local or global solutions (i.e., respectively, , finite or ), have been already studied in the literature for a class of reaction-diffusion models, where the first equation of (1) reads , and verifying some standard ellipticity behaviors as well as growth assumptions (we refer, for instance, to [10, 11, 12, 25] for the case and [24] for ). In particular, as to the questions concerning existence of classical solutions to the previous equation and/or their nonnegativity (through applications of maximum principles), some results for the case can preserved if so called “non-degenerate” data are considered (see [30, 3.1 and 3.2]).
Despite a deep research, to the best of our knowledge the problems on the existence and regularity of solutions to (1) are not directly indicated in the present literature. For this reason, in this investigation we abstain from such an analysis, but rather we follow the same approach used in largely cited papers (see, for instance, [20, 21, 23, 26, 27] and references therein) where nonnegative classical solutions are a priori assumed to exist for a period of time but, also, the may become unbounded at some finite time . In particular, in [30, 1] a discussion on the Porous Medium Equation, , and the Signed Porous Medium Equation, , is carried out: in agreement with our purpose, we indicate that the default setting of the first case includes only nonnegative solutions.
As to well established results, there exists an important number of papers concerning variants of the IBVP (1), some of which dealing with properties of classical solutions: global and/or local existence, lower and upper bound of blow-up time, blow-up rates and/or asymptotic behavior. In particular, we collect the following results: I)* , and replaced with , for . When is a bounded and smooth domain of and Dirichlet boundary conditions are assigned (i.e. for ), in [21] a lower bound for the blow-up time of solutions, if blow-up occurs, is derived, and [22] essentially deals with blow-up and global existence questions for the same problem in the -dimensional setting, with , and endowed with Robin boundary conditions (i.e. , , on ). II) , and replaced with , for . For , , in [6], [7] and [13] it is shown that for the problem has no global positive solution, whilst for there exist initial data emanating global solutions. When is a bounded and smooth domain of , , and under Dirichlet boundary conditions, in [5] is proved that for the problem admits global solutions for all such that while for specific initial data produce unbounded solutions. III) , and replaced with , with and *. With bounded and smooth in , , and under Dirichlet boundary conditions, in [2] the authors treat the existence of the so called admissible solutions and show that they are globally bounded if or , as well as the existence of blowing up admissible solutions, under the complementary condition . IV) , and replaced with , with . In a bounded and smooth domain of and under Robin boundary conditions, a lower bound for the blow-up time if the solution blows up is determined under the assumption whilst conditions which ensure that the blow-up does not occur are also presented if (see [15]). V) and , with . In a bounded and smooth domain of and under proper nonlinear boundary conditions, in [16] a lower bound for the blow-up time if the solution blows up is determined under the assumption VI) , . In a bounded and smooth domain of , , and under Dirichlet boundary conditions, classical nonnegative solutions which are global or blow up in finite time are derived for any , for some , provided some compatibility conditions and assumptions on the data are given (see [14]). VII) , . In a bounded and smooth domain of , , and under various boundary conditions, in [35] for any compatible classical nonnegative solutions which are global are attained if , whereas for blowing up ones are detected (see also [28]).
Motivated by the discussion so far presented, aim of the present research is expanding the underpinning theory of the mathematical analysis of problem (1), which is not included in the above cases. In particular, the aforementioned state of the art inspires our work, and even if we will use some ideas employed in those items to address our statements, some further derivations will be necessarily required; moreover we do not restrict to prove our main theorems but we complement the general presentation of the manuscript by means of remarks and discussions.
To be precise, our contribution includes an analysis for the maximal interval of existence for classical solutions (in the sense of the Definition given in 2 below) to system (1), where plays the role of the unknown and obeys the following extensibility criterion ([4, 10]): either , so that remains bounded for all and all time and , or is finite (blow-up time), so that exists only in and as .
Thereof, we prove three theorems which provide its estimates or its precise value; they are discussed in details in 3, whilst now they are briefly summarized as follows:
Lower bound of in and : Theorem 3.1 and Theorem 3.2. If for , with , with , behaving as and sufficiently regular problem (1) admits a positive classical solution which becomes unbounded in at some finite time , then there exists a computable such that .
Criterion for global existence in , : Theorem 3.3. If for , , behaving as and sufficiently regular problem (1) admits a positive classical solution , then holds that .
2. Assumptions, definitions and preparatory lemmas
In this section we fix crucial hypothesis and lemmas which will be considered through the paper in the proofs of the main theorems. This preparatory material is herein presented according to our purposes.
Assumption .
For any , is a bounded and smooth domain of , star-shaped, convex in two orthogonal directions and such that, for some origin inside , its geometry is characterized by
[TABLE]
Definition .
A classical solution to problem (1) is a positive function which satisfies (1), for some .
Definition .
For any and , let finite. We say that a nonnegative function blows up in -norm at finite time if
[TABLE]
Lemma 2.1**.**
Let be a domain satisfying Assumption . For any positive function and , we have
[TABLE]
Moreover for every arbitrary we also have that:
If
[TABLE]
If
[TABLE]
Proof.
For the proofs see [19] and [31, Lemma 3.2]. ∎
3. Analysis and proofs of the main results
After the preparations in 2, we are in the position to demonstrate the theorems whose general overviews were summarized in 1.
3.1. Lower bounds of the blow-up time
The first theorem is concerned with lower bounds of the blow-up time , through which is identified the maximal interval where solutions to system (1) are defined. We are not aware of general results indicating assumptions on the data which straightforwardly infer the existence of unbounded solutions to such a system; nevertheless, in the spirit of the results discussed in , for which blow-up may manifest for large initial data and high effects of source (coefficient ), or low absorption or/and diffusion (coefficient or/and ), we understand that also in view of the incoming flow of the population , it seems reasonable to expect scenarios where unbounded solutions may appear.
Theorem 3.1**.**
Let be a domain of satisfying Assumption , and . Moreover for any and
[TABLE]
let be a continuous function such that , for and . If is a classical solution, in the sense of Definition , to (1) emanating from a positive initial data , for some and such that on , which additionally complies with Definition , then there exist computable constants and such that for
[TABLE]
In particular
Proof.
If is a positive classical solution of (1) defined in and satisfying on , by setting and using the integration by parts formula, the evolution in time of fulfills for all
[TABLE]
Since by the Hölder inequality (recall and ) we have that
[TABLE]
from assumption , , and the pointwise identity we get neglecting the nonpositive term
[TABLE]
For the value of as in our assumptions, the above relations reads
[TABLE]
so that (2) with and provides
[TABLE]
and by plugging this gained estimate into (6), one achieves for all
[TABLE]
On the other hand, applications of the Hölder and the Young inequalities allow us to control some terms in (7). Precisely for all holds that
[TABLE]
which infer through (7) and on the entire interval
[TABLE]
As to , we invoke (4) to get on
[TABLE]
so that, using the identity and introducing the constants
[TABLE]
after some tedious computations, inequality (9) is simplified to
[TABLE]
where for convenience we have set on .
Additionally, for any fixed there exists such that , leading to
[TABLE]
In order to obtain an explicit estimate (see Remark 1 below) of lower bounds for , we do not neglect the negative addendum but rather we treat it in terms of and . In this sense, by using Young’s inequality, we can write (recall and ) for any
[TABLE]
from which (10) is transformed into
[TABLE]
Finally, choosing and, in turn, setting we have
[TABLE]
Now, since we are assuming that as , can be non decreasing, so that with , or non increasing (possibly presenting oscillations), so that there exists a time where . In any case, for all , where . Henceforth, by integrating (11) between and , we arrive at (recall ) this explicit estimate for :
[TABLE]
∎
Remark 1**.**
We point out that if in (10) we ignored the negative term associated to , instead of (11) we would write
[TABLE]
and the claim of the theorem would read
[TABLE]
being in this case the last integral convergent but not explicitly computable.
Through some straightforward manipulations we can prove that the previous theorem holds even in 2-dimensional settings, precisely as established in this
Theorem 3.2**.**
Let be a domain of satisfying Assumption . Then, under the remaining assumptions of Theorem 3.1, there exist computable constants and such that for
[TABLE]
In particular
Proof.
Similarly to what done throughout the proof of Theorem 3.1, let us rely on (7) and (8). Conversely, in order to estimate we have now to refrain from using (4) but (3), which yields for
[TABLE]
Subsequently, for on , manipulations of the previous bound in conjunction with (7) and (8) provide computable positive constants , , (which we omit to calculate) and
[TABLE]
with the property that the following is ensured:
[TABLE]
As before, for any fixed there exists such that and henceforth
[TABLE]
Using Hölder’s and Young’s inequality, we can estimate on the term involving by means of a combination of and , precisely obtaining
[TABLE]
In this way, expression (12) reads
[TABLE]
and for and we finally have
[TABLE]
As a consequence of these operations, and reasoning as in Theorem 3.1, our claim is given since
[TABLE]
∎
Remark 2**.**
In line with Remark 1, but unlike its conclusion, if in (12) we neglected the last negative part, instead of (13) we would have
[TABLE]
and the claim of the theorem would read
[TABLE]
being the last integral also explicitly computable if (and only if) . More exactly, properties of inverse hyperbolic functions give
[TABLE]
3.2. A criterion for global existence
In the last result, we are interested to examine the opposite situation described in Theorems 3.1 and 3.2. More exactly, we establish that when the effect of the source (coefficient ) is enough stronger than that of the diffusion (coefficient ) but weaker than the one of the dampening (coefficient ), if a double stabilizing effect from the diffusion and the absorption somehow surpasses the same action of the source, system (1) does not suffer from blow-up phenomena, even for arbitrary large initial data and in presence of an incoming flow of the population .
Theorem 3.3**.**
Let be a domain of , satisfying Assumption . Moreover, for , , let , with . If is a classical solution, in the sense of Definition , to (1) emanating from a positive initial data , for some and such that on , then , or equivalently .
Proof.
If is a positive classical solution of (1) defined in and satisfying on , by differentiating we derive
[TABLE]
where we have employed the following bound, consequence of the Hölder inequality:
[TABLE]
An application of (2) and the identity provide
[TABLE]
Now, by considering that
[TABLE]
relation (14) becomes by virtue of (15)
[TABLE]
where, evidently, we have neglected the nonpositive term .
Additionally, from the Young inequality we obtain that for any
[TABLE]
so that fixing this expression holds
[TABLE]
Combining this gained bound with (16), we get
[TABLE]
Since , Young’s inequality produces for any
[TABLE]
where in view of the hypothesis and . Subsequently, by plugging (18) into (17), we obtain
[TABLE]
where
[TABLE]
Now we let sufficiently small as to ensure (as an example we see that for we have ). Thereafter, since the Hölder inequality (recall ) gives
[TABLE]
we deduce from (19) that
[TABLE]
where we introduced for all . In order to establish an absorptive differential inequality for , we use again Hölder’s inequality to observe that
[TABLE]
so that in view of (20) we arrive at this initial value problem,
[TABLE]
from which is guaranteed that
[TABLE]
Finally, well know extension results for ODE’s with locally Lipschitz continuous right side (see, for instance, [8]), show that ; indeed, if were finite, as and it would contradict (21). ∎
Acknowledgements
The authors thank professor Stella Piro Vernier for her fruitful remarks and indications. MM and GV are members of the Gruppo Nazionale per l’Analisi Matematica, la Probabilità e le loro Applicazioni (GNAMPA) of the Istituto Nazionale di Alta Matematica (INdAM) and are partially supported by the research project Integro-differential Equations and Non-Local Problems, funded by Fondazione di Sardegna (2017).
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