Existence and uniqueness of solution to a hyperbolic-parabolic free boundary problem for biofilm growth
Abstract
This work presents the existence and uniqueness of solution to a free boundary value problem related to biofilm growth. The problem consists of a system of nonlinear hyperbolic partial differential equations governing the microbial species growth, and a system of parabolic partial differential equations describing the substrate dynamics. The free boundary evolution is governed by an ordinary differential equation that accounts for the thickness of the biofilm. We use the method of characteristics and fixed point strategies to prove the existence and uniqueness theorem in small and all times. All the equations are converted into integral equations, in particular this transformation is made for the parabolic equations by using the Green’s functions. We consider Dirichlet-Neumann and Neumann-Robin boundary conditions for the substrates equations and their extension to the case with variable diffusivity.
keywords:
Biofilms , free boundary problem , Existence and uniqueness , Integral equations, ModelingMSC:
35A20 , 35A08 , 35A07 , 35A22, 35C15 , 35R35[inst1]organization=Dipartimento di Matematica e Applicazioni ”Renato Caccioppoli”,Università degli di Studi di Napoli ”Federico II”,addressline=Via Cintia 1, Complesso di Monte Sant’Angelo, city=Naples, postcode=80126, state=Naples, country=Italy \affiliation[inst2]organization=Faculté des Sciences et Technologies, Université de Limoges,addressline=123 Avenue Albert Thomas, city=Limoges, postcode=87100, state=Haute-Vienne, country=France
1 Introduction
Biofilms are defined as a community of microorganisms embedded in a matrix of extracellular polymeric substances [1].
The experimental study of biofilms is relatively complex and expensive. Yet, a good understanding of the metabolic and chemical mechanisms taking place in and around the biofilm is important in several fields. In the medical field, for example, this understanding can facilitate the development of high-powered antibiotics since biofilms are known to be resistant to antibiotics.
In the environmental field, biofilms are very important in wastewater treatment as they are responsible for various metabolic processes participating in waste degradation.
For several decades mathematical models have been proposed to contribute to the understanding of biofilms, evolving from 1D to 2D to 3D. Early models treated the biofilm as a continuum in one dimension and are exemplified by the founding stone biofilm model introduced by Wanner and Gujer [2]. Such model is based on a free boundary problem comprising a system of nonlinear hyperbolic systems which accounts for the biofilm growth, a system of diffusion-reaction equations for the substrates diffusion and conversion within the biofilm, and an ordinary differential equation that accounts for the biofilm thickness evolution. Although more sophisticated 2D and 3D models have been designed starting from the late 1990s with the aim to catch the highly complex heterogeneous 3D biofilm structure, these models have not found applications in engineering practice due to their complexity, and instead, there has been a pull-back towards 1D biofilm models for engineering applications [3].
In line with this trend, 1D Wanner-Gujer based models have been formulated and advocated for modelling biofilms in engineering systems.
The phenomena modelled include, but are not limited to, biosorption [4], precipitation [5], invasion and attachment of new species [6], the role and interactions between the suspended microbial populations and the biofilm [7, 8].
In most of the models in literature, the forcing terms for the hyperbolic equations are modeled according to Monod kinetics which account for the microbial growth as a nonlinear function of the available nutrients. In the diffusion equations, these terms express the uptake or production of substrates by microbial activity.
Due to the complexity of biofilm models, both with respect to mathematical structure and number of parameters, many works are limited to numerical simulations without ever considering the mathematical justification of the models or a rigorous analysis of its dynamics [9, 10, 7].
To cover this lack, recent works have been dedicated to the qualitative analysis of biofilm models of this type. Some of them focus on existence results for simplified models [11, 12]; others consider the pseudo stationarity of the diffusion equations due to time-scale arguments [13, 14].
In this work we study the existence and uniqueness of the complete 1D biofilm model as originally formulated in [2]. This study can be adapted to any kind of 1D biofilm from sorption to precipitation models.
To achieve this, we use the method of characteristics and transpose the partial differential equations into integral systems. Then we state and prove an existence and uniqueness theorem of the solution to the problem in small and large time.
Next, we briefly consider the case of the parabolic equation with a variable diffusion coefficient using the single layer potential.
The rest of this manuscript is organized as follows: in section 2, we present the model subject to this study, section 3 is devoted to the reduction of the PDEs to integral equations and to the existence theorem in small times. The extension of this result in large time is presented in section 4 while the case of parabolic equations with variable diffusivity case is discussed in section 6. We consider the Neumann-Robin boundary conditions in section 5 and conclude the paper and propose future recommendations in section 7.
2 The mathematical model
The biofilm model considered in this work is formulated as a free boundary problem made of a system of nonlinear hyperbolic PDEs, a system of quasi-linear parabolic PDEs, a PDE for the velocity growth of the microbial mass, and the free boundary is given by an ODE modelling the evolution of the biofilm thickness over time.
In the sequel, we will denote by
-
1.
the concentration of biomass where are the volume fractions occupied by the biomasses in the biofilm and the density of the biomass, assumed constant for simplicity. In addition, the volume fractions are supposed to satisfy the incompressibility constraint
(1) -
2.
the concentration of nutrients (dissolved components) in the biofilm;
-
3.
the convective growth velocity of the biofilm;
-
4.
the reaction term in the hyperbolic equations which accounts for the biomass growth and decay rate;
-
5.
the reaction term of the parabolic equations which accounts for the impact of the consumption/production of the substrate (nutrient) by the biomass;
-
6.
the thickness of the biofilm, which is the unknown boundary (free boundary) of the mathematical problem, and the initial biofilm thickness.
The complete model considered can be stated as follows (details on the derivation and some applications can be found in [2]):
(2) |
with the following initial condition:
(3) |
By writing equations (2) in terms of volume fractions , summing over and using the constraint (1), we get the velocity equation below:
(4) |
with boundary condition reflecting the zero biomass flux at the substratum ()
(5) |
The equation for the thickness is given by:
(6) |
where is the attachment and detachment function which can assume positive or negative values. In last position we have the system of diffusion equations for the substrates, with initial and boundary conditions:
(7) |
3 Reduction to integral equations and local existence and uniqueness
The diffusion system in a planar biofilm is now given by 7. We make a change of variable by setting , and after substituting in (7) we get the following equation:
(8a) | |||
(8b) | |||
(8c) | |||
(8d) |
where and In the sequel, we will also use and and the notation will stand for with any variable when no confusion is possible.
Consider the following kernel of the heat equation [15, 16, 17] :
(9) |
Define the following Green and Neumann functions in the half plane respectively given by:
(10) |
(11) |
To derive the solution of (8), we integrate the following Green’s identity on , :
After introducing the boundary and initial conditions, we get:
(12) |
where
(13) |
(14) |
and in equation (12), we have to determine and . By letting in equation (12) we get:
(15) |
Next, we use the following property of the function K which is given in Theorem 1 of Chapter 5, page 137 of [15] and in Lemma 4.2.1, page 50 of [16] :
(16) |
where is a continuous function. Taking the derivative of over in the domain , and letting , and using relation 16 (or equivalently if we let ), we get:
(17) |
where
(18) |
In this way we have just proved that for any solution of (8) for all , (defined by (13)) has to satisfy the integral equation (17), where is given by (19) (for ) below:
(19) |
Conversely, we consider that for some is a continuous solution of the integral equation (17) for and then we prove that form a solution of equations (8) for for all .
We can easily check that satisfies (8a), (8b), and (8d). To verify that it satisfies the boundary condition (8c), we integrate Green’s identity 12 as before and we get:
(20) |
where Equation (20) is the same as (12) if the third integral of the right hand side is null. Since vanishes, the third integral is zero. So, the condition is fulfilled. However, we still need to prove that so that the boundary condition is satisfied. We thus have
(21) |
for ,
We recall that
Hence, for any continuous function
Since is continuous and bounded, we can write
and in particular that
Using the continuity of , we get
with
Using Grönwall’s lemma, we conclude that and thus, the boundary condition (8c) is satisfied.
In summary, we have proved the following theorem:
Theorem 1.
Next, we will derive integral equations for the hyperbolic equations rewritten here in compact form:
(22) |
with the following initial condition:
(23) |
Let us denote the characteristics of this system by so that they satisfy the following initial value problem:
(24) |
Considering equation (6) for , it follows immediately that Thus, to get the integral equation for (22)–(23), we will use the characteristics coordinates that will be noted by for simplicity:
(25) |
(26) |
(27) |
(28) |
with The integral equation for the free boundary is given by:
(29) |
Finally, we convert equations (12) and (17) into characteristics coordinates. When , and (to simplify the writing, we will drop the variable in brackets and write and for and respectively when no confusion is possible), we have:
(30) |
and the equation for is
(31) |
where and denote respectively and . Moreover, in characteristic coordinates assumes the following form:
Before we prove the existence and uniqueness theorem, we need the following lemmas to use the Banach-Caccioppoli fixed point theorem.
We consider the space of continuous functions
where is given by
We choose the vector such that and we define the map such that
where () are respectively given by
We shall prove the properties of . We first need the following lemma whose proof is immediate.
Lemma 2.
P1. maps into itself. In what follows, we will mainly focus on the fourth component of The proof for the other components is similar to the one proposed in [14], so we skip it.
Lemma 3.
Let , and a Lipschitz over with a Lipschitz constant Under the hypothesis of Lemma 34 we have the following properties
(35) |
(36) |
(37) |
(38) |
(39) |
(40) |
(41) |
Proof:
To prove (35), we choose such that
We have
By using this last inequality and the definition of
the inequality (35) follows easily.
The inequality 36 is immediate and can be found in [18], same for 38.
To prove 37, we use the definition 11 and the inequality holds. The inequality 39 can also be proven in the same way. Finally, inequality 40 holds because is Lipschitz and
To prove inequality 41 we use the following exponential inequality [18, 19]:
(42) |
We have
P2. is a contraction. To show that is contraction in its fourth component, we consider that and and denote
(43) |
If we consider two functions and corresponding respectively to and but by means of 29, then we have the following inequalities:
(44) |
(45) |
Note that and also satisfy inequality 34.
Lemma 4.
Let and F a Lipschitz function over Then we have:
(46) |
(47) |
(48) |
(49) |
(50) |
(51) |
where
and
(Here and correspond to and ).
(52) |
By using the mean value theorem and inequalities 33, 34, and 44 we get inequality 46.
Let us denote by I the left hand side of the inequality 47.
By taking such that and by using the mean value theorem again, we have
Setting
and
it can be checked that
Then, we make the following change of variable and the inequality becomes
The same reasoning can be applied to . So, the original inequality holds .
Inequality 48 can be proved as follows again by using the MVT:
Inequality 50 can also be proved in the same way. Denote the left hand side of 49, by J, we have:
On one hand we have
and on the other hand we have
By carrying out similar calculations as before and taking into account that is inferior to the product of its first term and we get:
This completes the proof for the original inequality.
The left hand side of 51 is equal to:
It is easy to check that
Inequality 52 can be also proved in the same way. This completes the proof.
Theorem 5.
The map is well defined and it is a contraction if it satisfies the following inequalities:
(53) |
(54) |
(55) |
where
with
and is the sum of right hand site of inequalities in lemma 4.
Then, the original problem has a unique solution.
Proof. By lemma 3, we know that Choosing M to satisfy and if 55 holds, we have To complete the proof, we define , and
We can finally write:
Then by choosing two functions and corresponding to v we have the following
By lemma 4, we have and by 55, and choosing M and such that we have a contraction. Then the theorem is proved.
Remark 1.
When attachment or detachment is the most prevailing, then the function is different from zero. In either of these two cases the free boundary coincides with the characteristics-like lines. In case of detachment, the thickness equation is given by
(56) |
This case can be treated as in [14, 20]. When attachment is the most prevailing as at the earlier moments of the biofilm life, the free boundary is given by
(57) |
This case has been widely studied in [21] especially for biomass equations and the steady-state substrates equations.
In both these cases, the free boundary and the characteristics-like lines do not coincide anymore.
All the equations presented here can be treated in the same way for each of these cases.
We will briefly prove the global existence.
4 Global existence
We want now extend our solution to We consider such that
We introduce the following notations to get
where
We also have
(58) |
(59) |
(60) |
and
(61) |
Now, we check that these integrals are still bounded. First, we notice that can be written as
Then we notice that
and
Thus,
(62) |
On the other hand we have:
5 Robin-Neumann boundaries
The formulation of the second principle is influenced by these analyses. In [23, 24], it is hypothesized that a specific measurement away from the substratum, defined as (where h stands as a specified positive constant), the concentration of the substrate to that within the main fluid, denoted by This particular substrate, once dissolved, moves from the primary liquid into the biofilm between and is then utilized as per equation 7. It’s assumed that no biochemical processes take place on which leads to consider homogeneous parabolic equations for . The resolution at steady-state results in
(63) |
or equivalently
(64) |
where denotes the diffusion rate of substrate j in the bulk liquid. In equation 64 and For we get the boundary conditions in the previous sections and for we have a Neumann boundary condition which can be treated in the same way as in this section.
By integrating the Green’s identity as before we get
Introducing the initial and boundary conditions as before, we get
(65) |
where
(66) |
The function is still given by equation 15 as follows
(67) |
and the function is determined by letting so that we can write
(68) |
Hence, the substrates system 8a-8c together with Robin boundary condition 63 is equivalent to the simultaneous system of integral equations 65, 67 and 68 whenever satisfy the equation 19. Converting these integral equations into characteristics we get the following system
(69) |
(70) |
(71) |
As for lemmas 3 and 4 we can establish estimates that guarantee the existence and uniqueness theorem 5.
6 Parabolic equation with variable diffusivity
We have considered so far equations with constant coefficients. However, experiments show that some phenomena happening inside a biofilm cannot be modeled by means of equations with constant coefficients. One of leading processes occurring in a biofilm is precipitation. We recently proposed a model on this topic (see [25]) where the following diffusion equation was introduced:
(72) |
where
(73) |
In the last equation, is the diffusivity in water, and is the porosity of the biofilm. The formulation was made following the assumption that precipitates ”clog” the pores of the biofilm during their accumulation.
Since is a differentiable function, equation 72 can be rewritten as follows:
(74) |
where , , and
The boundary and initial conditions considered here are the same as those considered in with constant coefficients.
Note that this variable diffusivity does not affect the growth equation for biomass.
We are first interested in the homogeneous equation associated to 74 in the spirit of [26, 27, 28]:
(75) |
From [15] this equation has the following fundamental solution :
(76) |
where
(77) |
and
(78) |
We have the following properties of and adapted from ([28]):
(79) |
(80) |
(81) |
Instead of following the method proposed in [29, 28]; we will construct a new Green’s function as we did for the constant coefficients equation. Define
(82) |
By using the Green’s relation as equality as before on and including the boundary and initial conditions and using characteristics coordinates, we end up with the following integral equation:
In addition, we can show that satisfies 16. Then, we define as before.
(83) |
By using inequalities 79–81 we can prove propositions similar to lemmas 3 and 4 but we have to be careful because we don’t need a Neumann function such as the one defined in 11. In this way, we can prove the existence and uniqueness of the solution.
7 Conclusion and future works
We have presented in this paper a qualitative analysis of the biofilm model. The model takes into account the growth of the biofilm and the dynamics of the substrates in the biofilm.
The work mainly showed the existence and uniqueness of solution to this free boundary problem.
However, our system describing the growth of biofilm is not strictly hyperbolic due to a major simplification made on the model formulation. This simplification consists in assuming that the growth velocity is the same for all the biomass. But this is not the case in reality. Considering different growth velocities leads to a strictly hyperbolic system and this induces major changes in the study of the problem. Such considerations have never been taken into account and this comprises a long list of open problems.
In addition, we made strong regularity assumptions on the initial data and the boundary conditions. In some cases we can have functions that are not smooth enough and the existence and uniqueness criteria studied here are no longer valid.
In the case of variable diffusivity, we may have a coefficient which is not derivable, then the transition we made is not valid.
Additionally, we considered the Dirichlet boundary conditions to be ”given” but in general, this not the case. The boundary conditions are derived following a mass balance low following the inlet and outlet from the bioreactor. For this reason, we need a supplementary system of ODE which has additional complications in the study of the system.
Finally, in some works, the biofilms growth is modeled by a system of advection-diffusion-reaction equations. Combined with the diffusion equation, we have a completely new system whose solution may or not blow up.
Acknowledgements
This research has been supported by the European Union’s Horizon 2020 research and innovation programme under the Marie Sklodowska-Curie grant
agreement 861088.
Maria Rosaria Mattei acknowledges support from
the project PRIN 2022 titled Spectral reectance signature of colored subaerial biolms as an indicator of stone heritage susceptibility to biodeterioration, project code: 2022KTBX3M, CUP: E53D23010850006.
Luigi Frunzo
acknowledges support from the project PRIN 2022 titled
MOMENTA-Modelling complex biOlogical systeMs for biofuEl productioN and sTorAge: mathematics meets green industry, project code: 202248TY47, CUP: E53D23005430006.
This paper has been performed under the auspices of the G.N.F.M. of I.N.d.A.M.
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