In this paper, we present new homogenization results of a stochastic model for flow of a single-phase fluid through a partially fissured porous medium. The model is a double-porosity model with two flow fields, one associated with the system of fissures and the other associated with the porous system. This model is mathematically described by a system of nonlinear stochastic partial differential equations defined on perforated domain. The main tools to derive the homogenized stochastic model are the Nguetseng’s two-scale convergence, tightness of constructed probability measures, Prokhorov and Skorokhod compactness process and Minty’s monotonicity method.
A fissured or fractured medium is a material made up of permeable and porous blocks interwoven by a system of fissures, the porous blocks make up the matrix of the media. Fissured media are differentiated by the extent to which the system of fissures are developed within the medium. Bulk of the fluid transport takes place through the system of fissures while significant fluid storage occurs in the porous blocks.
Flow in fissured porous domains was first investigated by reservoir engineers in the petroleum industry because many petroleum reservoirs are in fractured rock formations made up of porous blocks of rocks surrounded by fractures. The blocks have low permeability but the porosity and consequently the storage capacity of fluids is high, which led to an overestimation in well production and capacity. Scientists and engineers have been studying this subject. Hence there are many articles and professional literature in multiple fields including hydrology, geology and environmental engineering.
There are certain characteristics of fissured media, namely, that transport occurs through the fissures while fluid storage occurs in the pore system. There are two cases of fissured media, the totally fissured media and the partially fissured media. In the case of a totally fissured medium, the matrix is assumed to be broken down into individual porous blocks by well developed system of fissures, resulting in no flow in the porous matrix and only through the system of fissures. In the case of a partially fissured medium, the system of fissures are less developed and the porous blocks may be connected, resulting in some amount of flow within the porous matrix. See Fig. 1.
An illustration of a partially fissured material.
A mathematical model that describes the flow of a fluid through a fissured porous medium domain can be stated for every point in the phase considered and on the matrix-fissure interface. This description is said to be at the microscopic scale. Due to the difficulty in measuring values of variables within a phase and determining the parameters of the model, a complete description of a model at the microscopic level is difficult and a solution to a said model is almost impossible. To bypass these difficulties, a macroscopic model is derived as the limit of the microscopic model, this process can be done using various homogenization methods, see for instance [9,15] (Chapter 9) and [29].
Fluid flows through fissured media as if it has two pore systems, one for the porous matrix and the other for the system of fissures, giving rise to the concept of double porosity. The flow of a fluid through totally fissured medium can be modeled using two flow fields, one representing the porous matrix and the other representing the system of fissures. These systems are coupled to form a system of equations over the flow domain, this type of model was introduced by Barenblatt, Zheltov and Kochina in [3]; see also [2,32].
Coeffield and Spagnuolo in [11] considered a model for single-phase flow through a totally fractured layered medium, where the fractures are horizontal and the matrix blocks are stacked vertically. The structure considered in [11] is assumed to be periodic only in one direction (vertically). In [12], Douglas, Peszyńska and Showalter extended the model for single phase flow in totally fissured media to that of a single phase fluid through periodic partially fissured media in the deterministic case; the model was constructed following [3,33] and the macroscopic model was derived using the method of asymptotic expansion. In the microscopic model for partially fissured medium in [12], there are two flows in the matrix; a global flow within the matrix and a flow that leads to local storage. The model for partially fissured media in [12] was extended by Clark and Showalter [10] to a quasi-linear version still in the deterministic case and the corresponding macroscopic model was derived using Nguetseng’s two-scale convergence. Nguetseng, Showalter and Woukeng [25] considered a general deterministic version of the problem in [12] beyond the periodic setting using Sigma convergence.
In geological formations, such as oil reservoirs, there are many factors that affect the flows within the domain, leading to uncertainties in estimating or predicting the flow in this type of formations which could lead to overestimates in well capacity. A stochastic process or random process is used to quantify uncertainties associated with physical or chemical processes since it provides a natural method for evaluating uncertainties. In [34], Wright reformulated the model in [12] for a randomly fissured media and used stochastic two-scale convergence in the mean (introduced by Bourgeat, Mikelić and himself in [6]) for the homogenization process. The homogenized problem obtained is a stochastic analog of the homogenized problem obtained in [12]. Here, we model the influence of random fluctuations on a single-phase flow through a random force driven by the Wiener process. This leads to the flow in the partially fissured media being governed by a system of stochastic partial differential equations (SPDEs) of nonlinear diffusion type involving oscillating coefficients. Since SPDEs are more advanced and more efficient tools in modelling random fluctuations on evolution systems arising in applied sciences, our model is naturally more elaborate than Wright’s in [34] which captures random influence through the random perturbation of the coefficient of a partial differential equation which does not involve random forces.
In this paper, we study the homogenization of a stochastic nonlinear evolution problem. We use the two-scale convergence together with Ito’s stochastic calculus and the probabilistic compactness process of Prokhorov and Skorokhod. For general account of homogenization of SPDEs, we refer to [19–23,31] and the references therein. In Section 2, we state the assumptions on the geometry of the partially fissured porous medium under consideration, some monotone operator properties including Browder–Minty theorem and the function spaces relevant to our study. In Section 3, we introduce the microscopic model and assumptions on the model. Section 4 contains the existence result of the governing stochastic diffusion equation and the a priori estimates for the solution of the equation. Section 5 is devoted to the tightness property for a family of probability measures linked to the sequence of the solution to the stochastic diffusion equation and the driving Wiener process, it also contains the Prokhorov and Skorokhod compactness procedure, see [5]. In Section 6, we prove the convergence of the microscopic problem to the macroscopic problem using Nguetseng’s two-scale convergence [1,24] and use Minty’s trick (monotonicity method) [14,17,18], to identify the weak limit. For more on Minty’s monotonicity method, we refer to [13].
Setting of the problem and preliminaries
Let us consider ϵ to be a positive parameter taking its values in a sequence which tends to zero and , a time interval with .
Let Q be a bounded domain in consisting of two sub-domains; one representing the fissures and the other representing the matrix.
Let denote the unit cell of measure consisting of two disjoint parts, and representing the local structure of the fissure and the matrix respectively. We let denote the characteristic function of for such that . We assume that the sets for are smooth, -periodic and extended to all of periodically.
For a given scale factor , the sub-domains and of Q represent the fissures and the matrix respectively with
Let us denote the interface of and lying within Q as and let be the interface in the representative cell Y, and we denote by the outer normal on for .
Functional spaces
We introduce some functional spaces needed throughout the paper. Let Q be an open bounded set in . We define as the closure of for the -norm.
For , we define the following spaces
equipped with the inner product
where , for .
We write
and
Let for be the usual trace map. We define the space
where with and and
is a Banach space equipped with the norm
Let X be a Banach space and be a probability space. For , the space is a probability space with filtration consisting of all stochastic processes such that is progressively measurable with respect to . is the corresponding mathematical expectation.
For , we endow this space with the norm
For , the norm in the space is given by
Minty’s trick
In this subsection we recall the classical result of Minty (Minty’s trick) [18]. This result will be used in Section 6 in the construction of the homogenized problem for a sequence of SPDEs involving monotone operators. For proofs of the results, we refer to [13,35].
Let X be a real, reflexive Banach space and its dual. Let us denote the inner product by for , .
A mapping is said to be bounded if it maps bounded subsets of X to bounded subsets of .
is continuous if ,
and E is hemicontinuous if the map
is continuous.
[Minty’s trick] Letbe monotone and hemicontinuous on a real Banach space X and letThen
The micro-model
Now we develop a microscopic model for a single phase flow in a partially fissured medium.
In the fissures , we shall denote the flow potential of the fluid by and its corresponding flux. On the matrix , we account for the global diffusion through the pore system in the matrix denoted by with flux and the very high frequency spatial variation which leads to local storage in the matrix which we shall denote by with flux . We specify two coefficients β and α which correspond to the proportion of the local and global phases of the total flow potential in the matrix as measured on the interface . Here, we take with and .
Let , (), we make the following assumptions;
is measurable and Y-periodic for every ,
is continuous for a.e. ,
there are positive constants k, C, , and such that for every and a.e. ;
,
,
.
Let for be given such that
For , we can define the corresponding scaled coefficient at , by
The micro-model for diffusion in a partially fissured medium driven by a random force is given by
where , . The first equation is the conservation of mass defined in the fissures, with representing the flow potential in the fissures. We have two components of flow potential in the matrix; represents the usual flow through the matrix and scaled by ϵ represents the very high frequency variation in the flow resulting from the relatively low permeability of the matrix, () is the intensity of the noise. These flows are assumed to satisfy corresponding conservation equations. () are mutually independent standard 1-dimensional Wiener processes defined on a given filtered probability space .
We assume that
for () and is such that () is uniformly bounded.
is a transmission problem of stochastic partial differential equations due to the prescribed transmission boundary conditions on the interface .
Recall that on the matrix , α and β denote the corresponding partitions for the flow potentials and respectively. The coupling on the interface is a vital element in the system. The continuity of the flow potential is represented in the first interface condition (the fourth relation in ), with prescribed partitions corresponding to the global and local phases in the matrix. The fifth and sixth relations describe the flux across the interface between the flow potential in the fissures and the total flow potential in the matrix. The external boundary conditions (on ) will play no role so we assume the following homogeneous Dirichlet boundary conditions;
with initial conditions
The aim of the paper is to show that the sequence converges in suitable topologies to the stochastic process which is a solution to the following SPDEs:
with initial conditions
where
and is an appropriate Wiener process which is the result of the Prokhorov–Skorokhod process.
Existence and uniqueness
We define the notion of solution of problem that is of interest to us.
For fixed , we define a strong probabilistic solution of problem as a stochastic process such that
.
For all , satisfies
For each, under assumptionsthere exists a unique solution of problemin the sense of Definition
4.1
.
Theorem 4.2 has essentially been proven by Pardoux in [27] and Krylov and Rozovskii in [16] using monotonicity method.
If we weaken the condition to the usual monotonicity condition i.e
for all , we lose uniqueness of the solution but the existence still holds in a weaker sense. Indeed Bensoussan established in [4] the existence of a weak probabilistic solution in the case of one equation involving monotone operators.
A priori estimates
We now establish essential a priori estimates for problem .
We assume that ϵ is a fixed positive number, under the assumptions, the solutionofsatisfies the following estimate;
Using Ito’s formula on the first equation of gives
Integrating by parts on the second term on the right hand side of (4.2) yields
using the identity , on we get
Ito’s formula on the second equation in gives
where we have used the relation on .
Lastly, Ito’s formula on the third equation on and the relation on gives
Summing (4.3), (4.4) and (4.5), we get
The boundary terms mutually cancel out thanks to the fifth and sixth relations in . Using in the resulting relation we have
Taking the supremum over followed by the expectation in both sides we get
Thanks to Burkhölder–Davis–Gundy inequality, Cauchy–Schwarz’s and Young’s inequalities, we get
where ϖ is an arbitrary positive number. Similarly,
and
For ϖ sufficiently small, we have
Based on the assumptions on , , and on , , we get
□
Next we establish a key estimate of the finite difference of in the dual of . It plays an important role in the implementation of the compactness result. It should be noted that such an estimate was not required in the deterministic case considered in [10].
Under the assumptions of Lemma
4.3
, the solutionof problemsatisfies the estimatefor any h such thatand.
Let , such that , we have
Since , we have on and the terms on cancel out due to the fifth and sixth relations in , so we get
Using assumption on the first two terms on the right hand side of (4.6) gives
Now we estimate the terms involving the stochastic term using the following embedding
and since both and are reflexive spaces, we have
Consequently,
where we have used (3.1) on the functions .
Estimating each term at a time, we have
For , using Hölder’s inequality and Fubini’s theorem we get
Recall that , using Burkhölder–Davis–Gundy’s inequality, we deduce that
By Hölder’s inequality and the assumption on i.e. , we get
Similarly,
and
Raising (4.7) to the power of , integrating over , taking the supremum, the expectation and using Lemma 4.3 gives
Similarly,
and
Hence collecting all the above inequalities, we assert that
□
One of the difficulties encountered in the homogenization of problems in perforated domain is to establish that the sequence of solutions admits a limit in the whole domain, in our case Q. From the estimates in Lemmas 4.3 and 4.4, we cannot extract a convergent subsequence by weak compactness, since each () is defined on a space which varies in ϵ.
As in [1], we will extend the functions by zero to the whole domain Q. The domain Q has two sub-domains representing the fissures and representing the matrix with , hence we can assert that the flow potential defined on equals zero on and the flow potentials , defined on are zero on .
We recall the characteristic function
We use this function to denote the extension by zero of various functions from to Q and to denote the extension of functions from to Y.
Now we state the estimates for the extension of to all of Q from , .
Let us still denote the zero extension of by , we state the estimate of the finite difference in the space
where we define as
Compactness result and tightness property
This section contains some results that are essential in the proof of the tightness property of the probability measures generated by the sequence , where and .
(Prokhorov).
A sequence of probability measuresonis tight if and only if it is relatively compact.
(Skorokhod).
Supposeis a separable Banach space withas it’s σ-algebra. Assume that the probability measuresonweakly converges to a probability measure μ. Then there exists random variablesdefined on a common probability spacesuch thatandandwherestands for the law of ·.
Let us consider the set Z depending on the sequences of numbers such that as and on the constants J, K, L, M, N, R. We define the set Z by
The set Z is a compact subset of.
The proof of this lemma is similar to the proof found in [4] (Proposition 3.1).
Let the space H be defined as
equipped with the inner product
Let and be equipped with the Borel σ-algebra . Let be the -valued measurable map defined on by
We introduce the probability measures on defined by
The family of probability measuresis tight in.
The proof is carried out following [4], see also [30] and [21,31].
By Prokhorov’s result, (Lemma 5.1), there exists a subsequence of and a probability measure π such that
Using Lemma 5.2 due to Skorokhod, there exists a probability space and -valued random variables and defined on such that the probability law of is and that of is π. Furthermore,
where , , , and .
and are Wiener processes on and the pair satisfies problem as stipulated in the following;
For anyand. The sequencesatisfies, the relationswith, in the sense of distributions.
Since satisfies the same type of problem as , we have the following corresponding estimates for ;
and on the dual we have,
where .
Homogenization process
In this section, we derive the homogenized problem using the two-scale convergence. We start by introducing some theorems that will be useful in the convergence process. For their proofs, we refer to [1,8].
Some results on two-scale convergence
The following results are the-time dependent version of some fundamental results on [8].
Letbe a bounded sequence of functions inwith. Then there exists subsequenceand a functionsuch thatis two-scale convergent to φ.
Letbe a sequence satisfying the assumptions of Theorem
6.1
. Furthermore, letbe bounded in. Then
there exists a subsequenceand a couple of functionswithandsuch that up to a subsequence,.
there exists a functionsuch that up to a subsequence,and.
Letbe a sequence of functions insuch thattwo-scale converges toin. Thenconverges weakly toin, whereFurthermore, we have
Passage to the limit
Now we study the asymptotic behaviour of as using the two-scale convergence method.
For the sequences, there exists subsequencessuch that, we have the following two-scale convergences,-almost surely:Furthermore, there exist some functions,, forsuch that the following convergences hold-almost surely;and
According to Lemma 4.3, the sequences and are bounded in and respectively. Since by definition, is zero in , and , is zero in , we have the estimates (4.8) and (5.3) for the subsequences , , .
By Theorem 6.2(1) and Theorem 2.9 in [1], we have the following two-scale convergences, -a.s.,
where and , for .
Using the same argument and Theorem 6.1, () and are bounded in . Hence, the subsequences two-scale converge to () and respectively in , -a.s.
Theorem 6.2(2) gives
Lastly, from , we have
Hence, by Theorem 6.1, () is bounded in , and similarly, is bounded in . Consequently, the sequences two-scale converge to () and -a.s., respectively with . □
Before we proceed with the homogenization process, we establish the conditions on the interface .
Let . Owing to the transmission conditions on in , we have
Thus
Hence, according to Lemma 6.4,
and
Let , we have
Taking the two-scale limits on both sides give
The left hand side of (6.1) can be written as
while the right hand side of (6.1) can be written as
From (6.1) we see that
Since and are periodic on , this implies that
Now we state our main result.
Suppose the assumptionsare satisfied. Then there exists a probability spaceand random variablesandsuch thatwhereandsuch thatis the solution of problemandsatisfies the homogenized problems (
3.4
), (
3.5
) and (
3.6
); recall that.
Let , , and , , with for .
We take the triple
in as a test function, where we define
Substituting these test functions in the weak formulation (5.2) of problem , we get
Let us determine the limit of each term in this relation using the two-scale result in Lemma 6.4.
For the first term on the left hand side we have,
The second term yields
Similarly, using the definitions of and taking the limit at on the remaining terms on the left hand side of (6.2) give ,
Taking the limit as in the first and second terms on the right hand side of (6.2), we obtain
Lastly, we deal with the limits of the last two terms on the right hand side of (6.2); which are stochastic integrals.
For the integral involving , we have
We start with the first term on the right hand side of (6.3). Since has unbounded variations, some care is needed. We first split the integral as
For the first term on the right hand side of (6.4), we adopt the process of regularization for with respect to t in the following form
where ρ is a standard mollifier.
Now we have that is differentiable with respect to t and satisfies the following relation
and
We write the first term on the right hand side of (6.4) as
Since is differentiable, we integrate by parts on the first term in the right hand side of (6.5) to get
The condition on and together with the convergence of to in -a.s., give that the right hand side of (6.6) is bounded by a positive number , where vanishes as ϵ tends to zero, while is finite.
Thanks to Burhölder–Davis Gundy inequality and the convergence of to , the second term on the right hand side of (6.5) is estimated as
where converge to zero as .
Hence from (6.5), we have
From (6.4), we conclude that
Passing to the limit as , we get
But since the left hand side of this relation is independent of λ, and as , we can pass to the limit on both sides as to get
By Lemma 6.4, we have the two-scale convergence of to -a.s., which implies weak convergence
Hence by using the convergence result for stochastic integrals in [28] (Theorem 4, pg 63), we get
Now we show that
With the assumptions of and Burkhölder–Davis–Gundy’s inequality, we have
Combining the above convergences, we assert that
Similarly,
and
Combining all the above convergences yield
let us decouple equation (6.7) by making specific choices of test functions , , , , .
Let be such that at and and choose such that for and . Then we get the following equation;
Integrating by parts with respect to t in the first and second terms on the left hand side and with respect to x on the seventh term gives
This is the weak formulation of the following macro-fissure equation;
Similarly, let and is such that at and and be such that , for Then we obtain the following
Integrating by parts with respect to t in the first and second terms on the left hand side and with respect to x on the seventh term gives
Since is arbitrary, we have that (6.10) is the weak formulation of the following macro-matrix equation;
Next, let and is such that at and on ., together with , on , we get the cell system
Integrating by parts with respect to t on the first and third terms on the left hand side gives
This is a weak formulation of the following the cell system;
Lastly, letting and , we obtain
which is weak formulation of the following system of equations;
We will have our homogenized problem when we have identified the terms , and .
Next we split (6.7) using special choices of test functions , , , , , in order to be able to use Ito’s formula.
In the first stage, we choose and , we have
Next we choose and , we have
Now we choose and , we have
Next we choose and , we have
Lastly, we choose and , we have
Ito’s formula on (6.15)–(6.17) at and adding (6.18) and (6.19) we get
Now we identify , , . For this we use Minty’s trick (Lemma 2.2) [18], see also [4] and [7]. Let and and for , we define the functions
Since and () arises from an admissible test function, we have the following two-scale convergence
by , we get
Expanding the above inequality yields
Recall that Ito’s formula on yields
Adding a suitable zero to (6.21) and using (6.22) gives
Recall that , and . We now take the limit as to get
where we omit the variable in order to avoid cumbersome writing.
We use (6.20) in (6.24) and replace by () to get
Now let us set where we take (). Using Proposition 6.3, the right hand side of (6.25) is nonnegative. Thus (6.25) becomes
Following Bensoussan’s argument in [4], first we divide the above equation by σ and then let to obtain
Hence owing to Minty’s trick (Lemma 2.2) [18] as implemented by Bensoussan in [4], we conclude that
We note that and are unique probabilistic weak solutions of the homogenized problems (3.4), (3.5) and (3.6). Thus by the infinite dimensional version of Yamada–Watanabe’s theorem (see [26]), we get that and are the unique strong solutions of (3.4), (3.5) and (3.6). Thus up to distribution (probability law) the whole sequence of solutions of converges to the solutions of (3.4), (3.5) and (3.6). This completes the proof of Theorem 6.5. □
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