Abstract
P-adic numbers serve as the simplest ultrametric model for the tree-like structures arising in various physical and biological phenomena. Recently p-adic dynamical equations started to be applied to geophysics, to model propagation of fluids (oil, water, and oil-in-water and water-in-oil emulsion) in capillary networks in porous random media. In particular, a p-adic analog of the Navier–Stokes equation was derived starting with a system of differential equations respecting the hierarchic structure of a capillary tree. In this paper, using the Schauder fixed point theorem together with the wavelet functions, we extend the study of the solvability of a p-adic field analog of the Navier–Stokes equation derived from a system of hierarchic equations for fluid flow in a capillary network in porous medium. This equation describes propagation of fluid’s flow through Geo-conduits, consisting of the mixture of fractures (as well as fracture’s corridors) and capillary networks, detected by seismic as joint wave/mass conducts. Furthermore, applying the Adomian decomposition method we formulate the solution of the p-adic analog of the Navier–Stokes equation in term of series in general form. This solution may help researchers to come closer and find more facts, taking into consideration the scaling, hierarchies, and formal derivations, imprinted from the analogous aspects of the real world phenomena.
Keywords:
tree-like geometry; capillary networks; p-adic model of porous medium; fluid’s propagation; complex geological phenomena; p-adic analog of Navier–Stokes equation; pseudo-differential equations; p-adic wavelet basis; Schauder fixed point theorem; Vladimirov’s operator; existence of solution 1. Introduction
The last decades have witnessed great use of Fourier and more generally wavelet analysis over the p-adic fields, and its various physical applications in physics, biology and cognitive science, and recently in geophysics. The keyword of these applications is “hierarchy”. These applications are based on representation of hierarchies by tree-like geometry. Hierarchy is also a natural attribute of ultrametric spaces which mathematically can be represented as a duality between ultrametric (non-Archimedean) spaces and trees of balls in these spaces where mathematical tools such as integral and series are frequently used (see also [1,2]). Thus, ultrametric (non-Archimedean) spaces play the crucial role in aforementioned applications. The simplest ultrametric spaces are given by homogeneous trees, m-adic trees, where is a natural number encoding the number of branches leaving each vertex of the tree. If is a prime number, such ultrametric spaces can be endowed with the algebraic structure of a number field (addition, subtraction, multiplication, and division) that is denoted as the field of p-adic numbers (Each number represents a branch of the p-adic tree. In the mathematical model, branches are infinite. Of course, trees in nature, e.g., capillary networks in random porous media, are finite. They are obtained as cutoffs of p-adic trees represented by ). This algebraic structure in combination with the ultrametric topology on serve as the basis for analysis that have some similarity and a lot of dissimilarity with the real analysis (see, e.g., Escassut [3,4]).
The p-adic numbers were first applied in theoretical physics in an effort to solve one of the most remarkable problems of modern physics, that of combining quantum mechanics and gravitation theory. Hence it was conjectured in [5,6] that space-time geometry is non-Archimedean at Planck magnitudes ( cm). Regarding with diverse applications of the field of p-adic numbers several later papers including applicable contents have been published, e.g., [7,8,9,10,11,12,13,14,15,16,17,18,19,20,21]. These applications in turn motivated the pure mathematicians to develop the new areas of p-adic analysis, containing p-adic wavelet theory (see, e.g., [22,23,24,25,26,27,28,29,30,31,32,33,34,35,36,37,38,39,40,41,42,43]).
In this paper, the solvability of the p-adic analog of the Navier–Stokes equation via the wavelet theory is discussed by the example of real world problem: the precise modeling of fluid flow in highly heterogeneous, multiscale, and anisotropic porous media with strongly hierarchical architecture. This problem is recognized among key technical challenges of Petroleum Industry looking for new analytical solutions of classical mathematical analogue and new type of computing perspectives, more closed to the pure science. The continuous interaction among rock, fluid, and flow properties, result in dynamics of the geometry of mass transfer and waves routes, especially their continuity and tortuosity, affected by strong mixture of a complex geological phenomena: tectonics, salt tectonics, carbonatation, fluid dynamics, including the turbulence. The joint physical, petrophysical, geological, and mathematical modeling in these conditions require the new typing of pores. In spite of classical pores division in families of fractures, vughs and micropores, we propose their joint typing as fluid/waves conduits, resulting from the complex mixture of different from the geological point of view, elemental flow units. The tree-like geometry of these multi-sized conduits can be described with high precision by p-adic numbers, which not only encode the scaling of real porous media space distribution, but also provide the modeling of fluid flow with industry-leading quality and resolution. This work is our new attempt to ensure the solvability of the p-adic analogue of Navier–Stakes equation via wavelet tools for real porous media. The further model, combining the p-adic analogue of conduits with multifractal modeling of flow and transport thorough these geometrically complex and strongly no lineal networks, just on the road. Under the general assumption of the thermodynamical nature of multifractal systems, we conclude that our trans-disciplinary approach is the example of the real world demands of the future of the Era of Big Data and Entropy, the Queen of the Unified Physical, Geological, Numerical and, in general, Mathematical analogical modeling.
Considering the historic remarks of this applied field, the cooperation between the research groups of K. Oleschko (applied geophysics and petroleum research) and A. Khrennikov (p-adic mathematical physics) led to initiating a new promising field of research [35,36,37,38]: p-adic and more generally ultrametric modeling of the dynamics of flows (of, e.g., water, oil, and oil-in-water and water-in-oil emulsion) in capillary networks in porous random media. The starting point of this project is the observation that tree-like capillary networks are very common geological structures, especially in carbonates (see Figure 1 and Figure 2). The latter serves as rock base of oil-reservoirs. Fluids propagate through such trees of capillaries, so it is useful to reduce the configuration space to these tree-like structures and the appropriate mathematical model of such a configuration space is defined by an ultrametric space.
Figure 1.
(a). The general view of Isosurface Cube constructed from the unfiltered seismic waves amplitudes, distributed across the oil reservoir. The tree-like signature of Geo-conduits is especially clear in the down part of the original image and is zoomed in on (b). The main question is to show that the same connected and tortuous Geo-conduits, which conducted the seismic waves, are also the guides of mass (oil) transfer in fractured reservoir of complex and unconventional architecture.
Figure 2.
The effective metric for Geo-conduits patterns measurement was constructed by distribution of three sized balls within seismic cube.
In 2017, Oleschko et al. [38] focused the p-adic dynamics described by fractional differential operators (Vladimirov operators) starting with discrete dynamics based on hierarchically-structured interactions between the fluids’ volumes concentrated at different levels of the percolation tree and coming to the multiscale universal topology of the percolating nets. They presented a system of dynamical equations reflecting the tree structure of a capillary network in porous media and then derived the following nonlinear p-adic pseudo-differential equation for fluid’s velocity along capillaries:
where is the viscosity parameter with the initial condition This equation can be considered as the p-adic analogue of the Navier–Stokes equation. We stress that this is just an analog of the Navier–Stokes equation. The tree-like configuration space differs crucially from the real space of hydrodynamics and this difference is reflected in dynamical equations. In particular, u is a real scalar and not a real vector with three coordinates as in the Navier–Stokes equation in the Euclidean space, see Section 3 for details. Alternative nonlinear term in p-adic analogue of the Navier–Stokes equation was considered in paper of Kozyrev [39]. Moreover, the mathematical theory of such equations has not yet been developed. Very recently, Khrennikov and Kochubei [43] investigated the local solvability of Equation (1) using the von Wahl’s theorem for the case as the source term vanishes.
In the present paper, inspired by [43], our attention will be turned exclusively to study the solvability of Equation (1) using the technique of wavelet basis and a well-known fixed point theorem. Theory of p-adic wavelets was initiated by Kozyrev [11] and it found numerous applications (see, e.g., [2,12,13,35]), including modeling of fluid propagation in capillary networks in random disordered medium [36,37,38]. In Section 4, under certain conditions we study the solvability of an infinite system which is derived from (1) (with wavelet expansion of solution) in the sequence space . In Section 5, we employ a numerical method, the so-called Adomian decomposition method (ADM), to formulate the solution of Equation (1) represented by series.
This paper demonstrates that, for fluids’ propagation through capillary networks in porous disordered media, p-adic linear models developed and investigated in our previous works [35,36] can be successfully generalized (at the mathematical level of rigorousness) to nonlinear phenomena.
2. Geophysics: From Fractal to Tree-Like Models
The starting point of our research was fractal/multifractal modeling in geophysics [44,45]. The detailed presentation on such an approach can be found in Section 1.1 of our paper [36]. Here we briefly point to the most important moments. The fractal/multifractal scaling features of capillary networks was studied (both theoretically and experimentally) since the early 1980s and 1990s [46,47]: for invasion percolation, diffusion-limited aggregation (DLA), anti-DLA processes [48].
Later fractal modeling of fluids’ flows in porous random media [49], including transport through tree-like networks and diffusion on fractals [50] was widely used in oil recovery studies [51]. This modeling was supported by theoretical and experimental studies demonstrating that fluid’s flow through tree-like networks is faster [52,53].
Stanley and Meakin [46] have discussed the important thermodynamics aspects of multifractality in physics and chemistry, founding the formal analogy among the probability distribution function and partition function Therefore, the analogy between the Legendre transform and entropy H, as well as between the function and energy E was found. These analogies are the key points for physics of fractal capillaries patterns treelike morphology. The difference in the medium heterogeneity can be quantified by several multifractal indicators (for instance, the degree of the graph symmetry or strength of singularity).
Thus, fractal/multifractal studies led to an understanding of the importance of tree-like structures in mathematical modeling of fluids’ flows through capillary networks in porous disordered media.
4. Mathematical Preliminaries
In this section, we recall some auxiliary facts concerned with p-adic fields and wavelet theory. In view of the Ostrovski theorem (see [6], Ch. I, § 1.1), there exists, in some sense, only two “universes” of equal status: the real universe and the p-adic one. The real “universe” is structured by the field of real numbers , which is introduced by the completion of the field of rational numbers with relevance to the usual Euclidean norm, and the p-adic “universe” is based on the field of p-adic numbers, which is given as the completion of the field with respect to the p-adic norm . This norm is defined as below. ; if an arbitrary rational number is represented as uniquely, where and are not divisible by p then . This norm satisfies the following properties:
- (i)
- for every , and if and only if
- (ii)
- for every ;
- (iii)
- for every , and when , we have .
The condition (iii) as the strong triangle inequality makes the norm non-Archimedean and hence the space is an ultrametric space.
We shall systematically utilize the notation and results from [6]. Denote by the sets of positive integers, integers, and complex numbers, respectively.
Any p-adic number , , is represented in the canonical form as follows
where , and The series converges in the p-adic norm to , that is, . Hence, the absolute value takes the discrete set of nonzero values , for . The fractional part of a p-adic number given by (2) is defined as
The additive character of the field is given by
The topology equipped with in are known by
as balls and spheres of radius with center at a, respectively. It is worth mentioning that any point of the ball is its center, besides, any two balls in are either disjoint or one is included in the other. Furthermore, all balls and spheres are simultaneously open and closed sets in . For the certain case, the unit ball is the ring of p-adic integers consisting of the elements represented by the sum of p mutually disjoint balls.
The topological group is locally compact commutative and thus there is a additive Haar measure , which is positive and invariant under the translation, i.e., . This measure is unique by normalizing so that
Regarding with the additive normalized character on we get
where is the characteristic function of the segment .
A complex-valued function f in is said to be a locally constant function if for any , there exists an integer such that , for every . The largest of these numbers, , is called the parameter of constancy of the function We denote the space of locally constant functions on by . Indicate by the space of Bruhat–Schwartz test functions, i.e., the subspace of including compactly supported functions. Moreover, denote by the set of all linear functionals on (see also ([6], VI.3)).
The Fourier transform of test function is given by the formula
This means and as the inverse Fourier transform.
Consider as the set of measurable -valued functions f on such that
which is evidently a Hilbert space with the inner product
and
This guarantees a linear isomorphism taking onto . It can be uniquely extended to a linear isomorphism of . Moreover, the Plancherel equality holds
4.1. p-Adic Wavelet Theory
Throughout this section, we gather some facts related with the theory of p-adic wavelets which is widely employed in so many applications. It is now hard to find an area of engineering where wavelets are not applied. In 1910, Haar [58] initially presented the wavelet basis by an orthonormal basis in including dyadic translations and dilations of a single function; since then various generalizations of it have been revealed in several results. It is interesting to know that it took almost a century to create another wavelet function whose shifts and dilations would bring an orthogonal basis. The intensive progression in wavelet theory initiated only in the 1990s. At that moment Meyer [59] and Mallat [60,61] improved a scheme of structure for wavelet functions based on the concept of multiresolution analysis (MRA); see, for instance, [62], Ch. 5, [63], § 2.1.
Regarding with the theory of p-adic wavelets, it has a short background in comparison with that in the real status. In 2002, Kozyrev [11] found a compactly supported p-adic wavelet basis, similar to the real Haar basis, for . Kozyrev’s wavelet functions have the following structure:
where and are the standard additive character of and characteristic function of , respectively.
This wavelet basis (created by the shifts and dilations of the wavelet functions (4)) contains of the wavelet functions
where , , and n is taken as an element of the m-direct product of factor group
That is, n belongs to
4.2. Vladimirov’s Operator and p-Adic Lizorkin Spaces
Introduced by V.S. Vladimirov [6], pseudo-differential operator A (on the field of p-adic numbers) in an open set is given by
which acts on -valued functions of p-adic arguments Here we assume that functions are extended by zero from the set on whole space , and are their Fourier transforms recalled previously. The function is called symbol of the operator
In [64,65] Lizorkin presented spaces invariant under the real actions of fractional operators. These spaces can be defined in p-adic case. In view of [25,66], the p-adic Lizorkin space of test functions is described as follows:
such that
Clearly, . Regarding the fact that Fourier transform is a linear isomorphism into , one can see that . The space can be decorated with the topology of the space , which turns it into a complete space. The space can be determined by the following characterization:
if and only if and
In addition, the space as the topological dual of is said to be the Lizorkin space of p-adic distributions (see also [25]).
The Vladimirov operator (initially introduced by Taibleson) also is included in the class (6) with symbol , i.e.,
where The formula (7) can be rewritten as a convolution of the following functions:
where the distribution is called the Riesz kernel given by
and is the -function (for more details see [6]).
The domain of is given by
We remark that all the concepts as above can be reconsidered in multidimensional p-adic field which is not in our considerations in the current paper.
6. Solvability of Infinite System (12) over the Sequence Space
Let us first convert the infinite system of differential equations (12) into the following infinite system of integral equations
The existence theory concerning the infinite systems of integral equations is satisfactorily developed up to now and we are interested in study the system (14) in the Banach sequence space containing sequences of real numbers converging to zero. We recall that is a closed subspace of as the space of convergent sequences. It turns out this space is very convenient and natural for investigations of infinite systems both differential and integral equations. In what follows, we proceed our study in the Banach space including of real sequences converging to zero with the standard norm for . Note that the index has been altered following our notation and the subjected problem.
In the following we intend to apply the generalized theorem of Arzéla (see also [68]) which describes a criterion of compactness in the space for the arbitrary interval I and the Banach space E.
Theorem 1.
A bounded subset U of the space is relatively compact if and only if all functions belonging to U are equicontinuous on I and the set is relatively compact in E for each .
It is worth mentioning that a bounded subset U of is relatively compact if and only if
Suppose that and the interval for is given. To investigate the solvability of nonlinear pseudo-differential Equation (1) it only needs to focus on the existence of from the system (14). To do this, let us first present the following well-known fixed point result.
In what follows, system (14) will be investigated under the following hypotheses.
- (i)
- The functions are given on the set and take real values (). Further, the operator is defined on the space in the following way:which maps the space into and is such that the class of all functions is equicontinuous at every point of the space .
- (ii)
- There exist nonnegative functions and defined, integrable and uniformly bounded on I and such that . Furthermore, the function sequence converges monotonically to zero at each point while the function sequence is non-increasing at each point and the following estimate is satisfied:for each , and for each .
- (iii)
- The functions are continuous on I and the sequence converges monotonically to zero at each point .
In the following we recall the well-known Schauder fixed point theorem which is crucial to present our result.
Theorem 2
(Schauder Fixed Point Theorem ([69], [Theorem 4.1.1])). Let U be a nonempty and convex subset of a normed space E. Let T be a continuous mapping of U into a compact set . Then T has a fixed point.
Now we can formulate our main result.
Theorem 3.
Under the assumptions (i)-(iii), the infinite system (14) has at least one solution such that for each .
Proof.
Indicate by the subset of space including all functions so that
for and , where ≤ in index is the usual partial order in and , are defined in the following way:
for .
Remark that the functions and are nondecreasing functions on the interval I and non-increasing sequences. Besides, from the assumptions, it follows that the functional sequences and converge uniformly on I to the function vanishing identically on I.
Let us assume the operator defined on the space as follows:
Notice that the operator maps the set into itself. Indeed, fix arbitrarily ı and . Then for , we get
Now we prove that the operator is continuous on the set .
Consider arbitrarily fixed and . Then, taking into account the equicontinuity of the family of functions revealed in assumption (i) let us take , i.e., for such that we derive for each . Moving forward,
which implies the desired claim.
Now, let us take the set . Recall that this set contains equicontinuous functions on I. In fact, taking an arbitrary , and bringing in mind our hypotheses, we conclude
Since the function sequences , and are uniformly bounded on I and the function sequence is equicontinuous on I, from the above estimation, we conclude that the set is equicontinuous on I.
Suppose that stands for (i.e., the closed convex hull of the set ). Clearly, is closed, bounded, and equicontinuous on I. Furthermore, .
From another point of view, for , we get
Since the sequence converges uniformly on I to the function vanishing identically on I, we conclude that for each , there exists an index such that for each and for any Therefore, by virtue of the criterion of compactness in the space as mentioned before, we infer that for each , the set is relatively compact in the space . The above arguments allow us to deduce that the set is relatively compact in the space . Besides, the closedness of yields that it is compact. Hence, keeping in mind that transforms continuously the set into itself, we result (by the Schauder fixed-point principle) that the operator has a fixed point in the set being a solution of our problem. This completes the proof. □
Remark 1.
In Theorem 3, if for some
then one can easily utilize the Banach contraction principle and find the unique solution for the subjected system.
Theorem 3 implies the following result immediately.
7. Adomian Decomposition Method (ADM)
In this section we give standard description of the ADM to find the solution of Equation (1) in which we proved its existence in the last section. Consider the general equation
where u is the function subjected to be found, is the linear differential operator of higher order which is simply invertible. Suppose that its inverse is and it will be an integral operator, N is the nonlinear operator, R is the remaining linear part and g is a given function (source). Taking to both sides of (16) we get:
hence,
where is chosen from the initial conditions or from the boundary conditions or both, it depends on how we select differential operator that solve the given problem. The ADM considers that solution u of the functional equation can be decomposed into infinite series
and the nonlinear term can be expressed as infinite series where the ’s are the Adomian polynomials, which depend upon . We recall that the Adomian polynomials ’s are first constructed by Adomian in 1992, he gave a general formula to determine the values of ’s:
Therefore, Equation (16) takes the following form:
Now from Equation (17), we can derive the solution algorithm as follows:
Given , the other terms of u can be defined, respectively. Hence, the existing solution u of Equation (16) can be determined by the series of recursive sequence . To do this, let us rewrite the nonlinear differential Equation (13) as below
Assuming , and applying ADM we obtain
where would be specified by the initial condition in (8). Moreover, the convergence of Adomian’s decomposition method is discussed in the Appendix A.
Since we have no information about the form of and the initial condition of the problem (1), we present a model to see how ADM works.
Example 1.
In Equation (1), let us suppose the non-homogeneity term and the initial condition which is the refinable function.
To formulate the function G in terms of basis , using the symbol we arrive at
For the case we get
and, otherwise, for the case , we have
On the other hand,
where and . Considering for some integer together with the fact that if and only for some , we obtain
If then
Otherwise, for the case , using the fact that
we see that
On the other hand, looking at (11) one can see that
where
Hence,
Now, we are ready to apply ADM as follows.
The first three terms of ’s are
We recall that the ADM is analogous to find the Taylor’s series expansion for the nonlinear function around the initial function . Following this way and finding the Adomian polynomials , from (21) we get the solution as form of Moreover, using the value of as initial value, the constant ϕ would be determined.
8. Concluding Remarks
The use of tree-like (ultrametric) geometry is the promising direction in modeling of fluids’ transport through capillary networks in porous disordered media. Such geometry approximates fractal (and multi-fractal) structures in Geo-conduits.
Theory of linear dynamical equations (especially, p-adic) is well developed and its application to geophysics (see [36]) did not demand essential mathematical efforts. However, as well as in Euclidean geophysical modeling, the basic ultrametric dynamical equations are nonlinear. One of such equations, an analog of the Navier–Stokes equation, was derived in recent paper [38]. Its study posed a variety of new problems. This study is especially complicated in the absence of the general theory of nonlinear (pseudo-)differential equations on p-adic spaces; just the first steps in this direction were done in articles [37,43]. The present paper is the important step towards establishing theory p-adic Navier–Stokes equation.
Fractal and multifractal mathematical models are widely used for diagnostic of hydrocarbon-reservoirs stratigraphic patterns anisotropy (see, e.g., [44,45]). The concrete “on field applications” are based on software; one of the promising complexes of diagnostic programs was developed by the research group of K. Oleschko. This complex was actively used in realization of the projects for Mexican oil-industry, e.g., the project SENER-CONACYT-Hidrocarburos, Yacimiento petrolero como un reactor fractal. Development of ultrametric models for oil transport plays the important role in mathematical justification of application of (multi-)fractal models for Mexican Petroleum Industry.
Author Contributions
Funding
This paper was financially supported by the project SENER-CONACYT-Hidrocarburos, Yacimiento Petrolero como un Reactor Fractal, No. 168638, and by the Consejo Nacional de Ciencia y Tecnología (CONACYT), Mexico, under grant 312-2015, Fronteras de la Ciencia.
Acknowledgments
The authors would like to thank all researchers participated in software design, especially to Edith Perrier and Thibault Rieutord (France), Ana Tarquis (CEIGRAM, Spain), whose very first versions of algorithms for fractal and multifractal analysis for non-stationarity time series, ensure the final software quality.
Conflicts of Interest
The authors declare no conflict of interest.
Appendix A. (Convergence of Adomian’s Decomposition Method)
The convergence of ADM has been investigated by various authors. One significant fact is that the series solution of Adomian’s decomposition technique often converges very fast to the exact solution, if there is only one, and to one of the solutions, if several exist, tending the general term of the series solution to zero very fast, as , for m terms and the qth order of the linear operator L (see [66,70]).
Suppose the Hilbert space defined by the set of applications
In Equation (16) let us consider the operator be hemicontinuous and satisfy the following hypothesis:
- (a)
- (b)
If the above assumptions are fulfilled, the Adomian’s method is convergent (see [71,72,73]). Replacing , the following are sufficient conditions of convergence of ADM to the Equation (19),
- (c)
- (d)
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