Asymmetric Random Walk in a One-Dimensional Multi-Zone Environment
A.V. Nazarenko, V. Blavatska

TL;DR
This paper models a one-dimensional asymmetric random walk across multiple zones with fixed transition probabilities, deriving analytical solutions for the probability distribution and mean squared displacement, revealing transient anomalous diffusion.
Contribution
It introduces an analytical approach to asymmetric random walks in multi-zone environments, accounting for interface effects and validating with numerical simulations.
Findings
Derived probability distribution function considering diffusion and drift.
Identified transient anomalous diffusion behavior.
Validated analytical results with numerical simulations.
Abstract
We consider a random walk model in a one-dimensional environment, formed by several zones of finite width with the fixed transition probabilities. It is also assumed that the transitions to the left and right neighboring points have unequal probabilities. In continuous limit, we derive analytically the probability distribution function, which is mainly determined by a walker diffusion and drift and accounts perturbatively for interface effects between zones. It is used for computing the probability to find a walker in a given space-time point and the time dependence of the mean squared displacement of a walker, which reveals the transient anomalous diffusion. To justify our approach, the probability function is compared with the results of numerical simulations for a three-zone environment.
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ASYMMETRIC RANDOM WALK IN A ONE-DIMENSIONAL MULTI-ZONE ENVIRONMENT
A.V. Nazarenko
Bogolyubov Institute for Theoretical Physics of NAS of Ukraine,
4b, Metrologichna Str., Kyiv 03680, Ukraine
V. Blavatska
Institute for Condensed Matter Physics of NAS of Ukraine,
1, Svientsitskii Str., Lviv 79011, Ukraine
Abstract
We consider a random walk model in a one-dimensional environment, formed by several zones of finite width with the fixed transition probabilities. It is also assumed that the transitions to the left and right neighboring points have unequal probabilities. In continuous limit, we derive analytically the probability distribution function, which is mainly determined by a walker diffusion and drift and accounts perturbatively for interface effects between zones. It is used for computing the probability to find a walker in a given space-time point and the time dependence of the mean squared displacement of a walker, which reveals the transient anomalous diffusion. To justify our approach, the probability function is compared with the results of numerical simulations for a three-zone environment.
random walk, inhomogeneous environment, diffusion, advection
pacs:
05.40.Fb, 02.50.Ga
I Introduction
The present paper is devoted to a deeper study of a random walk (RW) in a one-dimensional inhomogeneous environment, consisting of zones with constant parameters. The base model is formulated in our previous work NaBla , where we have referred to a number of problems Ascher60 ; Lehner ; Gupta ; Tanner ; Percus ; BHMST ; NFJH ; Powels investigated before and influencing our motivation. We have tried there to apply an analytical approach for finding the probability distribution function (PDF) of a walker in heterogeneous environment.
Here, we supply the RW model by seating an attractor/repulsor at the root point, which serves as a source of external field. Its presence determines the preferable directions of a walk and leads therefore to emergence of inequality (asymmetry) between probabilities of transition to the left and to the right.
Our investigations are stimulated by the RW models application in the majority of fields like polymer physics, economics, computer sciences RWbook . Besides it, RW is often used as simple mathematical formulation of diffusion process. Moreover, the RW in inhomogeneous environment is of great interest because of its connection with transport phenomena in fractures and porous rocks, diffusion of particles in gels, colloidal solutions and biological cells (see, e.g., Havlin87 for a review).
Thus, we formulate here the RW in -zone environment, located along coordinate axis and symmetric under coordinate sign inversion. The transition probability is assumed to be varying within the different zones and unequal for the left and right steps.
This model is engaged to describe, for instance, the linear chaotic structures, passing through the finite number of zones with viscous properties in external field. Imagining for a moment a few-dimensional problem, these may be polymer chains crossing the cellular membranes MGCh . Applying an analytical approach, we take a possibility here to evaluate the mean squared end-to-end distance in a one dimension.
We can also suppose the model applicability to a study of chaotic particle dynamics with barriers, which are associated with various matter sorts or (static) properties of space itself. Our goal is to derive also the probability as a function of space-time, which is accounting for transition between zones due to diffusion and advection.
In principal, we have no preference for the treatments and investigate the general properties. We are interested in finding new effects and functions in comparison with NaBla , approaching our model step by step to realistic situations which can be considered elsewhere.
Analytically, we are aiming to reduce the problem in continuous limit to finding a PDF from differential equation with a diffusion coefficient and a drift velocity, which inherit the established step-like space dependence. Further, a space-time evolution might be characterized by the averages, which are found by means of PDF and allow us to compare the properties of similar models with various parameters. We would like also to demonstrate a strong dependence of the meaningful quantities on attractive or repulsive character of the starting point. In particular, it is predicted a steady state existence when the diffusion and the advection are equilibrated.
As it is already shown in NaBla , there is a possibility to compare the derived probability function to find a walker in a given point of space-time with the result extracted from numerical simulations on the lattice. We test here these functions in the case of three-zone environment too.
Technically, a time dependence of the mean squared displacement does not look easily computable. Then, we neglect the interface effects, but account accurately for the bulk ones. This simplification is justified by studies, performed without advection (drift) in NaBla . There, the time asymptotic of the variance corresponds to uniform model, while the multi-zone structure of environment leads to emergence of transient anomalous diffusion at finite time. These phenomena are investigated here in the drift presence.
The layout of the paper is as follows. In the next Section, we fix the random walk rules and obtain the differential equation for PDF. An approximate PDF is found in Section 3. The probability function is calculated analytically in Section 4 and is compared with the numerical simulations performed. After computing the mean squared displacement in Section 5, we end up with giving discussion and outlook.
II Asymmetric RW in -Zone Environment
We start with a lattice RW model, considered as a Markov process with either zeroth or unitary step in space after successive unitary step in time. The walk is determined here by stationary transition probability defined as
[TABLE]
where is implied for a fixed ; is the Kronecker symbol.
Functions and determine probabilities to find a walker at points and if it was at in a previous time instant, respectively; corresponds to probability of adhesion (adsorption) Gupta . In general, , are regarded as arbitrary non-negative functions less than the half of unit.
Let sequence of positive numbers,
[TABLE]
define the separation points of environment zones in space .
Reproducing the same configuration for negative by inverting , we introduce the characteristic functions of zones : for , to obtain always the arithmetic mean of the left and right-handed functions at separation points, and otherwise. To make use these in differential calculus, are written as the distributions:
[TABLE]
Here is the Heaviside function.
The functions are orthogonal:
[TABLE]
Given the basis, we further introduce constant parameters , where defines the diffusion coefficient of -th zone; is a measure of probability asymmetry and plays a role of external field. Supposing the drift velocity dependence on both attractor strength and zone properties, we define -th zone velocity as .
Thus, we consider the asymmetric RW in heterogeneous environment with the following rules:
[TABLE]
where .
To preserve a probability meaning of functions and , we require .
The rules (6) allow us to simulate immediately the random trajectories for various sets , which we analyze here analytically.
Physically, definition of leads to a common and finite time of advection residence in a whole space. Therefore, the -th zone advection length and the diffusion length give us the Peclet number Pat for all . Thus, the both processes are tantamount at obeying as usual. At larger , the advection becomes dominant.
Although we give a common analytical description at and , these cases physically differ because of repulsive or attractive role of the origin, where velocity sign is inverted due to . Scenario with accords with the presence of a single attractor at , while the case of admits an existence of two attractors at , which produce two particle flows, moving in opposite directions.
The Markovian evolution of the probability distribution function (PDF) , so that , can be given by master equation with arbitrary distance and time between successive steps as
[TABLE]
To obtain a differential equation at large , (7) is expanded into the Taylor series up to the order . Omitting the rest terms, the lattice parameters are fixed to give constant scales and of the drift velocity and diffusivity, respectively.
Further, defining the functions for all ,
[TABLE]
we arrive in continuous limit at differential equation of RW in diffusion approximation:
[TABLE]
Differentiating, we can use where the prime means derivative with respect to coordinate NaBla .
Note also that for , and in general.
Evolving in space-time, the PDF defines the normalized statistical measure for a fixed :
[TABLE]
which is used for computing the averages.
III Finding a PDF
To find a PDF, we follow NaBla and concentrate the geometrical data in the new coordinate
[TABLE]
Note that the derivatives of are singular, in general, at the points .
Integrating (11), we obtain ,
[TABLE]
We also define the functions :
[TABLE]
here and .
Then, introducing the probability distribution , we re-write statistical measure as
[TABLE]
Substituting the re-defined into (9), we arrive at equation:
[TABLE]
where constant controls an interface effect between zones; .
Reformulating the model in the terms of , is regarded as a global velocity, which takes the opposite signs in two infinite intervals of : and .
The right hand side of (15) can be reduced to the form with and . Computations performed lead to the expression:
[TABLE]
A sign of is defined by difference , although the form of can vary.
We substitute now a formal series in :
[TABLE]
where
[TABLE]
is a basic and normalized solution to (15) at .
It is instructive to compare the fundamental solution with analytical solutions to the advection-diffusion equation under other conditions from recent works GPSG ; KJK ; Singh .
Remaining problem is to examine the surface effect induced by , which disappears in the homogeneous environment.
In general, each term is determined by divergence with a point-like carrier in the right-hand side of (15) and, therefore, results in
[TABLE]
what preserves the normalization. This integral statistically means that is fluctuating and a sign alternating function of space. Its magnitude is not suppressed by factor , and the probability may fall down to negative value. Although the series (17) allows us to calculate all of in a simple way, appropriate resummation is still needed.
Nevertheless, we compute here the first-order term from inhomogeneous equation
[TABLE]
contracting with to obtain
[TABLE]
where ; .
Performing an integration, one has
[TABLE]
Limiting ourselves by accounting for the first-order correction, we obtain our main result for PDF:
[TABLE]
where .
At the vanishing , this reproduces the result of NaBla and describes the ordinary RW at for all , when and .
If for two neighboring zones, the interface points become regular, and (24) welds these zones automatically.
Note that the correction by looks improper at because it has no static limit at large . Although the diffusion in an attractor presence at has to be a relaxation process leading to a steady state distribution and preventing a collapse due to chaotic motion. Taking and () in (24), one obtains
[TABLE]
It results in the limiting value of the variance at as we shall see. Thus, the PDF (24) is applicable to the models with at .
Considering the case of , the surface term is relevant at because is of the same order of magnitude as . As the result, Fig. 1 demonstrates two peaks of PDF, tending to escape in opposite directions to infinity with increasing . However, the speeds of peak motion for two sets of parameters look different because of a different damping, caused by adhesion.
Note finally that Eq. (15) can be transformed into the potential form by excluding the term .
IV The Probability Function
Using the PDF, let us compute the probability of walker manifestation at a given space-time point,
[TABLE]
that is the frequency of visiting a point in a time .
Integrating, results in
[TABLE]
Computing the total probability, we arrive at
[TABLE]
where the first-order term in is determined by
[TABLE]
We test our formulas by comparing with outcomes of numerical simulations. Data are presented in Fig. 2 and Fig. 3, putting respectively and , as it was argued above. Indeed, the bulk analytical solution is justified by RW simulation in three-zone environment. However, we hope that the accounting for the series in or its finite part, at least, will permit us to reproduce better the considerable changes of the probability profile at short .
The difference between peak heights obtained analytically and numerically at is independent on approximation in and can be also explained by the feature of our formalism, describing mainly a walker behavior in the bulk .
At , we see actually coincidence of three probability functions inside zones: numerical one, at , and at .
On the other hand, we observe in Fig. 2 the widening of probability profile in comparison with one of NaBla at for the same environment parameters. Comparing, we also note the growing peaks of probability in Fig. 2a which correspond to the zone with . It turns out that the attractors presence causes the pumping effect, which depends on the local adsorption (determined by ) and is already revealed in the leading order ().
V Variance Computing in the Leading Order
Variance is important RW characteristic, denoted here as
[TABLE]
In our approach, one has ,
[TABLE]
We focus on the properties of , corresponding to the leading order approximation.
Although the function can be presented similarly to (12), it is convenient to substitute it in terms of characteristic functions . We find that
[TABLE]
where numeric coefficients are
[TABLE]
Note that coincides with diffusivity .
Combining the environment parameters and time-dependent integrals, we write
[TABLE]
where functions ,
[TABLE]
determine the integrals for positive (or ):
[TABLE]
Questioning on behavior of at large , the answers turn out to be sufficiently different for the models with and , respectively. We can see that Fig. 4a shows an existence of equilibrium and static limit at , while Fig. 4b indicates the ballistic regime for with at . Moreover, the environment structure, given by the different sets of parameters , does not affect these tendencies.
Assuming an attractor presence at () and taking in (38), one has
[TABLE]
It follows that the maximum values of for models in Fig. 4a are and , when and , respectively. Thus, points lie inside the first zone for both models.
Focusing on the case of , a time asymptotic of is determined by the term containing at . Thus, at . This formula is valid, when the PDF peaks are far from region of the basic environment structure presence (see Fig. 1). Thus, we arrive at the asymptotic values of in Fig. 4b: and .
We would like to note that the velocity correlator reproduces here the typical properties of at from NaBla for the same environment parameters . We observe similarity in a sign alternating at small for the model with , while the regime is preserved during the whole evolution for the model with .
Note that the ’s sign allows us to classify a system behavior. Stages with correspond, as usual, to superdiffusion. On the other hand, the regime with reveals the transient subdiffusion, caused by particle capture for a short time by zones with relatively small .
Thus, the adsorption effect of each zone, determined by , lasts important at , although a magnitude and time intervals of ’s variations depend on . Moreover, the models with give rise a possibility to investigate the influence of the distant zones in comparison with the models at during the same time . On contrary, the case of does not allow here to overstep actually the first zone.
VI Discussion
We consider an asymmetric RW model in a one-dimensional space, densely covered by the finite-sized zones , , with the properties specified, what allows us to investigate an affect of inhomogeneities in chaotic systems of a different nature. Although a number of the RW characteristics can be extracted from numerical simulations, a deeper analysis requires an analytical description which is based in continuous limit on the advection-diffusion equation at the large total number of steps , associated with a time.
Our model, initially formulated in the terms of probabilities, is designed also to include the familiar problems of RW with various barriers Ascher60 ; Lehner ; Gupta ; Tanner ; Percus ; BHMST ; NFJH into the concept of the heterogeneous environment. At this time, these stimulate us by their predictions, methods and the unsolvable problems there.
Diffusion and advection are main and competing processes which we account for. Their parameters (diffusion coefficients and drift velocities ), varying from zone to zone, permit to reveal also an adsorption in the bulk (determined by ) and an action of long range external field . Sometimes, the latter notions are convenient for physical treatment of the observed phenomena.
Widening the model understanding, we can also relate the diffusion coefficient to an effective walker mass for each zone. Then, thinking about macroscopic particle ensemble, the mass variations might be interpreted as the result of geometrically dependent interaction among particles which is not specified here but leads to the emergence of different states, confined within the zones.
Before summarizing the results, we note briefly a role of advection, which contributes the directed motion into RW and is induced by a global asymmetry parameter , determining the preference between the left and right directions.
Precisely, the advection is involved here by means of the space-dependent velocity , where makes the RW root point to play an attractive or repulsive role, depended on the ’s sign. The case of means that the point attracts a walker. On contrary, at , we have a repulsor at , sending a walker from there in one of mutually opposite directions of axis .
Technically, such a definition preserves the model symmetry under coordinate inversion and leads to for any .
Thus, the diffusion and advection processes under our assumptions on the environment piece-wise structure determine a probability to find a walker at space-time point. Finding a probability distribution function (PDF) from the advection-diffusion differential equation, the parameter constancy almost everywhere looks as a crucial condition of the problem solvability. Indeed, the geometrical data are easily concentrated in new spatial variable what leads to equation for homogeneous environment with the singular terms, corresponding to the residual interface effects and containing the Dirac -function and its derivatives. Although this contradicts to a probabilistic meaning of the quantities involved, it is a sequel of using the distributions in continuous limit. The lattice RW simulations have no singularities. However, a receipt of obtaining a PDF by accounting for the interface contribution has to be found yet. It may be resolved exactly by constructing the solutions with a gap Powels which are not considered here.
To obtain a PDF, we use a formal series in a switching parameter , controlling the surface effects in equation. The leading term by gives us a basic and normalized solution for the bulk, which is equal in the terms of to the fundamental solution of homogeneous system. Nevertheless, the resulting PDF of reflects an environment complexity and the drift presence. We have also found a solution with the surface correction by , which is applicable at and as shown. We should use additional restrictions to limit the correction magnitude, which is not suppressed by .
Although such an approach is already exploited and justified by numerical simulations in NaBla without drift, the advection inclusion changes considerably the system dynamics and the PDF form, resulting in new outcomes.
To describe analytically the RW, we also compute the probability function in the linear approximation in and the variance dependence on in the leading order, neglecting the interface term.
For any , we reveal the variance time asymptotic:
[TABLE]
This tendency is independent on the environment structure with and also happens for uniform models as is already known.
However, an environment complexity leads at finite to effective power law with intermediate values of exponent , indicating a transient anomalous diffusion. It is clearly seen at .
Showing it, we appeal to the models with a three-zone environment, given by the parameter sets from NaBla . Furthermore, it is convenient to study the diffusion regimes by means of the velocity autocorrelation function
[TABLE]
Then, super/sub-diffusion processes correspond to , respectively. Using that, such time intervals are found in Fig. 4b.
It is important to note that for fixed set indicates a similar (anomalous) behavior at and (see NaBla ). Although a possibility to observe an affect of distant zones at is higher than at for the same .
Comparing the probability profiles at and (see NaBla ), we can see that the adsorption property of zones is intensified in the advection presence (see Fig. 2). Such a pumping effect looks surprisingly because the advection and the diffusion are competing.
At negative values of one has the PDF relaxation to a steady state distribution when . Although a walker is attracted to the origin , diffusion prevents a collapse with . However, there is no manifestation of all zones.
Note finally that a perspective is analytical description of the model with independent local velocities , extending the parameter set up to . Formalism, accounting for local fluctuations of smooth-varied diffusivity , where , could be developed.
Authors are indebted for partial support of this work by Department of Physics and Astronomy of NAS of Ukraine.
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