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Research article

Analysis of travelling wave solutions for Eyring-Powell fluid formulated with a degenerate diffusivity and a Darcy-Forchheimer law

  • Received: 24 April 2022 Revised: 31 May 2022 Accepted: 06 June 2022 Published: 16 June 2022
  • MSC : 35B65, 35Q35

  • The goal of this paper is to provide analytical assessments to a fluid flowing in a porous medium with a non-linear diffusion linked to a degenerate diffusivity. The viscosity term is formulated with an Eyring-Powell law, together with a non-homogeneous diffusion typical of porous medium equations (as known in the theory of partial differential equations). Further, the equation is supplemented with an absorptive reaction term of Darcy-Forchheimer, commonly used to model flows in porous medium. The work starts by analyzing regularity, existence and uniqueness of solutions. Afterwards, the problem is transformed to study travelling wave kind of solutions. An asymptotic expansion is considered with a convergence criteria based on the geometric perturbation theory. Supported by this theory, there exists an exponential decaying rate in the travelling wave profile. Such exponential behaviour is validated with a numerical assessment. This is not a trivial result given the degenerate diffusivity induced by the non-linear diffusion of porous medium type and suggests the existence of regularity that can serve as a baseline to construct numerical or energetic approaches.

    Citation: José Luis Díaz Palencia, Saeed ur Rahman, Antonio Naranjo Redondo. Analysis of travelling wave solutions for Eyring-Powell fluid formulated with a degenerate diffusivity and a Darcy-Forchheimer law[J]. AIMS Mathematics, 2022, 7(8): 15212-15233. doi: 10.3934/math.2022834

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  • The goal of this paper is to provide analytical assessments to a fluid flowing in a porous medium with a non-linear diffusion linked to a degenerate diffusivity. The viscosity term is formulated with an Eyring-Powell law, together with a non-homogeneous diffusion typical of porous medium equations (as known in the theory of partial differential equations). Further, the equation is supplemented with an absorptive reaction term of Darcy-Forchheimer, commonly used to model flows in porous medium. The work starts by analyzing regularity, existence and uniqueness of solutions. Afterwards, the problem is transformed to study travelling wave kind of solutions. An asymptotic expansion is considered with a convergence criteria based on the geometric perturbation theory. Supported by this theory, there exists an exponential decaying rate in the travelling wave profile. Such exponential behaviour is validated with a numerical assessment. This is not a trivial result given the degenerate diffusivity induced by the non-linear diffusion of porous medium type and suggests the existence of regularity that can serve as a baseline to construct numerical or energetic approaches.



    K1: Permeability of the medium.

    K2: Inertial permeability.

    L: Fluid characteristic length.

    M: Hartmann number.

    MHD: Magnetohydrodynamics.

    PME: Porous Medium Equation.

    Re: Reynolds.

    U0: Fluid characteristic velocity.

    ρ: Fluid density.

    μ: Fluid viscosity.

    ν: Fluid kinematic viscosity.

    B0: Applied magnetic field.

    σ: Electrical conductivity in the medium.

    Any kind of material exhibiting pores filled by a flowing fluid leads to a physical interpretation beyond the Newtonian description related with viscosity and diffusion. Currently, flow in porous medium is a source of research, not only because of purely mathematical interests, but also because of their applications in electrochemical, mechanical, geophysical, metallurgical and chemical processes. In 1856, the observations made by Henry Darcy [1] associated to fluid flow in porous medium led to the formulation of a physical law to describe the basic dynamic experienced. Such law was intended to describe the fluid principles for low Reynolds numbers, typical of flows in this kind of porous medium. Afterwards, Forchheimer in 1901 [2] and Jaeger in 1956 [3] provided an extension of Darcy's law to account for turbulent flows at higher Reynolds numbers. Based on these works, the Darcy's law was renamed as Darcy-Forchheimer's law by Mustak in [4] and [5].

    It shall be noted that the above mentioned researchers considered the viscosity and diffusive terms as provided by the classical Newtonian description. Nonetheless and since then, several researchers have tried to extend the viscosity formulation to increase the modelling accuracy beyond the Newtonian scope. As a set of representative examples of the described non-Newtonian fluid models, the reader is referred to the works [6,7,8,9] together with references therein. The non-Newtonian fluids are classified into several classes. It is relevant to highlight that efforts have been made to describe diffusion phenomena based on the kinetic theory of liquids rather than on experimental or intuitive principles related with viscosity. Such efforts were conducted with success leading to a kind of non-Newtonian fluid known as Eyring-Powell. The use of the kinetic theory of liquids to describe viscosity and diffusive mechanisms makes the Eyring-Powell fluid particularly attractive to model flows given by electrically conducting particles arising in Magnetohydrodynamics (MHD). In a set of interesting analysis, Akbar et al. [10] obtained the numerical results for two dimensional MHD Erying-Powell fluid over stretching surface. Hina et al. [11] analyzed the heat transfer for MHD Erying-Powell fluid under the slip effect at the boundary. Bhatti et al. [12] considered two dimensional MHD Erying-Powell fluid under permeable surface and analyzed the heat transfer by converting the equations into nonlinear ordinary equations and that are solved based on numerical principles. Other interesting results in non-Newtonian fluids are given in the references [13,14,15,16,17,18], but particularly there are some recent achievements in this regards to highlight: In [19] a modified Eyring-Powell model is introduced to improve predictions related with the Eyring-Powell parameter on flow velocity. In [20], the authors discuss the adequacy of Eyring-Powell models for viscous dissipation in a flow past a convectively heated stretching sheet. Furthermore, in [21] and [22], an Eyring-Powell fluid is considered to model Coriolis effects over a non-uniform surfaces together with a discussion on the adequacy of the formulation. Finally, the reader is referred to [23] and [24] for discussions on other types of fluids and other types of analysis based on purely numerical schemes respectively.

    Other techniques have been of help to describe flows under non-Newtonian approaches. For instance, some kinds of solutions known as travelling and solitary waves have provided interesting results from analytical and numerical perspective. In this regard, the reader is referred to the set of studies [25,26,27].

    As a main research question driving the present study, it shall be mentioned the idea of searching for appropriate regularity conditions even when the Eyring-Powell viscosity term is formulated with a degenerate diffusion. Specially but not limited, the question of finding an exponential profile of solution.

    Let us start by considering a one dimensional Darcy-Forchheimer flow with a diffusion term given by an Erying-Powell principle. The velocity vector is then V=(v1,0,0) where v1(y,t) is the velocity profile in the xdirection that is dependant on the transversal direction y. The geometry under study is given by an open porous domain where the flow is developed through the xdirection and is initially distributed by an initial condition in the ydirection. In addition, the diffusion is further modified to account for a nonlinear term of the form 2vm1y2 (refer to [28] and [29] for a complete discussion about this kind of non-linearity and to [14,15,16] for different applications of particular diffusion terms). Note that the basic homogeneous problem

    v1t=2vm1y2,m>1, (1.1)

    is well known as porous medium equation. The PME is a nonlinear parabolic equation with degenerate diffusivity. Indeed, the diffusivity is given by D(v1)=mvm11 that is null whenever v1=0. This degeneracy leads to the loss of a positive principle for null (or slightly null) solutions, and hence to the loss of regularity as understood for gaussian diffusion problems.

    Based on the exposed principles, the equation under study emerges from the MHD theory and reads

    v1t=1ρdPdx+(ν+1βd1ρ)2vm1y212βd31ρ(v1y)22v1y2(σB20ρ+νK1)v1v21K2, (1.2)

    where m>1, P is the pressure field acting along the xdirection and β and d1 are the characteristic constants of the Eyring-Powell fluid model.

    To account for a single general equation, introduce the following non-dimensional quantities (see [30]) as follows

    v1=v1U0,x=xL,y=yL,t=U0tL,P=PρU20,A1=1νβρd1ϵ=12βρd31L3,A2=LνU0K1,A3=LK2,A4=Um10Re, (1.3)

    where L is a characteristic length that can be given by the pores dimension. After replacement of the set of expressions in (1.3) into the Eq (1.2) (ignoring * for simplicity)

    v1t=1ρdPdx+A4(1+A1)2vm1y2ϵ(v1y)22v1y2(M2Re+A2)v1A3v21, (1.4)

    where Re=U0Lν is the Reynolds number and and M=B0Lσρ refers to the Hartmann number. Making the differentiation of Eq (1.4) with respect to x

    1ρdPdx=A5.

    After using the value of dPdx in Eq (1.4)

    v1t=A5+A4(1+A1)2vm1y2ϵ(v1y)22v1y2(M2Re+A2)v1A3v21. (1.5)

    In addition, consider the following initial generalized condition

    v1(y,0)=v0(y)L1(R)L(R), (1.6)

    where v0(y) is the initial velocity that represents any kind of non-homogeneous distribution with the only requirement to be bounded in Lnorm and under a finite flowing mass quantity, i.e., a bound in L1norm. In addition, note that this initial condition allows modelling any kind of irregularities or discontinuities that may exist in the porous medium involved.

    Given the degeneracy in the diffusivity introduced by the non-linear term 2vm1y2 and given the generalized initial velocity distribution, solutions are analyzed based on a weak formulation. To this end, assume the existence of a test function ΩC(R) with compact support (or at least with a decreasing behaviour over R) such that for 0<τ<t<T

    Rv1(t)Ω(t)dy=Rv1(τ)Ω(τ)dy+tτRv1(t)Ωsdyds+A5tτRΩdyds+A4(1+A1)tτRvm12Ωy2dyds+ϵ3tτR(v1y)3Ωy(M2Re+A2)tτRv1ΩdydsA3tτRΩv21dyds. (2.1)

    Given a finite r0, admit the following ball Br centered in r0 and with radium r>>r0, such that the following equation is defined

    v1(t)Ωs+A5Ω+A4(1+A1)vm12Ωy2+ϵ3(v1y)3Ωy(M2Re+A2)v1ΩA3Ωv21=0, (2.2)

    in Br×[0,T], with the following boundary like and initial conditions

    0<Ωy=Ω<<1,v1(y,0)=v0(y)L1(R)L(R). (2.3)

    Firstly, the following theorem expresses the regularity properties of any solution to (1.5), i.e., solutions exist globally.

    Theorem 2.1. Given v0(y)L1(R)L(R), then any non-negative solution (v10) to (1.2) is bounded for all(y,t)Br×[0,T] with r>>1.

    Proof. Consider λR+, the following supporting cut-off function is defined as

    ψλC0,          0ψλ1,ψλ=1inBrλ,ψλ=0inRBrλ,

    such that

    |ψλλ|=Ccλ.

    Multiplying Eq (2.2) by ψλ and integrating over Br×[τ,T]

    tτBrv1Ωsψλdyds+A5tτRΩψλdyds=A4(1+A1)tτRvm12Ωy2ψλdydsϵ3tτR(v1y)3Ωyψ5dyds+(M2Re+A2)tτRv1Ωψλdyds+A3tτRΩv21ψλdyds. (2.4)

    Based on some results in [28] and [29], for some large r>>r0>1 the following holds

    tτv1dstτvm1dsC1(τ)r2mm1, (2.5)

    and

    tτv21dsC1(τ)r4. (2.6)

    Considering the spatial variable y close to Br, it can be assumed yr. Then

    tτ(v1y)3ds8m3m1C31(τ)r3m+3m1. (2.7)

    After using the expression (2.4) and after integration in the nonlinear diffusion term, the following holds

    A4(1+A1)tτBrvm12Ωy2ψλdydsA4(1+A1)C1(τ)r2mm1((Ωyψλ)BrBrΩyψλydyds).

    Since r>>1 and since Ω is sufficiently small and regular in the asymptotic approach, it is possible to choose Ω in such a way Ωyψλ<<1 in the proximity of the boundary Br. Then, the above expression becomes

    A4(1+A1)tτBrvm12Ωy2ψλdydsA4(1+A1)C1(τ)Brr2mm1ΩyψλydydsA4(1+A1)C1(τ)Brr2mm1Ωyψλydyds. (2.8)

    Based on (2.7), the following integral holds

    ϵ3Brtτ(v1y)3Ωyψλdyds8ϵm33(m1)3C31(τ)Brr3m+3m1Ωψλydy. (2.9)

    After using the expressions (2.5), (2.6), (2.8) and (2.9) into (2.4), the following holds

    tτBrv1Ωsψλdyds+A5tτRΩψλdydsA4(1+A1)C1(τ)Brr2mm1Ωyψλydy+8ϵm33(m1)3C31(τ)Brr3m+3m1Ωψλydy+(M2Re+A2)C1(τ)Brr2mm1Ωψλdy+A3C1(τ)Brr4ΩψλdyA4(1+A1)C1(τ)Brr2mm1ΩyCcλdy+8ϵm33(m1)3C31(τ)Brr3m+3m1ΩCcλdy+(M2Re+A2)C1(τ)Brr2mm1Ωψλdy+A3C1(τ)Brr4Ωψλdy,

    which implies that

    tτBrv1Ωsdyds+A5tτRΩdydsA4(1+A1)CcC1(τ)Brrm+1m1Ωydy+8ϵm33(m1)3CcC31(τ)Brr2m+4m1Ωdy+(M2Re+A2)C1(τ)Brr2mm1Ωdy+A3C1(τ)Brr4Ωdy. (2.10)

    Consider a test function ΩC(R) of the form

    Ω(r,s)=els(1+r2)α. (2.11)

    Choose α in a way that the expression (2.10) is convergent, therefore

    tτBrv1Ωsdyds+A5tτRΩdyds2A4(1+A1)CcC1(τ)Brelsr2m12αdy+8ϵm33(m1)3CcC31(τ)Brelsr2m+4m12αdy+(M2Re+A2)C1(τ)Brelsr2mm12αdy+A3C1(τ)Brelsr42αdy. (2.12)

    For convergence, take α>m+2m1 and r, so that the expression (2.12) becomes

    0tτBrv1Ωsdyds+A5tτRΩdydsΥ, (2.13)

    where Υ is a suitable value obtained for each Br and is sufficiently small for r; hence, a finite value of Υ holds. Note that Ω and v1 are not negative, then the integrals in the expression (2.13) are finite in τ<s<tT, which shows that the solution v1 is bounded in R×[0,T].

    Now, it is the aim to show additional regularity results, in particular that v1y is bounded.

    Theorem 2.2. Assume that v1(y) is a non-negative solution to Eq (1.5), then v1y is bounded for all(y,t)R×[0,T].

    Proof. Multiplying Eq (1.5) by v1 and applying integration by parts, the following holds

    12ddtR|v1|2dy=A5Rv1dymA4(1+A1)Rvm11(v1y)2dy+ϵ3R(v1y)4dy(M2Re+A2)Rv21dyA3Rv31dy,

    which implies that

    R(v1y)2[ϵ3(v1y)2mA4(1+A1)vm11]dy=12ddtR|v1|2dyA5Rv1dy+(M2Re+A2)Rv21+A3Rv31dy.

    Now, applying the integration done

    t0R(v1y)2[ϵ3(v1y)2mA4(1+A1)vm11]dyds=12R|v1|2dyR|v0(y)|2dyA5t0Rv1dyds+(M2Re+A2)t0Rv21dyds+A3Rv31dyds. (2.14)

    The Theorem 2.1 established the bound properties of non-negative solutions, as a consequence the right hand side of Eq (2.14) is bounded. Choose a finite bounding constant A5 such that

    t0R(v1y)2[ϵ3(v1y)2mA4(1+A1)vm11]dydsA5,

    leading to conclude on the bound of v1y.

    The degeneracy introduce by the non-linear diffusion term may lead to the loss of uniqueness of non-negative solutions. Hence, a result about uniqueness of solutions is required to be shown.

    Theorem 2.3. Let us consider two non-negative solutions to the Eq (1.5), v11(y,t) andv12(y,t). Then, if both solutions have the same initial distribution, uniqueness holds, i.e., v11(y,t)=v12(y,t).

    Proof. First of all, define a test function Ψ(y,t)C(QT), where QT=R×[0,T]. The weak formulations for both solutions v11 and v22 are given as

    Rv11(y,t)Ψ(y,t)dy=Rv11(y,0)Ψ(y,0)dy+t0Rv11Ψsdyds+A4(1+A1)t0Rvm112Ψy2dyds+A5t0RΨdydt+ϵ3t0R(v11y)4Ψydyds(M2Re+A2)t0Rv11ΨdydtA3t0Rv211Ψdydt, (2.15)

    and

    Rv12(y,t)Ψ(y,t)dy=Rv12(y,0)Ψ(y,0)dy+t0Rv12Ψsdyds+A4(1+A1)t0Rvm122Ψy2dyds+A5t0RΨdydt+ϵ3t0R(v12y)4Ψydyds(M2Re+A2)t0Rv12ΨdydtA3t0Rv212Ψdydt. (2.16)

    Assume v11v12. After substraction, the following holds

    R(v11v12)(y,t)Ψ(y,t)dy=t0R(v11v12)(y,t)Ψsdyds+A4(1+A1)t0R(vm11vm12)(y,t)2Ψy2dyds+ϵ3t0R((v11y)4(v12y)4)Ψydyds(M2Re+A2)t0R(v11v12)(y,t)Ψ(y,t)dydtA3t0R(v211v212)(y,t)Ψ(y,t)dydt. (2.17)

    For v11(y,t)>v12(y,t), the following holds

    vm11vm12mvm111(v11v12)mCm12(v11v12), (2.18)

    where C2=max(y,t)QT(v11). Now, consider

    ((v11y)4(v12y)4)=(v11yv12y)(v11y+v12y)((v11y)2+(v12y)2)C3(v11yv12y), (2.19)

    where C3 is a suitable bounding constant that can be defined supported by the regularity results shown in Theorem 2.2.

    Based on the expressions (2.18) and (2.19), the Eq (2.17) becomes

    R(v11v12)(y,t)Ψ(y,t)dy=t0R(v11v12)(y,t)Ψsdyds+(mCm12A4(1+A1)ϵC33)t0R(v11v12)(y,t)2Ψy2dyds(M2Re+A22A3C2)t0R(v11v12)(y,t)Ψdyds. (2.20)

    Assume the following smooth shape test function defined as

    Ψ(y,s)=eas(1+y2)γ1, (2.21)

    where γ1 can be chosen such that

    RΨ(y,t)dy<. (2.22)

    For simplicity

    RΨ(y,t)dy=1. (2.23)

    For |y|, the integral mass shall be null. Then, for R>>1

    ||y|R|Ψ(y,t)dy=0. (2.24)

    In the asymptotic approximation |y|

    |y|2γ1|y|0, (2.25)

    then

    γ1>12. (2.26)

    Now, define

    Rψ(y,s)dy=easR1(1+y2)γ1dy=easχ(y), (2.27)

    where

    χ(y)=y1(1+y2)γ1dy. (2.28)

    The integral (2.28) is finite under the condition for γ1 in (2.26).

    Now, differentiate (2.21) with respect to y, so that

    2Ψy2=4γ1(γ1+1)y2eas(1+y2)γ1+22γ1(1+y2)γ1+14γ1(γ1+1)eas(1+y2)γ1=4γ1(γ1+1)Ψ.

    After integration

    R2Ψy2C4(γ1)Ψ=C4(γ1)easχ(y),

    where C4(γ1)=4γ1(γ1+1).

    Now, the intention is to assess each of the integrals involved in the right hand side of Eq (2.20)

    t0R(v11v12)(y,t)Ψsdyds=at0R(v11v12)(y,t)Ψdydsat0R(v11v12)(y,t)Ψdydsasup|v11v12|χ(y)t0easds=asup|v11v12|χ(y)(1eas). (2.29)
    (mCm12A4(1+A1)ϵC33)t0R(v11v12)(y,t)2Ψy2dyds(mCm12A4(1+A1)ϵC33)sup|v11v12|C4(γ1)χ(y)t0RΨ(y,t)dyds=(mCm12A4(1+A1)ϵC33)sup|v11v12|C4(γ1)χ(y)t0easds=(mCm12A4(1+A1)ϵC33)sup|v11v12|C4(γ1)χ(y)(1eat), (2.30)

    and similarly

    (M2Re+A22A3C2)t0R(v11v12)(y,t)Ψdyds(M2Re+A22A3C2)sup|v11v12|χ(y)(1eat). (2.31)

    Combining the assessments in (2.29), (2.30) and (2.31) with the Eq (2.20), the following holds

    R(v11v12)(y,t)Ψ(y,t)dyasup|v11v12|χ(y)(1eas)+(mCm12A4(1+A1)ϵC33)sup|v11v12|C4(γ1)χ(y)(1eat)+(M2Re+A22A3C2)sup|v11v12|χ(y)(1eat). (2.32)

    Since |χ(y)|< and for t>0, with sup|v11v12|0

    R(v11v12)(y,t)Ψ(y,t)dy0,

    which implies that v11v12. This result contradicts the initial assumption v11v12. As a consequence, the only compatible result is to consider v11=v12, leading to conclude on solutions uniqueness.

    The travelling wave profiles of solutions are given as per the following definitions: v1(y,t)=k(ζ), where ζ=ya1t, a1 denotes travelling wave speed and the profile k:R(0,) belongs to L(R). The Eq (1.5) is then transformed in terms of the travelling wave profile as

    a1k=A5+A4(1+A1)(km) (3.1)

    Let us introduce the following new variables

    \begin{eqnarray} Y = k(\zeta){\rm{, }} \, \, \, \, \, Z = \left(k^{m}\right)', \end{eqnarray} (3.2)

    such that the Eq (3.1) can be analyzed in a phase space driven by the following set of equations

    \begin{eqnarray} Y'& = &\frac{1}{m}Y^{1-m}Z\\ Z'& = &\frac{m^{3}\left[-\frac{a_{1}}{m}Y^{1-m}Z +\frac{\epsilon(1-m)}{m^{3}}Y^{2-3m}Z^{3} -A_{5}+\left(\frac{M^{2}}{R_{e}}+A_{2}\right)Y +A_{3}Y^{2}\right]}{m^{3}+A_{4}\left(1+A_{1}\right)- \epsilon Y^{3-3m}Z^{2}}. \end{eqnarray} (3.3)

    Making Y' = 0 and Z' = 0 to determine the critical points, the following is obtained

    \begin{eqnarray} Y^{2}+\left(\frac{M^{2}}{A_{3}R_{e}}+\frac{A_{2}}{A_{3}}\right)Y -\frac{A_{5}}{A_{3}} = 0. \end{eqnarray} (3.4)

    with solutions

    \begin{eqnarray} Y_{1} = -\frac{1}{2}\left(\frac{M^{2}}{R_{e}}+\frac{A_{2}}{A_{3}}\right) +\frac{1}{2}\sqrt{\left(\frac{M^{2}}{A_{3}R_{e}}+\frac{A_{2}}{A_{3}}\right)^{2} +\frac{4A_{5}}{A_{3}}} \end{eqnarray} (3.5)

    and

    \begin{eqnarray} Y_{2} = -\frac{1}{2}\left(\frac{M^{2}}{R_{e}}+\frac{A_{2}}{A_{3}}\right) -\frac{1}{2}\sqrt{\left(\frac{M^{2}}{A_{3}R_{e}}+\frac{A_{2}}{A_{3}}\right)^{2} +\frac{4A_{5}}{A_{3}}}. \end{eqnarray} (3.6)

    Consequently, the system critical points are given by (Y_{1}, 0) and (Y_{2}, 0) . The next intention is to characterize such critical points together with the bundles of orbits in their proximity.

    The Geometric perturbation theory is used to show the asymptotic behavior of specifically defined manifolds in the proximity of the system critical points. Firstly, assume the following manifold I_0 defined as

    \begin{equation*} \begin{split} I_{0} = [ \, \, (Y,Z) \, \, / \, \, \, & Y' = \frac{1}{m}Y^{1-m}Z; \\& Z' = \frac{m^{3}\left[-\frac{a_{1}}{m}Y^{1-m}Z +\frac{\epsilon(1-m)}{m^{3}}Y^{2-3m}Z^{3} -A_{5}+\left(\frac{M^{2}}{R_{e}}+A_{2}\right)Y +A_{3}Y^{2}\right]}{m^{3}+A_{4}\left(1+A_{1}\right)- \epsilon Y^{3-3m}Z^{2}} \, \, ], \end{split} \end{equation*}

    with the system critical points (Y_{1}, 0) and (Y_{2}, 0).

    A perturbed manifold I_{\beta} close to I_{0} in the critical point (Y_{1}, 0) is defined as

    \begin{eqnarray} I_{\beta} = \left[(Y,Z) \, \, / \, \, Y' = \beta Z; \, \, Z' = C_{5}\beta\left(Y-Y_{2}\right)\right], \end{eqnarray} (3.7)

    where \beta denotes a perturbation parameter close to the equilibrium \left(Y_{1}, 0\right) and C_{5} is a suitable constant obtained after root factorization. For the coming assessments, assume Y_{3} = Y-Y_{2} .

    The intention is to apply the Fenichel invariant manifold theorem [31] as formulated in [32] and [33]. To this end, it shall be shown that I_{0} is a normally hyperbolic manifold, i.e., the eigenvalues associated to I_{0} in the linear frame proximal to the critical points, and transversal to the tangent space, have non-zero real part. This is shown based on the following equivalent linear flow associated to I_{\beta}.

    \begin{eqnarray*} \begin{bmatrix} Y'_{3}\\ Z' \end{bmatrix} = \begin{bmatrix} 0 & \beta\\ C_{5}\beta & 0 \end{bmatrix} \begin{bmatrix} Y_{3}\\ Z \end{bmatrix} . \end{eqnarray*}

    The related eigenvalues are both real. Consequently, I_{0} is a hyperbolic manifold. Now, it is shown that the manifold I_{\beta} is locally invariant under the flow (3.3), so that the manifold I_{0} can be shown as an asymptotic approach to I_{\beta}. For this basis, consider the functions

    \begin{eqnarray*} \psi^{I_0}& = & \frac{m^{3}\left[-\frac{a_{1}}{m}Y^{1-m}Z +\frac{\epsilon(1-m)}{m^{3}}Y^{2-3m}Z^{3} -A_{5}+\left(\frac{M^{2}}{R_{e}}+A_{2}\right)Y +A_{3}Y^{2}\right]}{m^{3}+A_{4}\left(1+A_{1}\right)- \epsilon Y^{3-3m}Z^{2}}, \\ \psi^{I_\beta}& = & C_{5}\beta Y_{3}, \end{eqnarray*}

    which are C^{i}\left(R\times\left[0, \delta_{1}\right]\right), \, i \geq 1 , in the proximity of the critical point \left(Y_{1}, 0\right). In this case, \delta_{1} is determined based on the following flows that are considered to be measurable a.e. in R

    \begin{eqnarray*} \left\|\psi^{I_{\beta}} -\psi^{I_{0}}\right\|\leq \left\| C_{5}\beta Y_{3} - \varepsilon_0 \right\|\leq C_{5}\beta \left\|Y_{3}\right\|\leq\delta_{1}\beta, \end{eqnarray*}

    where \varepsilon_0 is the infinitesimal distance between the critical point (Y_1, 0) and the flow \psi^{I_{0}} , which exists given the normal hyperbolic condition of I_0 . As the solutions have been shown to be bounded, it is possible to conclude on a finite \delta_{1} . So the distance between the manifolds holds the normal hyperbolic condition for \delta_{1}\in\left(0, \infty\right) and \beta sufficiently small in the proximity of the critical point \left(Y_{1}, 0\right).

    Now, consider a perturbed manifold I_{\gamma} associated to I_{0} , but for the critical point (Y_{2}, 0) and defined as

    \begin{eqnarray} I_{\gamma} = \left[Y,Z/Y' = \gamma Z; Z' = C_{6}\gamma\left(Y-Y_{1}\right)\right], \end{eqnarray} (3.8)

    where \gamma denotes a perturbation parameter in the proximity of the equilibrium \left(Y_{2}, 0\right) and C_{6} is a suitable constant obtained after root factorization. Suppose Y_{4} = Y-Y_{1} , then the following flow associated to I_{\gamma} is given by

    \begin{eqnarray*} \begin{bmatrix} Y'_{4}\\ Z' \end{bmatrix} = \begin{bmatrix} 0 & \gamma\\ C_{6}\gamma & 0 \end{bmatrix} \begin{bmatrix} Y_{4}\\ Z \end{bmatrix} . \end{eqnarray*}

    The associated eigenvalues are both real, leading to state that I_{0} is, indeed, a hyperbolic manifold. Now, it is shown that the manifold I_{\gamma} is locally invariant under the flow (3.3), so that the manifold I_{0} can be shown as an asymptotic approach to I_{\gamma}. For this basis consider the functions

    \begin{eqnarray*} \psi^{I_0}& = & \frac{m^{3}\left[-\frac{a_{1}}{m}Y^{1-m}Z +\frac{\epsilon(1-m)}{m^{3}}Y^{2-3m}Z^{3} -A_{5}+\left(\frac{M^{2}}{R_{e}}+A_{2}\right)Y +A_{3}Y^{2}\right]}{m^{3}+A_{4}\left(1+A_{1}\right)- \epsilon Y^{3-3m}Z^{2}}, \\ \psi^{I_\gamma}& = & C_{6}\gamma Y_{4}, \end{eqnarray*}

    which are C^{i}\left(R\times\left[0, \delta_{1}\right]\right), \, i \geq 1 , in the proximity of the critical point \left(Y_{2}, 0\right). In this case, \delta_{1} is determined based on the following flows that are considered to be measurable a.e. in R:

    \begin{eqnarray*} \left\|\psi^{I_{\gamma}} -\psi^{I_{0}}\right\|\leq \left\| C_{6}\gamma Y_{4} - \varepsilon_1 \right\|\leq C_{6}\gamma \left\|Y_{4}\right\|\leq\delta_{1}\beta, \end{eqnarray*}

    where \varepsilon_1 is the infinitesimal distance between the critical point (Y_2, 0) and the flow \psi^{I_{0}} , which exists given the normal hyperbolic condition of I_0 . As the solutions are bounded, \delta_{1} is finite. Hence, the distance between the manifolds holds the normal hyperbolic condition for \delta_{1}\in\left(0, \infty\right) and \gamma sufficiently small, in the proximity of the critical point \left(Y_{2}, 0\right).

    Since the manifold I_{0} has been shown to satisfy the normal hyperbolic condition under the flow (3.3), it is possible to obtain asymptotic profiles operating in the linearized flows I_\beta and I_\gamma .

    For this purpose, consider the Eq (3.3) such that a family of trajectories in the phase plane (Y, Z) can be obtained by

    \begin{eqnarray} \frac{dZ}{dY} = \frac{m^{4}\left[-\frac{a_{1}}{m}Y^{1-m}Z +\frac{\epsilon(1-m)}{m^{3}}Y^{2-3m}Z^{3} -A_{5}+\left(\frac{M^{2}}{R_{e}}+A_{2}\right)Y +A_{3}Y^{2}\right]}{Y^{1-m}Z\left[m^{3}+A_{4}\left(1+A_{1}\right)- \epsilon Y^{3-3m}Z^{2}\right]} = H(Y,Z).\\ \end{eqnarray} (3.9)

    For Y \gg 1 , the function H > 0 while for 0 < Y \ll 1, the function H < 0 . In addition, as the function H is singular for Z = 0 , a trajectory in the proximity of the critical condition (Y_{1}, 0) shall require

    \begin{eqnarray} -\frac{a_{1}}{m}Y_{1}^{1-m}Z_{1} +\frac{\epsilon(1-m)}{m^{3}}Y_{1}^{2-3m}Z_{1}^{3} -A_{5}+\left(\frac{M^{2}}{R_{e}}+A_{2}\right)Y_{1} +A_{3}Y_{1}^{2} = 0. \end{eqnarray} (3.10)

    After using the Eq (3.3) into Eq (3.10), the following holds

    \begin{eqnarray} \epsilon(1-m)\left(Y_{1}'\right)^{3} -a_{1}Y_{1}Y_{1}' -A_{5}Y_{1}+\left(\frac{M^{2}}{R_{e}}+A_{2}\right)Y_{1}^{2} +A_{3}Y_{1}^{3} = 0. \end{eqnarray} (3.11)

    Typically, the flow velocity in a porous medium permits the hypothesis U_0 \ll 1 . In addition, in the assumption of a sufficiently large characteristic length, L \gg 1 , the parameter \epsilon \ll 1 (see (1.3)) for typical fluid densities. As a consequence, such \epsilon is considered to construct a solution as an asymptotic expansion in terms of the mentioned parameter \epsilon , understood as a perturbation and as given in (1.3). The selection of this parameter permits to account for a physical nuisance as \epsilon is related with some of the constants involved in the fluid problem. Then, the following expansion holds for suitable regular functions Y_{1j}, \, j = 0, 1, 2...

    \begin{eqnarray} Y_{1} = Y_{10}+\epsilon Y_{11}+\epsilon^{2} Y_{12}+... \end{eqnarray} (3.12)

    After using (3.12) into (3.11), the following holds

    \begin{eqnarray} \epsilon(1-m)\left(Y_{10}'+\epsilon Y_{11}'+\epsilon^{2} Y_{12}'+...\right)^{3} & = &a_{1}\left(Y_{10}+\epsilon Y_{11}+\epsilon^{2} Y_{12}+...\right) \left(Y_{10}'+\epsilon Y_{11}'+\epsilon^{2} Y_{12}'+...\right)\\ &+&A_{5}\left(Y_{10}+\epsilon Y_{11}+\epsilon^{2} Y_{12}+...\right)\\ &-&\left(\frac{M^{2}}{R_{e}}+A_{2}\right)\left(Y_{10}+\epsilon Y_{11}+\epsilon^{2} Y_{12}+...\right)^{2}\\ &-&A_{3}\left(Y_{10}+\epsilon Y_{11}+\epsilon^{2} Y_{12}+...\right)^{3}. \end{eqnarray} (3.13)

    Comparing the terms of orders \epsilon^{0} and \epsilon^{1}

    \begin{eqnarray} Y_{10}' = -\frac{A_{5}}{a_{1}} +\left(\frac{M^{2}}{R_{e}a_{1}}+\frac{A_{2}}{a_{1}}\right)Y_{10} +\frac{A_{3}}{a_{1}}\left(Y_{10}\right)^{2}, \end{eqnarray} (3.14)

    and

    \begin{eqnarray} Y_{11}'+\left(\frac{Y_{10}'}{Y_{10}} +\frac{A_{5}}{a_{1}Y_{10}} -\frac{2M^{2}}{R_{e}a_{1}}+\frac{2A_{2}}{a_{1}}-\frac{3A_{3}Y_{10}}{a_{1}} \right)Y_{11} = \frac{(1-m)\left(Y_{10}'\right)^{3}}{a_{1}Y_{10}}. \end{eqnarray} (3.15)

    The standard resolution of (3.14) leads to

    \begin{eqnarray} Y_{10}& = &\frac{1}{1-e^{-\frac{2A_{3}b}{a_{1}}\zeta}} \Big[\left(\frac{M^{2}}{2A_{3}R_{e}}+\frac{A_{2}}{2A_{3}}\right) +\sqrt{\left(\frac{M^{2}}{2A_{3}R_{e}}+\frac{A_{2}}{2A_{3}}\right)^{2}+\frac{A_{5}}{A_{3}}}\\ &+&\left(\left(\frac{M^{2}}{2A_{3}R_{e}}+\frac{A_{2}}{2A_{3}}\right) -\sqrt{\left(\frac{M^{2}}{2A_{3}R_{e}}+\frac{A_{2}}{2A_{3}}\right)^{2}+\frac{A_{5}}{A_{3}}}\right) e^{-\frac{2A_{3}\sqrt{\left(\frac{M^{2}}{2A_{3}R_{e}}+\frac{A_{2}}{2A_{3}}\right)^{2}+\frac{A_{5}}{A_{3}}}}{a_{1}}\zeta}\Big].\\ \end{eqnarray} (3.16)

    Differentiate (3.16) to get

    \begin{eqnarray} Y_{10}'-\frac{\left(\frac{M^{2}}{A_{3}R_{e}} +\frac{A_{2}}{A_{3}}\right)\frac{2A_{3}\sqrt{\left(\frac{M^{2}}{2A_{3}R_{e}}+\frac{A_{2}}{2A_{3}}\right)^{2}+\frac{A_{5}}{A_{3}}}} {a_{1}}e^{-\frac{2A_{3}\sqrt{\left(\frac{M^{2}}{2A_{3}R_{e}}+\frac{A_{2}}{2A_{3}}\right)^{2}+\frac{A_{5}}{A_{3}}}}{a_{1}}\zeta}} {\left(1-e^{-\frac{2A_{3}\sqrt{\left(\frac{M^{2}}{2A_{3}R_{e}}+\frac{A_{2}}{2A_{3}}\right)^{2}+\frac{A_{5}}{A_{3}}}}{a_{1}}\zeta}\right)^{2}}. \end{eqnarray} (3.17)

    Upon substitution of (3.16) and (3.17) in (3.15), it holds

    \begin{eqnarray} Y_{11}'&+&\left[-\frac{2abe^{-b\zeta}}{\left(1-e^{-b\zeta}\right)\left(c+de^{-b\zeta}\right)} +\frac{A_{5}\left(1-e^{-b\zeta}\right)}{a_{1}\left(c+de^{-b\zeta}\right)} +f -\frac{3A_{3}\left(c+de^{-b\zeta}\right)}{a_{1}\left(1-e^{-b\zeta}\right)}\right]Y_{11}\\ & = &-\frac{(1-m)8a^{3}b^{3}e^{-3b\zeta}}{a_{1}\left(c+de^{-b\zeta}\right)\left( 1-e^{-b\zeta}\right)^{5}}, \end{eqnarray} (3.18)

    where a = \left(\frac{M^{2}}{2A_{3}R_{e}}+\frac{A_{2}}{2A_{3}}\right), \, \, \, \, \, \, b = \frac{2A_{3}\sqrt{\left(\frac{M^{2}}{2A_{3}R_{e}}+\frac{A_{2}}{2A_{3}}\right)^{2}+\frac{A_{5}}{A_{3}}}}{a_{1}}, \, \, \, \, \, \, \, c = \left(\frac{M^{2}}{2A_{3}R_{e}}+\frac{A_{2}}{2A_{3}}\right)+ \sqrt{\left(\frac{M^{2}}{2A_{3}R_{e}}+\frac{A_{2}}{2A_{3}}\right)^{2}+\frac{A_{5}}{A_{3}}}, \, \, \, \, \, \, d = \left(\frac{M^{2}}{2A_{3}R_{e}}+\frac{A_{2}}{2A_{3}}\right)- \sqrt{\left(\frac{M^{2}}{2A_{3}R_{e}}+\frac{A_{2}}{2A_{3}}\right)^{2}+\frac{A_{5}}{A_{3}}} \, \, and f = -\frac{2M^{2}}{R_{e}a_{1}}+\frac{2A_{2}}{a_{1}}.

    After solving the Eq (3.18)

    \begin{eqnarray} Y_{11} = \frac{\left(1-e^{-b\zeta}\right)^{C_{3}}} {\left(c+de^{-b\zeta}\right)^{C_{1}}e^{C_{2}\zeta}} \left[\frac{c^{C_{1}-1}e^{(C_{2}-1)\zeta}}{C_{2}-3} +\frac{c^{C_{1}}[cC_{3}+C_{1}d-d+5]e^{(C_{2}-b-3)\zeta}}{C_{2}-b-3}+...\right], \end{eqnarray} (3.19)

    where C_{1} = \frac{2a}{d-c}- \frac{2A_{3}A_{5}(c+d)}{a_{1}bcd} , C_{2} = \frac{A_{5}}{c}+\frac{3(2A_{3}a+a_{1}b)}{2a_{1}}+f and C_{3} = \frac{2a}{d-c}-\frac{12aA_{3}}{a_{1}^{2}b} .

    Introducing the expressions (3.16) and (3.19) into (3.12), the following holds

    \begin{eqnarray} Y_{1}& = &\frac{1}{1-e^{-\frac{2A_{3}b}{a_{1}}\zeta}} \Big[\left(\frac{M^{2}}{2A_{3}R_{e}}+\frac{A_{2}}{2A_{3}}\right) +\sqrt{\left(\frac{M^{2}}{2A_{3}R_{e}}+\frac{A_{2}}{2A_{3}}\right)^{2}+\frac{A_{5}}{A_{3}}}\\ &+&\left(\left(\frac{M^{2}}{2A_{3}R_{e}}+\frac{A_{2}}{2A_{3}}\right) -\sqrt{\left(\frac{M^{2}}{2A_{3}R_{e}}+\frac{A_{2}}{2A_{3}}\right)^{2}+\frac{A_{5}}{A_{3}}}\right) e^{-\frac{2A_{3}\sqrt{\left(\frac{M^{2}}{2A_{3}R_{e}}+\frac{A_{2}}{2A_{3}}\right)^{2}+\frac{A_{5}}{A_{3}}}}{a_{1}}\zeta}\Big].\\ &+&\frac{\epsilon\left(1-e^{-b\zeta}\right)^{C_{3}}} {\left(c+de^{-b\zeta}\right)^{C_{1}}e^{C_{2}\zeta}} \left[\frac{c^{C_{1}-1}e^{(C_{2}-1)\zeta}}{C_{2}-3} +\frac{c^{C_{1}}[cC_{3}+C_{1}d-d+5]e^{(C_{2}-b-3)\zeta}}{C_{2}-b-3}+...\right]+O(\epsilon^{2}),\\ \end{eqnarray} (3.20)

    which implies that

    \begin{eqnarray} &\,&v_{1}(y,t) = \frac{1}{1-e^{-\frac{2A_{3}b}{a_{1}}(y-a_{1}t)}} \Big[\left(\frac{M^{2}}{2A_{3}R_{e}}+\frac{A_{2}}{2A_{3}}\right) +\sqrt{\left(\frac{M^{2}}{2A_{3}R_{e}}+\frac{A_{2}}{2A_{3}}\right)^{2}+\frac{A_{5}}{A_{3}}}\\ &+&\left(\left(\frac{M^{2}}{2A_{3}R_{e}}+\frac{A_{2}}{2A_{3}}\right) -\sqrt{\left(\frac{M^{2}}{2A_{3}R_{e}}+\frac{A_{2}}{2A_{3}}\right)^{2}+\frac{A_{5}}{A_{3}}}\right) e^{-\frac{2A_{3}\sqrt{\left(\frac{M^{2}}{2A_{3}R_{e}}+\frac{A_{2}}{2A_{3}}\right)^{2}+\frac{A_{5}}{A_{3}}}}{a_{1}}(y-a_{1}t)}\Big]\\ &+&\frac{\epsilon\left(1-e^{-b(y-a_{1}t)}\right)^{C_{3}}} {\left(c+de^{-b(y-a_{1}t)}\right)^{C_{1}}e^{C_{2}(y-a_{1}t)}} \Big[\frac{c^{C_{1}-1}e^{(C_{2}-1)(y-a_{1}t)}}{C_{2}-3} +\frac{c^{C_{1}}[cC_{3}+C_{1}d-d+5]e^{(C_{2}-b-3)(y-a_{1}t)}}{C_{2}-b-3}\\ &+&...\Big] +O(\epsilon^{2}). \end{eqnarray} (3.21)

    The Eq (3.21) shows the existence of an exponential decaying under the travelling wave profile asymptotic expansion. This results is not trivial in this case given the degeneracy in the diffusivity under the non-linear diffusion of porous medium kind.

    Now, the intention is to show that the defined supporting manifold I_{\beta} preserves the exponential behavior shown in the proximity of the associated critical point. For this purpose, consider the expression (3.7), so that

    \begin{eqnarray} \frac{dZ}{dY} = \frac{C_{5}(Y-Y_{2})}{Z}. \end{eqnarray} (3.22)

    After solving (3.22)

    \begin{eqnarray} Z = -\sqrt{C_{5}}(Y-Y_{2}). \end{eqnarray} (3.23)

    Introducing the expression (3.7) into (3.23), the following holds

    \begin{eqnarray} Y' = -\beta\sqrt{C_{5}}(Y-Y_{2}), \end{eqnarray} (3.24)

    such that a solution is

    \begin{eqnarray} Y = Y_{2}+e^{-\beta\sqrt{C_{5}}\zeta}, \end{eqnarray} (3.25)

    which implies that

    \begin{eqnarray} v_{1}(y,t) = \frac{1}{2}\left(\frac{M^{2}}{R_{e}}+\frac{A_{2}}{A_{3}}\right) +\frac{1}{2}\sqrt{\left(\frac{M^{2}}{A_{3}R_{e}}+\frac{A_{2}}{A_{3}}\right)^{2} +\frac{4A_{5}}{A_{3}}}+e^{-\beta \sqrt {C_{5}}(y-a_{1}t)} \end{eqnarray} (3.26)

    This last expression shows the conservation of the exponential profile in the proximity of the critical point kept by the asymptotic manifold I_{\beta}.

    The existence and exact assessments of an orbit in the proximity of the critical point (Y_{2}, 0) follows the same procedure as discussed above for the point (Y_{1}, 0) . Indeed, a trajectory in the phase plane is given as

    \begin{eqnarray} \epsilon(1-m)\left(Y_{2}'\right)^{3} -a_{1}Y_{2}Y_{2}' -A_{5}Y_{2}+\left(\frac{M^{2}}{R_{e}}+A_{2}\right)Y_{2}^{2} +A_{3}Y_{2}^{3} = 0. \end{eqnarray} (3.27)

    Solving the Eq (3.27) leads to obtain

    \begin{eqnarray} Y_{2}& = &\frac{1}{1-e^{-\frac{2A_{3}b}{a_{1}}\zeta}} \Big[\left(\frac{M^{2}}{2A_{3}R_{e}}+\frac{A_{2}}{2A_{3}}\right) +\sqrt{\left(\frac{M^{2}}{2A_{3}R_{e}}+\frac{A_{2}}{2A_{3}}\right)^{2}+\frac{A_{5}}{A_{3}}}\\ &+&\left(\left(\frac{M^{2}}{2A_{3}R_{e}}+\frac{A_{2}}{2A_{3}}\right) -\sqrt{\left(\frac{M^{2}}{2A_{3}R_{e}}+\frac{A_{2}}{2A_{3}}\right)^{2}+\frac{A_{5}}{A_{3}}}\right) e^{-\frac{2A_{3}\sqrt{\left(\frac{M^{2}}{2A_{3}R_{e}}+\frac{A_{2}}{2A_{3}}\right)^{2}+\frac{A_{5}}{A_{3}}}}{a_{1}}\zeta}\Big] \\ &+&\frac{\epsilon\left(1-e^{-b\zeta}\right)^{C_{3}}} {\left(c+de^{-b\zeta}\right)^{C_{1}}e^{C_{2}\zeta}} \left[\frac{c^{C_{1}-1}e^{(C_{2}-1)\zeta}}{C_{2}-3} +\frac{c^{C_{1}}[cC_{3}+C_{1}d-d+5]e^{(C_{2}-b-3)\zeta}}{C_{2}-b-3}+...\right]+O(\epsilon^{2}),\\ \end{eqnarray} (3.28)

    where a = \left(\frac{M^{2}}{2A_{3}R_{e}}+\frac{A_{2}}{2A_{3}}\right), b = \frac{2A_{3}\sqrt{\left(\frac{M^{2}}{2A_{3}R_{e}}+\frac{A_{2}}{2A_{3}}\right)^{2}+\frac{A_{5}}{A_{3}}}}{a_{1}},

    c = \left(\frac{M^{2}}{2A_{3}R_{e}}+\frac{A_{2}}{2A_{3}}\right)+ \sqrt{\left(\frac{M^{2}}{2A_{3}R_{e}}+\frac{A_{2}}{2A_{3}}\right)^{2}+\frac{A_{5}}{A_{3}}},

    d = \left(\frac{M^{2}}{2A_{3}R_{e}}+\frac{A_{2}}{2A_{3}}\right)- \sqrt{\left(\frac{M^{2}}{2A_{3}R_{e}}+\frac{A_{2}}{2A_{3}}\right)^{2}+\frac{A_{5}}{A_{3}}} ,

    f = -\frac{2M^{2}}{R_{e}a_{1}}+\frac{2A_{2}}{a_{1}}, C_{1} = \frac{2a}{d-c}- \frac{2A_{3}A_{5}(c+d)}{a_{1}bcd} , C_{2} = \frac{A_{5}}{c}+\frac{3(2A_{3}a+a_{1}b)}{2a_{1}}+f and C_{3} = \frac{2a}{d-c}-\frac{12aA_{3}}{a_{1}^{2}b} .

    As a consequence, a solution is given by the following expression

    \begin{eqnarray} &&v_{1}(y,t) = \frac{1}{1-e^{-\frac{2A_{3}b}{a_{1}}(y-a_{1}t)}} \Big[\left(\frac{M^{2}}{2A_{3}R_{e}}+\frac{A_{2}}{2A_{3}}\right) +\sqrt{\left(\frac{M^{2}}{2A_{3}R_{e}}+\frac{A_{2}}{2A_{3}}\right)^{2}+\frac{A_{5}}{A_{3}}}\\ &+&\left(\left(\frac{M^{2}}{2A_{3}R_{e}}+\frac{A_{2}}{2A_{3}}\right) -\sqrt{\left(\frac{M^{2}}{2A_{3}R_{e}}+\frac{A_{2}}{2A_{3}}\right)^{2}+\frac{A_{5}}{A_{3}}}\right) e^{-\frac{2A_{3}\sqrt{\left(\frac{M^{2}}{2A_{3}R_{e}}+\frac{A_{2}}{2A_{3}}\right)^{2}+\frac{A_{5}}{A_{3}}}}{a_{1}}(y-a_{1}t)}\Big]\\ &+&\frac{\epsilon\left(1-e^{-b(y-a_{1}t)}\right)^{C_{3}}} {\left(c+de^{-b(y-a_{1}t)}\right)^{C_{1}}e^{C_{2}(y-a_{1}t)}} \Big[\frac{c^{C_{1}-1}e^{(C_{2}-1)(y-a_{1}t)}}{C_{2}-3} +\frac{c^{C_{1}}[cC_{3}+C_{1}d-d+5]e^{(C_{2}-b-3)(y-a_{1}t)}}{C_{2}-b-3}\\ &+&...\Big] +O(\epsilon^{2}). \end{eqnarray} (3.29)

    Again, the intention now is to show that the defined supporting manifold I_{\gamma} preserves the exponential behavior in the proximity of the critical point (Y_2, 0) . For this purpose, consider the expression (3.8) so that

    \begin{eqnarray} \frac{dZ}{dY} = \frac{C_{5}(Y-Y_{1})}{Z}. \end{eqnarray} (3.30)

    After solving (3.30), the following holds

    \begin{eqnarray} Z = -\sqrt{C_{5}}(Y-Y_{1}). \end{eqnarray} (3.31)

    Introducing the expression (3.8) into (3.31)

    \begin{eqnarray} Y_{1}' = -\gamma\sqrt{C_{6}}(Y-Y_{1}), \end{eqnarray} (3.32)

    such that a solution is given by

    \begin{eqnarray} Y = Y_{1}+e^{-\gamma\sqrt{C_{6}}\zeta}, \end{eqnarray} (3.33)

    which implies that

    \begin{eqnarray} v_{1}(y,t) = -\frac{1}{2}\left(\frac{M^{2}}{R_{e}}+\frac{A_{2}}{A_{3}}\right) +\frac{1}{2}\sqrt{\left(\frac{M^{2}}{A_{3}R_{e}}+\frac{A_{2}}{A_{3}}\right)^{2} +\frac{4A_{5}}{A_{3}}}+e^{-\gamma \sqrt {C_{6}}(y-a_{1}t)}. \end{eqnarray} (3.34)

    This last expression permits to show the conservation of the exponential profile in the proximity of the critical point under study by the asymptotic manifold I_{\gamma}.

    According to expressions (3.25) and (3.33), the analytical assessments have provided an exponential tail in the proximity of the system critical points. To validate the assessments, it is the intention to compare such analytical exponential tail with a numerical simulation of the Eq (2.1). Note that the numerical exploration is not intended to introduce a wide parametrical analysis with each of the involved fluid constants, on the contrary the objective is to provide evidences on the accuracy of the analytical process followed. In addition, for the validation exercise the expression (3.33) has been considered, under the form Y-Y_{1} = e^{-\gamma\sqrt{C_{6}}\zeta}. The numerical assessment is executed with the bvp4c in Matlab (refer to [34] for further details on this software tool).

    The R_e number has been considered as a free parameter to establish the accuracy of solutions. In addition, the following particular values in the other fluid constant have been considered for the sake of simplicity, but with no impact in the conclusions

    \begin{equation} 0 < A_5 \ll 1, U_0 = 1, A_1 = 1, 0 < \epsilon \ll 1, M = 1, \nu = 1, K_1 = 1, K_2 = 1. \end{equation} (4.1)

    Note that L = 1000 as the domain of integration has been considered as (-500,500) . This domain has been selected after some numerical trials and provides an efficient compromise between low impact of the collocation methods at the borders and a moderate computational time. In addition, the global absolute error allowed is of 10^{-4} .

    Note that the R_e in porous media is typically low, hence the considered values are R_e = 1; 100 .

    As it can be noticed from Figures 1 and 2, the analytical asymptotic solution (3.33) based on the geometric perturbation theory and the numerical solution to (2.1) fit an exponential behaviour with an order deficiency in the decreasing rate. Nonetheless, solutions are very close for increasing values of \zeta , this is in the asymptotic approach where the analytical solution has been obtained. This is not a trivial conclusion for the degenerate diffusion given in (2.1) and represents a finding to remark.

    Figure 1.  Solutions for Re = 1 . The left hand figure is a global representation. Both solutions preserves the exponential behaviour. The picture on the right represents a zoom in the interval [3, 5] . The reader can observe a certain order deficiency between the analytical and numerical assessments. Nonetheless, both solutions are close, the distance is of the order 10^{-7} .
    Figure 2.  Idem for R_e = 100 . For \zeta \geq 2 , the distance between the analytical and numerical solution is of order 10^{-4} .

    The set of assessments and discussions presented in this paper have provided evidences on the regularity of solutions to a kind of fluid flow with degenerate diffusivity and formulated with Darcy-Forchheimer porosity principles and Eyring-Powell viscosity terms. Afterwards, asymptotic travelling waves solutions have been explored based on a perturbation technique. Particularly, the Geometric Perturbation Theory has shown that an exponential decreasing rate holds even when the equation discussed presents a degenerate diffusivity. Furthermore, two linearized manifolds in the proximity of the critical points have been shown to hold and an exponential behaviour has been obtained accordingly. Eventually, a numerical exercise has been introduced to account for the validation of the analytical assessments done.

    The authors declare that there are not any conflict of interests.



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