Hall and Magnetic Field Effects on Peristaltic Transport through a Porous Medium of a Jeffery Fluid in a Channel Soliman R. El Koumy, El Sayed I. Barakat, Sara I. Abdelsalam* Abstract In this article, peristaltic motion induced by a sinusoidal traveling wave in the flexible walls of a two-dimensional channel occupied by an incompressible, viscous and electrically-conducting Jeffery fluid through a porous medium in the presence of a constant magnetic field, has been investigated taking into consideration the Hall effect. The problem is formulated using a perturbation expansion ( to the second order ) in terms of the small amplitude ratio. The effects of pertinent flow parameters are discussed graphically. This work can be considered as mathematical modeling to the case of gall bladder with stones. Keywords Peristaltic motion; Jeffery fluid; Flexible walls; Hall effect; Porous medium 1. Introduction The peristaltic pumping is a form of material transport that occurs when a progressive wave of area contraction or expansion propagates along the length of a distensible tube containing some material. This kind of fluid transport occurs in many biological systems; in particular, a peristaltic mechanism may be involved in swallowing of food through the esophagus, urine transport from kidney to bladder through the ureter. The study of the mechanism of peristalsis, in both mechanical and physiological situations, has recently become the object of scientific research. Since the first investigation of Latham [10], several theoretical and experimental trials have been investigated to understand peristaltic action in different situations. A review of much of the early literature is presented in an article by Jaffrin and Shapiro [9]. A summary of most of the experimental and theoretical investigations reported, with details of the geometry, fluid Reynolds number, wavelength parameter, wave amplitude parameter and wave shape has been given by Srivastava and Srivastava [13]. Peristaltic flow through a porous medium is presented by El-Shehawey et al. [4]. Peristaltic motion of a generalized Newtonian fluid under the effect of a transverse magnetic field is studied by El-Shehawey et al. [5]. However, some progress has also been made in the field of non-Newtonian fluid mechanics. For recent contributions, we refer to some interesting studies in the references [3, 8, 11, 12]. The Hall effect is important when the Hall parameter, which is the ratio between the electron-cyclotron frequency and the electron-atom-collision frequency, is high. This happens when the magnetic field is high or when the collision frequency is low [14]. The aim of this article is to study MHD peristaltic channel flow of a Jeffery fluid through a porous medium bounded by two flexible plates. A very strong magnetic field is imposed on the flow so as to take Hall effects into consideration. Modified Darcy's law has been used in the flow modeling. We formulate the problem in Section 2. In Section 3, we discuss the perturbed systems. We solve the problem in Section 4. The numerical results and discussion as well as the conclusions are presented in Sections 5 and 6, respectively. Soliman R. Elkoumy . El Sayed I. Barakat Department of Mathematics, Faculty of Science, Helwan University, Cairo, Egypt * Sara I. Abdelsalam Basic Science Department, Faculty of Engineering, The British University in Egypt, Al-Shorouk City, Misr-Suez Desert Road, P.O. Box 43, Cairo 11837, Egypt Tel.: +(202) 2689-0000 Fax: +(202) 2687-5889 / 97 e-mail: sara.abdelsalam@bue.edu.eg 2. Formulation of the Problem Consider a two-dimensional infinite channel of uniform thickness 2 h , and filled with an incompressible, viscous and electrically conducting Jeffery fluid. We introduce Cartesian coordinate system with the x axis along the center line of the channel and y axis normal to it. A constant magnetic field B = (0, 0, Bo) is applied on the flow. The walls of the channel are compliant on which imposed traveling sinusoidal waves of small amplitude. We neglect the induced magnetic field under the assumption that the magnetic Reynolds number is small. The governing equations representing this model are: V (2.1) [ ( V.) V] = P + . S J B R , t . V =0, (2.2) J [E V B ] JB , (2.3) e ne (2.4) H J , E 0 , . B 0 . where , t, , p, , , e, and ne are the density of fluid, time, kinematic viscosity, pressure, dynamic viscosity, electrical conductivity, electric charge and number density of electrons, respectively. V , J , B , E , and H are the velocity vector, electric current density, magnetic induction vector, intensity of the electric field, and magnetic field strength, respectively. From Eq. (2.4) for the current density J = (Jx, Jy, Jz), we obtain from the relation . J 0 that Jz = constant. Hence, we consider that the channel is non-conducting and therefore Jz = 0 at the channel. For Jeffery fluid, the constitutive equation for extra stress tensor S is (1 1 ) S (1 t 2 t )A 1 , (2.5) in which 1 is the relaxation time, 2 is the retardation time, and the first RivlinEricksen tensor A 1 is defined by (2.6) A 1 ( grad V) ( grad V)T . On the basis of Jeffery fluid model [15], the following expression of Darcy's resistance has been suggested: (1 1 )R (1 2 )V , (2.7) t K t where (0 1) and K (positive value) are the porosity (constant) and permeability of the porous medium, respectively. In the absence of an externally applied electric field and with negligible effects of polarization of the ionized gas, we assume that the electric field vector equals zero. i.e. E = 0. The x and y components of Eq. (2.1) are: B o2 u u P S xx S xy u u (u m1 ) R x , (2.8) x y x x y (1 m12 ) t B o2 P S yx S yy u ( m1u ) R y , (2.9) x y y x y (1 m12 ) t where R x and R y are the x and y components of R and S xx , S xy and S yy are to be computed from Eq. (2.5). From Eqs. (2.2), (2.5), (2.7), (2.8) and (2.9) we obtain: u u u 1 P 2 1 1 t t u x y 1 1 t x 1 2 t u 2 Bo 1 ( u m ) 1 1 1 2 u , t K t (1 m12 ) (2.10) 1 P 2 1 1 t t u x y 1 1 t y 1 2 t 2 Bo 1 1 ( m1u ) 1 2 , (2.11) 2 t K t (1 m1 ) where u and are the velocity components in the direction of increasing x and y , Bo ) is the Hall parameter. respectively , and m 1 ( ene The fluid is subjected to boundary conditions imposed by the symmetric motion of the flexible walls. Let the vertical displacements of the upper and lower walls be and respectively, where [6] (x , t ) a cos( 2 (x ct )) , (2.12) y ( x , t ) a cos ( 2 ( x ct )) h a x c a Bo z z Fig. 1 Geometry of the problem a is the amplitude, is the wave length, and c is the wave speed. The horizontal displacement will be assumed zero. The boundary conditions are u (x , d , t ) 0 , ( x , d , t ) (2.13) ( x , t ) , (2.14) t Equation (2.2) allows the use of the stream function ( x , y , t ) in terms of which u , . y x After eliminating p and dropping the stars, Eqs. (2.10) and (2.11) become 1 ( 2 ) 2 2 1 4 1 y x x y 2 t t t 1 1 (1 m ) t B 02 2 1 2 2 K 1 2 t , (2.15) (2.16) 2 in which denotes the Laplacian operator and subscripts of differentiation with respect to x and y . The equation of motion of the compliant wall is [2]: 2 4 2 m d B T K p p0 . t 2 4 2 t x x indicate partial (2.17) where m , d , B , T , K , and p 0 are the plate mass per unit area, the wall damping coefficient, the flexural rigidity of the plate, the longitudinal tension per unit width, the spring stiffness, and the pressure on the outside surface of the wall, respectively. Assuming p 0 0 and the channel walls inextensible so that only their lateral motions normal to the undeformed positions occur. The boundary conditions are then y 0 and x ( x , t ) t at y h (2.18) Continuity of stresses requires that p must be the same as that which acts on the fluid on y h at the interfaces of both the walls and the fluid. Employing the x momentum equation, we obtain: 2 4 2 1 m d B T K 1 2 4 2 t x t t x x 1 2 2 y 1 1 ( yt y xy x yy ) t t B 02 1 1 2 (1 m1 ) t ( y m1 x ) 1 2 K t y . (2.19) Introducing u , u* ,* , * , * , h h c c ch h ct m p dh B * * t * , m* , p* , d , B , h h c2 h 2 x* T * x , y* Th y , K* 2 Kh 3 , 1 * Dropping the stars we obtain 2 c h 1, 2 * c h 2, 1 K * h . Kc 1 (2 ) 2 2 M 2 1 1 y x x y 1 1 t t t 1 2 1 1 2 1 2 4 , K t R t cos ( x t ) , y 0 and x sin (x t ) at y 1 1 1 t x 2 (2.20) (2.21) (2.22) 2 d B 4 T 2 K m t 2 R t R x 4 R 2 x 2 R 2 1 2 1 2 1 2 y M 1 1 1 ( y m1 x ) 1 2 y R t t K t 1 1 t ( yt y xy x yy ) at y 1 (2.23) where a h is the amplitude ratio, 2 h is the wave number, R ch is Reynolds h c B 0 is Hartman number, and 1 number, M 1 1 m1 2 . 3. Perturbed Systems Assuming the amplitude ratio of the wave to be small, we obtain the solution for the p stream function as a power series in terms of , by expanding and in the form [7]: x o 1 2 2 ... p p )o ( p )1 ( p ) 2 ... (3.2) x x x x The first term at the right-hand side of Eq. (3.2) corresponds to an imposed pressure gradient which is considered as a constant. The higher-order terms correspond to the peristaltic motion. Introducing Eqs. (3.1) and (3.2) into (2.20), (2.22) and (2.23), and collecting the terms of like powers of , we obtain three sets of coupled linear differential equations with their corresponding boundary conditions in 0 , 1 and 2 for the first three powers of . ( )( (3.1) 2 3.1. System of Order Zero 1 2 2 1 2 0 1 1 ( R t t t 1 M 2 1 1 1 2 0 1 2 t K t 2 0 0 y 2 0 x 0 x 2 0 y ) 2 0 , (3.3) 0 y ( 1) 0, (3.4) 0 x ( 1) 0, (3.5) 1 2 1 2 0 y (1) 1 1 ( 0 yt (1) 0 y (1) 0 yx (1) R t t 0x (1) 0 yy (1)) M 2 1 1 1 ( 0 y (1) m1 0x (1)) t 1 1 2 0 y (1) 0 , K t (3.6) 3.2. System of Order One 1 1 2 2 2 1 1 1 ( 21 0 y 21x 1y 2 0x R t t t 2 1 2 2 2 2 0x 1y 1x 0 y ) M 1 1 1 1 1 2 1 , t K t 1 y ( 1) 0 yy ( 1) cos ( x t ) 0 , (3.7) (3.8) 1x ( 1) 1xy ( 1) cos ( x t ) sin ( x t ) , 1 1 t (3.9) d 2 B 5 3 m sin (x t ) cos (x t ) 2 sin (x t ) R R T 3 sin (x t ) K2 sin (x t ) 1 1 2 2 t R R R (1yxx (1) 1yyy (1) cos ( x t ) 0 yyxx ( 1) cos ( x t ) 0 yyyy ( 1)) M 1 (1 1 2 t )( 1y ( 1) cos ( x t ) 0 yy (1) m1 1x (1) m1 cos ( x t ) 0 xy ( 1)) 1 2 ( 1y (1) cos ( x t ) 0 yy ( 1)) 1 1 K t t cos (x t ) 0 yyt (1)) 1 1 ( 0 y ( 1) 1xy ( 1) t 1 ( 1yt (1) cos ( x t ) 0 y ( 1) 0 xyy ( 1) 1y ( 1) 0 xy ( 1) cos ( x t ) 0 yy ( 1) 0 yx ( 1)) ( 0 x ( 1) 1 yy ( 1) cos ( x t ) 0 x ( 1) 0 yyy ( 1) t 1x ( 1) 0 yy ( 1) cos ( x t ) 0 xy ( 1) 0 yy ( 1)) , 1 1 (3.10) 3.3. System of Order Two 1 1 2 2 2 2 R t 1 1 2 2 2 ( 2 0 y 2x 1y 1x t t 2 y 0x 0x 2 y 1x 1y 2x 0 y ) 2 2 M 1 1 1 2 2 2 1 2 2 1 2 t K t 2 2, (3.11) 2 2 y ( 1) cos ( x t ) 1 yy ( 1) 1 2 cos ( x t ) 0 yyy ( 1) 0, (3.12) 2 2 x ( 1) cos ( x t ) 1xy ( 1) 1 2 cos ( x t ) 0 xyy ( 1) (3.13) 0 0, 1 1 2 ( 2 yxx ( 1) 2 yyy ( 1) cos ( x t )( 1yyxx ( 1) 1yyyy ( 1)) R t 1 2 cos 2 ( x t )( 0 yyyxx ( 1) 0 yyyyy ( 1)) M 2 1 (1 1 t )( 2 y ( 1) cos (x t )1yy (1) 1 2 cos 2 (x t ) 0 yyy (1) m1 2x (1) 1 2 ( 2 y ( 1) 2 K t cos (x t ) 1yy (1) 1 2 cos 2 ( x t ) 0 yyy ( 1)) 1 1 ( 2 yt ( 1) t m1 cos ( x t ) 1xy ( 1) m1 cos 2 ( x t ) 0 xyy ( 1)) 1 cos (x t )1yyt (1) 1 2 cos 2 (x t ) 0 yyyt (1)) t 1 1 ( 0 y (1) 2 yx (1) cos (x t ) 0 y (1) 1xyy (1) 1 2 cos2 (x t ) 0 y (1) 0xyyy (1) 1y (1)1yx (1) cos ( x t ) 1y ( 1) 0 xyy ( 1) 2 y ( 1) 0 yx ( 1) cos (x t ) 0 yy ( 1) 1yx ( 1) cos 2 (x t ) 0 yy ( 1) 0 xyy ( 1) cos ( x t ) 1yy ( 1) 0 yx ( 1) 1 2 cos 2 (x t ) 0 yyy ( 1) 0 yx ( 1)) 1 1 ( 0 x (1) 2 yy (1) cos ( x t ) 0 x (1) 1yyy ( 1) t 1 2 cos 2 ( x t ) 0 x (1) 0 yyyy ( 1) 1x ( 1) 1yy ( 1) cos ( x t ) 1x ( 1) 0 yyy ( 1) 2 x ( 1) 0 yy ( 1) cos ( x t ) 0 xy ( 1) 1yy ( 1) cos 2 (x t ) 0 xy ( 1) 0 yyy ( 1) cos (x t ) 1xy (1) 0 yy (1) 1 2 cos2 ( x t ) 0 xyy (1) 0 yy (1)) , (3.14) 4. Method of Solution We note that the first set of differential equations in 0 subject to the steady parallel flow and transverse symmetry assumption for a constant pressure gradient in the x direction, yields the following classical Poiseuille flow: 2K 0 sinh y (4.1) 0 (y ) y C1 , 2 cosh RN K 0 R / 2 dp / dx , 0 in which N 2 M 2 1 1 K , RN 2 and C 1 is an arbitrary constant. The second and third sets of differential equations in 1 and 2 with their corresponding boundary conditions are satisfied by 1 i ( x t ) * i ( x t ) 1 ( x , y , t ) ( 1 ( y ) e 1 ( y )e ), (4.2) 2 1 2 i ( x t ) * 2 i ( x t ) 2 ( x , y , t ) (20 ( y ) 22 ( y ) e 22 ( y ) e ), (4.3) 2 where the asterisk denotes the complex conjugate. Substituting equations (4.2) and (4.3) into the differential equations and their corresponding boundary conditions in 1 and 2 leads to the following set of differential equations: d2 K0 cosh y R 1 i 1 2 ) RM 2 1 2 i R 2i 2 (1 ( ) N cosh K 1 i 2 dy d2 2 cosh y 1 i 1 2 2 1 ( y ) 2 i K 0 2 1 ( y ) , N cosh 1 i 2 dy 1/ (1) 2K 0 RN 2 tanh , (4.5) 1 i 1 R / 2 ( ) 1 (1) K 1 i 2 1/// (1) i R RM 2 1 i RM 2 1m1 2i (4.4) K 0 N 2 K 0 3 1 i 1 ( 1) 2 tanh 1 RN 2 1 i 2 tanh 2M 2 1 //// 20 K0 2 N 1 i 1 1 i 1 K0 tanh R 2 2 KN 1 i 2 1 i 2 tanh i 2 2 ( R m i Rd 4B 2T K ) , R2 iR 2 K 0 2 , 1 // *// ( 1) ( 1) 1 RN 2 21 1/// (1) 2 (4.7) [1 ( y ) 1*// ( y ) 1* ( y )1// ( y )] / RN 20/ (1) // 20 (y ) , 2 (4.8) (4.9) 1 1// (1) 1*// ( 1) 1//// ( 1) 1*//// ( 1) 2 2 K 0 4 RN 2 i m1 2 RN 20/ (1) K 0 2 2 RN 2 2 1// (1) 1*// (1) iR 1// ( 1) 1*// ( 1) RM 2 1 1/ (1) 1*/ ( 1) 2 iR 1 (1) *1// (1) *1 ( 1) 1// (1) 2 i K 0 2 1 (1) 1* (1) , 2 N (4.6) (4.10) 2 d2 1 2i 1 2 d 2 R 2 2 4 2 4 2 i R RM 1 22 ( y ) K 1 2i 2 dy dy 4i K 0 1 2i 1 cosh y d 2 2 1 2 4 22 ( y ) 2 1 2i cosh dy N 2 2 4i K 0 cosh y 1 2i 1 ( y ) cosh 1 2i 2 22 N2 i R 1 2i 1 / 1 ( y) 1// ( y) 1 ( y) 1/// ( y) , 2 1 2i (4.11) 2 / (1) 22 K 0 2 2RN 2 1 // (1) , 2 1 1 2 i 1 / 2R / (1) 22 (1) K 22 1 2 i 2 222/// (1) 4 2 iR 1 2 i 1 / 8 i K 0 tanh 22 (1) N2 1 2 i 2 2RM 2 1 1 2 i 1 //// 4 i RM 2 1 m1 22 (1) 1 (1) 1 2 i 2 1 2 i 1 // R // i R 1 (1) 1 (1) K 1 2 i 2 RM 2 1 2 i 1 // 1 2 i 1 / / 1 (1) i R 1 (1)1 (1) 1 2 i 2 1 2 i 2 1 1 2 i 1 2 i K 0 2 1 2 i 1 // ( 1) ( 1) 1 1 (1) 1 N2 1 2 i 2 1 2 i 2 i R (4.12) 1 2 i 1 / K02 2 K ( 1) 1 1 KN 2 R 1 2 i 2 m1 i RM 2 1 M 2 1K 0 2 1 2 i 1 N , 1 2i 2 2 (5.13) where the prime indicates the derivative with respect to y . Thus, we obtained a set of differential equations together with the corresponding boundary conditions which are sufficient to determine the solution of the problem up to the second order in . But these equations are fourth-order ordinary differential equations with variable coefficients and the resulting problem is not an eigenvalue problem since all the boundary conditions are not homogeneous. Therefore, we restrict our investigation to the case of free-pumping. Physically, this means that the fluid is stationary if there are no peristaltic waves. In this case we put (p / x )0 0 which means K 0 0 , and we are able to obtain a simple analytical solution in a closed form [1, 6, 8]. Under this assumption, the solution of Eqs. (4.4)-(4.6) is 1 ( y ) L1 sinh y L2 cosh y L3 sinh y L4 cosh y , (4.14) where 1 i 1 , p 2 q1 q 2 p1 1 i 2 R q2 1 i 1 L3 , q 2 p1 p 2 q1 1 i 2 R p2 L4 (4.15) (4.16) sinh , L sinh 4 cosh L1 L3 , cosh L2 ( 2 2 R K (4.17) (4.18) 1 i 1 1 i , 2 ) ( RM 1 i R ) (4.19) 1 i 1 , 1 i 2 (4.20) 2 1 i RM 1m1 2 p1 ( 3 2 ) cosh , q1 in which p2 1 1 sinh coth 1 cosh , cosh tanh 1 sinh , q 2 ( ) sinh , 3 2 Next, in the expansion of 2 , we are interested only in the terms 20 ( y ) as our aim is to determine the mean flow only. Thus the solution of Eqs. (4.8)-(4.10), under the assumption K 0 0 , takes the following form: / 20/ ( y ) F ( y ) F (1) sinh (1 y ) F ( 1) sinh (1 y ) sinh 2 D1 sinh (1 y ) D 2 sinh (1 y ) sinh 2 And the peristaltic mean flow is obtained as c 0 1 cosh y , cosh (4.21) u 2 2 2 F (1) sinh (1 y ) F ( 1) sinh (1 y ) F ( y ) 20/ ( y ) 2 sinh 2 D1 sinh (1 y ) D 2 sinh (1 y ) sinh 2 cosh y c 0 1 , cosh (4.22) where / D1 20 ( 1) 1 2 { [( L1 L1 ) sinh ( L 2 L 2 ) cosh ] L 3 sinh * 2 * 2 L 4 cosh L3 sinh L 4 cosh *2 * 2 / D 2 20 ( 1) 1 2 * *2 * * , (4.23) { [( L1 L1 ) sinh ( L 2 L 2 ) cosh ] L 3 sinh * 2 * 2 2 L 4 cosh *2 L*3 sinh * *2 L*4 cosh * , c0 (1 2 F ( 1) // ) D1 F ( 1) 2 i R D3 D5 i R (4.24) i RM 1m1 2 D7 D9 , (4.25) 2 2 2 2 2 1 1 *// * // *2 2 * * D 3 [1 ( 1) 1 ( 1) 1 ( 1) 1 ( 1)] ( ) L1L3 sinh y sinh y 2 2 L1L 4 sinh y cosh y L 2 L3 cosh y sinh y L 2 L 4 cosh y cosh y * * * * * * ( ) L1L3 sinh y sinh y L 2 L3 cosh y sinh y 2 2 * * L1*L 4 sinh y cosh y L*2 L 4 cosh y cosh y ( *2 2 ) L3L*3 sinh y sinh * y L3L*4 sinh y cosh * y L*3L4 cosh y sinh * y L4L*4 cosh y cosh * y , 1 D 5 [ 1 ( 1) 1 ( 1)] //// *//// 2 2 1 4 ( L1 L1 ) sinh ( L 2 L 2 ) cosh * *4 * * 4 L3 sinh L4 cosh L3 sinh L4 cosh 4 1 4 D 7 [ 1 ( 1) 1 ( 1)] // * // 2 2 1 2 * *4 * * *2 * 2 1 D 9 [ 1/ ( 1) 1*/ ( 1)] 2 (L 2 1 1 * , (4.27) ( L1 L1 ) sinh ( L 2 L 2 ) cosh * 2 L3 sinh L 4 cosh L3 sinh L 4 cosh 2 (4.26) * *2 * * , (4.28) L1 ) cosh ( L 2 L 2 ) sinh * * L3 cosh L 4 sinh *L*3 cosh * *L*4 sinh * , (4.29) F ( y ) s1 cosh( ) y s 2 sinh( ) y s 3 cosh( ) y s 4 sinh( * ) y s 5 cosh( ) y s 6 sinh( ) y s 7 cosh( ) y s 8 sinh( ) y s 9 cosh( * ) y * * * s10 sinh( * ) y s11 cosh( * ) y s12 sinh( * ) y ,(4.30) s1 s3 iR ) *2 2 4 ( ) * 2 iR ( *2 ) 4 ( ) iR 4 ( ) 2 ( 2 2 ) 4 ( ) 2 iR ( ) iR ) 2 4 ( ) 2 * ( L 3 L3 L 4 L 4 ), s12 2 2 ( 2 2 ) 4 ( ) 2 ( 2 4 ( ) *2 / 20 (L*2 L3 L1*L 4 ), 2 * 2 ( * ( L 2 L3 L1 L 4 ), 2 ) *2 ) * 2 * ( L 4 L 3 L 3L 4 ), 2 4 ( ) / * 4 ( ) iR * (L 2 L*3 L1L*4 ), ( ) * 2 Unlike most of the other investigations, 2 0 (+1) 2 2 iR 2 * 2 iR iR * * ( L1L 4 L 2 L3 ), 2 ( *2 2 ) 4 ( ) ( L 3L3 L 4 L 4 ), s10 * 2 * 2 (L1*L3 L*2 L 4 ), s 6 2 * ) *2 4 ( ) iR s4 ( * 2 2 4 ( ) ( s2 (L1*L3 L*2 L 4 ), s 8 2 * 2 iR s11 *2 *2 * L 2 L 4 ), * * ( L L L 2 L 4 ), 2 1 3 ( 2 2 ) iR s9 * ( L1L 3 2 2 * 2 s5 s7 ( * 2 * ( L 3 L 4 L 4 L 3 ). ( 1) in our investigation which gives the prediction that the motion of fluid is nonsymmetric and which will be discussed later. Now the critical reflux condition is defined as one for which the mean-velocity u ( y ) is zero at the center line y 0 [1, 8]. Therefore, according to Eq. (4.22), the critical reflux condition is given by g 21 ( g 21 )2 4 g 22 Tc , 2 (4.68) where g 1 1 (h1 h2 ( )2 h 3 ) cosh( ), g 2 (h1 h2 ( ) 2 h3 ) sinh( ), g 3 1 (h1 h2 ( ) 2 h3 ) cosh( ), g 4 ( h1 h2 ( ) 2 h3 ) sinh( ), g 5 1 (h1 h2 ( ) 2 h3 ) cosh( ), g 6 (h1 h2 ( ) 2 h3 ) sinh( ), g 7 1 (h1 h2 ( ) 2 h3 ) cosh( ), g 8 (h1 h2 ( ) 2 h3 ) sinh( ), g 9 1 (h1 h2 ( * ) 2 h3 ) cosh( * ), g 10 (h1 h2 ( * ) 2 h3 ) sinh( * ), g 11 1 (h1 h2 ( * ) 2 h3 ) cosh( * ), g 12 ( h1 h2 ( * ) 2 h3 ) sinh( * ), g 13 g 1 e1 g 1 e 4 g 3 e 7 g 4 e10 g 5 e13 g 6 e16 g 7 e19 g 8 e 22 g 9 e 25 g 10 e 28 g 11 e 31 g 12 e 34 , g 14 g 1 e 2 g 2 e 5 g 3 e 8 g 4 e11 g 5 e14 g 6 e17 g 7 e 20 g 8 e 23 g 9 e 26 g 10 e 29 g 11 e 32 g 12 e 35 , g 15 g 1 e 3 g 2 e 6 g 3 e 9 g 4 e12 g 5 e15 g 6 e18 g 7 e 21 g 8 e 24 g 9 e 27 g 10 e 30 g 11 e 33 g 12 e 36 , j j g 16 1 2 sinh (h4 h2 2 h3 ) 5 2 cosh (h4 h2 2 h3 ) 2 i 2 2 2R 2 c 2 sinh L6 (h4 h2 2 h3 ) i *2 2R 2 i 2 2R 2 c 2* sinh *L*6 (h4 h2 *2 h3 ) c1 cosh L6 (h4 h2 2 h3 ) i *2 2R 2 c1* cosh *L*6 (h4 h2 *2 h3 ) j3 2 (h6 cosh h5 sinh ) i 2R 2 2R j2 g 17 2 i 3 2 2R 2 2R j4 2R 2 2 j6 i * 2 j8 2 ( * 2 2 * * 2R 2 c1*L*6 (h5 * cosh * h6 sinh * ) 2 cosh (h4 h2 2 h3 ) i 3 2 2R 2 c1 cosh (h4 h2 2 h3 ) i 3 *2 2R 2 c1* cosh * (h4 h2 *2 h3 ) (h6 sinh h5 cosh ) i 3 2R 2 c 2 (h5 sinh h6 cosh ) * h5 g 18 c1L 6 (h5 cosh h6 sinh ) 2R 2 * c 2 (h5 sinh h6 cosh ) i 3 * 2R i c 2* sinh * (h4 h2 *2 h3 ) 2 i 3 * (h6 cosh h5 sinh ) 2 * c 2 sinh (h4 h2 2 h3 ) i 3 *2 (h6 sinh h5 cosh ) c 2 L 6 (h5 sinh h6 cosh ) * * 2 sinh (h4 h2 2 h3 ) 2 2 c 2 L 6 (h5 sinh h6 cosh ) i * j7 * c1 (h5 cosh h6 sinh ) i 3 * 2R 2 c1* (h5 * cosh * h6 sinh * ) , 2 )(c 5 sinh sinh * c17 sinh cosh * c 23 cosh sinh * c11 cosh cosh * ) ( 2 2 )(c 8 sinh sinh c 32 cosh sinh c 20 sinh cosh c14 cosh cosh ) ( *2 2 )(c 26 sinh sinh * c 35 sinh cosh * c 38 cosh sinh * c 29 cosh cosh * ) , g 19 h5 2 ( * 2 2 )(c 6 sinh sinh * c18 sinh cosh * c 24 cosh sinh * c12 cosh cosh * ) ( 2 2 )(c 9 sinh sinh c 33 cosh sinh c 21 sinh cosh c15 cosh cosh ) ( *2 2 )(c 27 sinh sinh * c 36 sinh cosh * c 39 cosh sinh * c 30 cosh cosh * ) , g 20 h5 ( *2 2 )(c 7 sinh sinh * c19 sinh cosh * c 25 cosh sinh * 2 c13 cosh cosh * ) ( 2 2 )(c10 sinh sinh c 34 cosh sinh c 22 sinh cosh c16 cosh cosh ) ( *2 2 )(c 28 sinh sinh * c 37 sinh cosh * c 40 cosh sinh * c 31 cosh cosh * ) , g 21 g 14 g 17 g 19 g g 16 g 18 , h1 , g 22 13 g 15 g 20 g 15 g 20 sinh 1 sinh 2 2 h2 sinh sinh 2 , h3 1 1 1 , h4 2 cosh sinh 2 cosh , 1 sinh 2 1 1 sinh 2 cosh sinh 2 1 , i R 2 h5 1 i R 1 , h6 2 cosh 1 2 2 2 4 1 M 1 m1 , L5 R m B K , cosh i R ( *2 2 ) 4 ( * )2 2 i R ( *2 2 ) 4 ( * ) 2 2 L6 i Rd L5 , L*6 i Rd L5 , e1 e2 i R ( *2 2 ) 4 ( * ) 2 2 i R ( *2 2 ) 4 ( * ) 2 2 i R ( *2 2 ) 4 ( * ) 2 2 e4 e6 e8 iR ( *2 2 ) 4 ( * ) 2 2 e10 e12 ( *2 2 ) 4 ( * ) 2 2 iR ( *2 2 ) 4 ( * ) 2 2 e18 4 ( ) 2 2 i R ( 2 2 ) 4 ( ) 2 2 i R ( 2 2 ) 4 ( ) 2 2 e 22 e 24 e 26 e 28 e 30 e 32 e 34 iR ( 2 2 ) iR ( 2 2 ) 4 ( )2 2 iR ( 2 2 ) 4 ( )2 2 (c 34 c 22 ) , e 25 ( * )2 2 i R ( *2 2 ) 4 ( * )2 2 i R ( *2 2 ) 4 ( * )2 2 iR ( *2 2 ) 4 ( * )2 2 iR ( *2 2 ) 4 ( * )2 2 ( *2 2 ) 4 ( * ) 2 2 (c18 c 2 4 ) , (c 5 c11 ) , (c 7 c13 ) , iR ( *2 2 ) 4 ( * ) 2 2 (c 24 c18 ) , i R ( 2 2 ) 4 ( ) 2 2 ( 2 2 ) 4 ( ) 2 2 (c 8 c14 ) , (c10 c16 ) , i R ( 2 2 ) 4 ( ) 2 2 (c 21 c 33 ) , i R ( 2 2 ) (c 8 c14 ) , 4 ( ) 2 2 iR (c 32 c 20 ) , e 23 4 iR i R (c 22 c 34 ) , e19 ( *2 2 ) ( * ) 2 2 ( * ) 2 2 (c 20 c 32 ) , e17 i R 4 4 (c 9 c15 ) , e 21 4 ( )2 2 ( *2 2 ) ( *2 2 ) (c 9 c15 ) , e15 (c 7 c13 ) , i R iR (c 25 c19 ) , e13 ( 2 2 ) e 20 (c19 c 25 ) , e 7 (c 23 c17 ) , e11 i R e16 (c17 c 23 ) , e 5 (c 6 c12 ) , e 9 iR e14 (c 6 c12 ) , e 3 (c 5 c11 ) , ( 2 2 ) 4 ( )2 2 iR (c10 c16 ) , ( 2 2 ) 4 ( )2 2 (c 33 c 21 ) , i R ( *2 2 ) 4 ( * )2 2 (c 27 c 30 ) , e 27 (c 35 c 38 ) , e 29 (c 37 c 40 ) , e 31 (c 27 c 30 ) , e 33 (c 38 c 35 ) , e 35 (c 26 c 29 ) , i R ( *2 2 ) 4 ( * )2 2 i R ( *2 2 ) 4 ( * )2 2 iR ( *2 2 ) 4 ( * )2 2 iR ( *2 2 ) 4 ( * )2 2 iR ( *2 2 ) 4 ( * )2 2 (c 28 c 31 ) , (c 36 c 39 ) , (c 26 c 29 ) , (c 28 c 31 ) , (c 39 c 36 ) , iR e 36 ( *2 2 ) 4 ( ) * 2 2 1 i 1 R p2 , 1 i 2 p 2 q1 q 2 p1 (c 40 c 37 ) , c1 cosh sinh 1 i 1 R q2 , c3 , c4 , cosh sinh 1 i 2 q 2 p1 p 2 q1 c2 c5 c8 c c c * L L* , c 6 4 2 3 2 6 6 R c17 R 4 c 29 c 38 2 * 2L6 L6 , 2 R i 2 4 R 4 4 R c c * L L* , c 39 4 1 2 6 6 ( c 2 i R i 2 2 i R 2 R R c 2 c 2 (L6 , c19 L*6 ) , 28 c 4 4 c c * ( L 6 L*6 ) , c 40 4 1 2 i R c3 L6 c 2* c3*L*6 ) , j 4 c 4 L6 c1* c 4*L*6 ) , j 8 R 4 6 R 4 6 R R 4 c1* c 2 c 3 , 4 c1 c 2* c 3* , 6 R4 c1 c 4 c 2* , c1 c1* , 6 R 4 c 2 c1* c 4* , c 2 c1* , c1 c 2* , 3 (c 2 2 i3 R 3 i R 6 c1 c1* c 4* , c 2 c 2* , 6 R 4 6 c c * c * ( L 6 L*6 ) , c 34 4 2 1 4 c c * ( L 6 L*6 ) , c 37 4 2 1 R R 4 4 4 6 c c * ( L 6 L*6 ) , c 31 4 1 1 R R c1 c1* c 4 , 4 6 c c c * ( L 6 L*6 ) , c 25 4 1 4 2 * R 4 c 4 L6 c1* c 4*L*6 ) , j 6 (c1 L*6 ) c c * c * (L 6 L*6 ) , c 22 4 1 2 3 c 3 L6 c 2* c 3*L*6 ) , j 2 (c 2 ( c1 c1 c 2 c 3 (L 6 * R c c * c *L L* , c 33 4 2 1 4 6 6 c c *L L* , c 36 4 2 1 6 6 R 4 4 c 27 2 R 2 R j7 c2 c * c c *L L* , c 30 4 1 1 6 6 R R , c18 c c * c * (L 6 L*6 ) , c16 4 1 1 4 c 2 c 2* c 3* , 4 6 c c * c * (L 6 L*6 ) , c13 4 1 1 4 4 c c c * L L* , c 24 4 1 4 2 6 6 R j3 j5 c1 c 2 c * 3 L6L6 R 4 R 2 4 R 6 4 R c c * c *L L* , c 21 4 1 2 3 6 6 R 2 R c 32 c 35 * 2 c 26 R c c * c * L L* , c15 4 1 1 4 6 6 c 23 c c * c * (L 6 L*6 ) , c10 4 2 2 3 c 2 c 3 c 2* , 4 R 4 c c * c L L* , c12 4 1 1 4 6 6 2 c 20 2 R c c c * ( L 6 L*6 ) , c 7 4 2 3 2 2 R 6 4 R c c * c *L L* , c 9 4 2 2 2 6 6 c14 j1 2 R c11 2 2 2 i R c 3 c 2* c 3* ) , * * (c 2 c 3 c 2 c 3 ) , (c1 c 4 c1* c 4* ) , 3 2 (c1 c 4 c1* c 4* ) . 5. Numerical results and discussion In order to have an estimate of the quantitative effects of various parameters involved in the results of the present analysis, the mean velocity at the boundaries of the channel, the mean velocity perturbation function, the time-averaged mean axial velocity distribution and the reversal flow are calculated for various values of these parameters when K 0 0 . The constants D1 and D2 arising from the nonslip boundary condition of the axial velocity on the wall are due to 20/ ( y) at the boundaries and are related to the mean velocity at the boundaries of the channel by u(1) 2/ 0 ( y) D1 , u(1) 2/ 0 ( y) D 2 . This 2 2 2 2 2 2 2 2 shows that the nonslip condition applies to the wavy wall and not to the mean position of the wall. The variations of D1 and D2 with for various values of the magnetic parameter M , Hall parameter m1 , wall damping d , permeability of porous medium K , relaxation time 1 , and retardation time 2 are plotted in Figs. 2 and 3. In Figs. 2a 5d, the effects of the various parameters involved are discussed for D1. In Figs. 2a and 2b, it is seen that D1 increases by increasing M . Figures 2c and 2d reveal that D1 decreases by increasing m1 . In Figs. 2a 2c, it is noted that D1 decreases by increasing d , K and 1 , whereas it increases by increasing 2 as seen in Fig. 2d. The effects of various parameters on D2 are shown to be similar to that on D1 except for the Hall parameter. Figures 3a, 3b, 3c, and 3d illustrate that M , m1 and 2 have an increasing effect on D2. However, d , K and 1 have a decreasing effect on it. It is noted that damping may cause the mean flow reversal at the walls, which is not possible in the elastic case. Following Fung and Yih [7], we define the mean-velocity perturbation function G ( y ) as 200 G ( y )= F (y ) 2 2 R F (1) sinh (1 y ) sinh 2 1 sinh 2 cosh y cosh , F ( 1) sinh (1 y ) sinh 2 The mean velocity perturbation function is plotted with for various values of M , m1 , d , K , 1 , and 2 in Figs. 4a 4d. It is obvious from Figs. 4a and 4b that M has an increasing effect on G ( y ) , while m1 has a decreasing effect on it as seen in Figs. 4c and 4d. It is noted that d , K , and 2 have a decreasing effect on G ( y ) , while 1 has an increasing effect on it. It is also observed that G ( y ) is minimum near the center of the channel. Unlike all other investigations, it is noticed that G ( y ) is nonsymmetric as illustrated in Figs. 4b and 4d (for example; G (0.4) 2.07327 and G (0.4) 4.51921 for the dot dashed curve in Fig. 4b). In Figs. 5a 5d, the variations of mean velocity distribution with y for various values of the concerned parameters are illustrated. Figures 5a and 4b depict that the possibility of flow reversal increases by an increase in M . However, Figs. 5c and 5d depict that the possibility of flow reversal decreases by an increase in m1 . It is noted that d , K , and 1 have a decreasing effect on the mean velocity distribution whereas 2 has an increasing effect on it. Figures 6a 6d elucidate the variations of critical value of T with for various values of the indicated parameters. It is obvious that Tc increases with the increase in M and decreases with the increase in m1 . It is also observed that R and 2 have an increasing effect on Tc , while K and 1 have a decreasing effect on it. We note that the critical value of T becomes exceedingly high for small values of as compared with the large ones. This can be interpreted physically that at high wave length (or at low frequency) reversal flow may occur for a very high rigidity of the boundary walls. Thus, when T is lower than Tc , there is no mean flow at the center of the channel [1]. It should be noted that the effects of some parameters were found to be similar to Hayat et al. [8] and Abd Elnaby and Haroun [1]; so the figures were excluded to avoid any kind of repetition. In such figures, it was shown that D1, D2, and possibility of flow reversal increase with an increase in 2 , T , and K , and decrease with an increase in 1 . Conversely, G ( y ) decreases with the increase in 2 , T , and K , and increases with the increase in 1 . It was also illustrated that Tc decreases with an increase in 1 and increases with an increase in 2 , and that K has a slight decreasing effect on Tc . (zero damping d 0.0) M 3.0 0 0.02 0.02 0.03 0.03 0.04 0.05 0.06 0.07 0 0.04 M 0.0 M 3.0 0.05 M 3.0 M 6.0 0.06 M 6.0 0.2 0.4 0.6 Wave number, 0.8 1 0 0.2 M 3.0 0.4 0.6 Wave number, d 0.01 0.8 1 2 0.0 0 K 0.2 m 1 1.0 c m1 1.0 0.02 D1 0.04 D1 1 1.0 M 0.0 0 0.02 b 0.01 D1 D1 0 aa 0.01 0.06 m1 0.0 m1 1.0 m1 2.0 0.08 0.1 0 0.2 0.03 m1 0.0 m1 1.0 m1 2.0 0.04 0.05 0.06 0.4 0.6 Wave number, 0.8 0 1 0.2 0.4 0.6 Wave number, 0.8 1 Fig. 2 The variation of D1 with wave number for three different values of magnetic parameter M (panels a and b) and Hall parameter m 1 (panels c and d). The other chosen parameters are m 0.01, B 2, T 1, K 1, R 10, d 0.35, K 1.5, 1 0.8, 2 0.5, and m 1 1 (panel a); m 0.01, B 2, T 1, K 1, R 10, d 0.2, K 1.5, 1 2, 2 0.5, and m 1 1 (panel b); m 0.01, B 2, T 1, K 1, R 10, d 0.5, K 1, 1 0.8, 2 0.5, and M 2 (panel c); m 0.01, B 2, T 1, K 1, R 10, d 0.2, K 1.5, 1 0.8, 2 0.6 , and M 2 (panel d) (zero damping d 0.0) M 3.0 0 a 0 b 0.01 0.02 D2 D2 0.02 0.04 0.06 0 1 1.0 M 3.0 0.03 M 0.0 0.04 M 0.0 M 3.0 0.05 M 6.0 0.06 M 3.0 M 6.0 0.2 0.4 0.6 Wave number, 0.8 1 0 0.2 0.4 0.6 Wave number, 0.8 1 0 0.02 d 0.005 0.01 0.03 0.015 D2 D2 0 K 0.2 m 1 0.5 c 0.01 0.04 0.06 0.07 0 0.2 m1 0.0 m1 0.5 m1 1.0 0.02 m1 0.0 m1 0.5 m1 1.0 0.05 0.025 0.03 0.4 0.6 Wave number, 0.8 1 0 0.2 2 0.0 m1 0.5 0.4 0.6 Wave number, 0.8 1 0 5 10 a The perturbationfunction, G y The perturbationfunction, G y Fig. 3 The variation of D2 with wave number for three different values of magnetic parameter M (panels a and b) and Hall parameter m 1 (panels c and d). The other chosen parameters are m 0.01, B 2, T 1, K 1, R 10, d 0.35, K 1.5, 1 0.8, 2 0.5, and m 1 1 (panel a); m 0.01, B 2, T 1, K 1, R 10, d 0.2, K 1.5, 1 2, 2 0.5, and m 1 1 (panel b); m 0.01, B 2, T 1, K 1, R 10, d 0.5, K 1, 1 0.8, 2 0.5, and M 4 (panel c); m 0.01, B 2, T 1, K 1, R 10, d 0.2, K 1.5, 1 0.8, 2 0.6 , and M 2 (panel d) (zero damping d 0.0) M 1.0 15 20 M 0.0 M 1.0 M 2.0 25 30 35 0 0.2 0.4 0.6 0.8 0 5 1 0.6 10 M 1.0 15 20 M 0.0 M 1.0 25 b 30 1 M 2.0 1 0.5 0 y 0 c 5 10 K 1.0 m1 1.0 15 m1 0.0 m1 1.0 m1 2.0 20 0 0.2 0.4 0.6 0.8 The perturbationfunction, G y The perturbationfunction, G y y 0.5 1 0 5 10 2 0.0 15 20 1 d 1 m1 0.0 m1 1.0 m1 2.0 m1 1.0 0.5 y 0 y 0.5 1 Fig. 4 The variation of the mean velocity perturbation function G ( y ) for three different values of magnetic parameter M (panels a and b) and Hall parameter m 1 (panels c and d). The other chosen parameters are m 0.01, B 2, T 1, K 1, R 1, d 1, K 1.5, 1 0.8, 2 0.5, 0.5, and m 1 2 (panel a); m 0.01, B 2, T 1, K 1, R 1, d 0.5, K 1.5, 1 1.2, 2 0.5, 0.5, and m 1 2 (panel b); m 0.01, B 2, T 1, K 1, R 1, d 0.5, K 1.5, 1 0.8, 2 0.5, 0.5, and M 1 (panel c); m 0.01, B 2, T 1, K 1, R 1, d 0.5, K 1.5, 1 0.8, 2 0.6, 0.5, and M 1 (panel d) (zero damping d 0.0) M 0.8 1 b 0.5 1 0.0006 M 0.8 0.5 M 0.4 M 0.8 M 1.2 y y 0.5 0 1 0.8 1 a 0 0.5 M 0.4 M 0.8 M 1.2 1 0.0004 0.0002 0 0.0002 T he mean velocity distribution, u y 0.002 0.0015 0.001 0.0005 T he mean velocity distribution, u y 0 1 0.5 d m 1 0.0 m 1 2.0 m 1 5.0 0.5 2 0.0 0.5 m1 2.0 m 1 0.0 m 1 2.0 m 1 5.0 0 y y 0 1 K 0.3 m 1 2.0 c 0.5 1 1 0.0025 0.001 0.0008 0.0006 0.0004 0.0002 The mean velocity distribution, u y 0.002 0.0015 0.001 0.0005 T he mean velocity distribution, u y Fig. 5 The variation of the mean velocity distribution and reversal flow for three different values of magnetic parameter M (panels a and b) and Hall parameter m 1 (panels c and d). The other chosen parameters are m 0.01, B 2, T 1, K 1, R 1, d 0.2, K 1.5, 1 0.8, 2 0.5, 0.5, 0.15, and m 1 0.5 (panel a); m 0.01, B 2, T 1, K 1, R 1, d 0.5, K 1.5, 1 1.2, 2 0.5, 0.5, 0.15, and m 1 0.5 (panel b); m 0.01, B 2, T 1, K 1, R 1, d 0.5, K 0.9, 1 0.8, 2 0.5, 0.5, 0.15, and M 0.5 (panel c); m 0.01, B 2, T 1, K 1, R 1, d 0.5, K 1.5, 1 0.8, 2 0.4 , 0.5, 0.15, and M 1 (panel d) M 0.4 M 0.5 10000 R 4.0 8000 M 0.6 M 0.5 6000 4000 a 0.5 0.6 0.7 0.8 Wave number, TCritical Values 8000 6000 K 1.2 m 1 1.0 4000 2000 0.9 1 0.9 6000 M 0.5 m 1 0.0 m 1 1.0 m 1 2.0 0.7 0.8 Wave number, 0.9 1 M 0.6 b 0.5 0.6 0.7 0.8 Wave number, 8000 2 0.1 6000 0.9 1 m 1 0.0 m 1 1.0 m 1 2.0 m 1 1.0 4000 2000 0.6 M 0.5 4000 1 c 0.5 8000 2000 TCritical Values 2000 M 0.4 10000 TCritical Values TCritical Values 12000 d 0.5 0.6 0.7 0.8 Wave number, 0.9 1 Fig. 6 The variation of critical values of the wall tension T with wave number for three different values of magnetic parameter M (panels a and b) and Hall parameter m 1 (panels c and d). The other chosen parameters are m 0.01, B 2, K 1, R 6, d 0.5, K 1.5, 1 0.8, 2 0.5, and m 1 0.5 (panel a); m 0.01, B 2, K 1, R 5, d 0.5, K 1.5, 1 1.6, 2 0.5, and m 1 0.5 (panel b); m 0.01, B 2, K 1, R 5, d 0.5, K 1.9, 1 0.8, 2 0.5, and M 0.5 (panel c); m 0.01, B 2, K 1, R 5, d 0.5, K 1.5, 1 0.8, 2 0.5, and M 0.5 (panel d) It is noted that the results of the hydrodynamic viscous fluid filling the porous medium of Hayat et al. [8] when M 0 can be obtained by choosing M 0 in our investigation. Also, the results of the hydrodynamic viscous fluid through non-porous medium of Abd Elnaby and Haroun [1] can be obtained by choosing 1 2 0 and M 0 in our investigation. 6. Conclusions In this study, the effects of physical parameters of interest are discussed for the constants D1 and D2, G ( y ) , u ( y ) , and Tc . The obtained results can be outlined and summarized as follows: The constants D1 and D2 increase with an increase in M and 2 , and decrease with an increase in d , K , and 1 . However, they behave differently with the Hall parameter m1 ; m1 has a decreasing effect on D1, while it has a increasing effect on D2. The mean velocity perturbation function G ( y ) increases by increasing M and 1 , while it decreases by increasing d , K , 2 , and m1 . The flow reversal increases with an increase in d , K , 1 , and m1 , and decreases with an increase in M and 2 . The critical value of T increases by increasing M , R , and 2 , and decreases by increasing m1 , K and 1 . The nonsymmetry of fluid motion was predicted since the mean flow at one boundary of the channel is not equal to that at the other boundary; accordingly, the result of the mean-velocity perturbation function being nonsymmetric is obtained. Moreover, Since the Hall effect cannot be taken into consideration unless there is a strong magnetic field imposed on the flow, so when there is no magnetic field, Hall effect vanishes. 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