IHJPAS. 36(2)2023 314 This work is licensed under a Creative Commons Attribution 4.0 International License Abstract The purpose of this research is to investigate the effects of rotation on heat transfer using inclination magnetohydrodynamics for a couple-stress fluid in a non-uniform canal. When the Reynolds number is low and the wavelength is long, math formulas are used to describe the stream function, as well as the gradient of pressure, temperature, pressure rise and axial velocity per wavelength, which have been calculated analytically. The many parameters in the current model are assigned a definite set of values. It has been noticed that both the pressure rise and the pressure gradient decrease with the rise of the rotation and couple stress, while they increase with an increase in viscosity and Hartmann number. The explanation of parameters is shown graphically by a series of figures using "MATHEMATICA". Keywords: Non-uniform channel, rotation, inclined MHD, Couple stress, Porous medium 1. Introduction Using a couple stress fluids as a model for describing biologically complicated fluids, such as colloidal fluids, polymeric suspensions, animal and human blood, and lubrication, is extremely beneficial in understanding a wide range of physical issues. One of the numerous models created to describe the reaction explanation of non-Newtonian fluids is the Couple stress fluid model. Non- Newtonian fluids, such as couple stress fluids, are those in which particle size is taken into account and studied by [1-4]. Shit and Ranjit [5] studied the fluid's peristalsis in non-uniform and asymmetric channels when an external magnetic field is provided. Murad and Abdulhadi [6] Analysis of mixed convective heat transfer for peristaltic transport of viscoplastic fluid: perturbation and numerical studies. Abdulla and Hummady [7] considered the influence of sliding speed on channel walls and the effect of nonlinear particle size. To make things even more complicated, non-Newtonian fluids can't be studied with non-slip boundary conditions because it's doi.org/10.30526/36.2.2987 Article history: Received 23 August 2022, Accepted 9 October 2022, Published in April 2023. Ibn Al-Haitham Journal for Pure and Applied Sciences Journal homepage: jih.uobaghdad.edu.iq The Effect of Rotation on the Heat Transfer of a Couple Stress Fluid in A Non- uniform Inclined Asymmetrical Channel with Inclined MHD Hanaa Abdulhussein Department of Mathematics, College of Science, University of Baghdad, Baghdad, Iraq. hshatty@uowasit.edu.iq Ahmed M. Abdulhadi Department of Mathematics, College of Science, University of Baghdad, Baghdad, Iraq. ahm6161@yahoo.com https://creativecommons.org/licenses/by/4.0/ mailto:hshatty@uowasit.edu.iq mailto:ahm6161@yahoo.com IHJPAS. 36(2)2023 315 easy to see how the walls slide. In technology, boundary slip condition fluids can be used to polish artificial hearts. See [8-13] for a list of studies that use this condition. Researchers have recently looked into how a magnetic field and rotation affect how fluid moves through an asymmetric channel, Abd-Alla and Abo-Dahab [14]. The effects of rotation and MHD on an asymmetric channel through a porous medium where a Jeffrey fluid flows nonlinearly have been looked at by Abdulhadi and Al-Hadad [15]. In porous media with non-symmetric canals, rotating waveform motion in two-dimensional channels of non-Newtonian fluid was explored by Alshareef [16]. For viscoplastic fluid and variable viscosity on peristalsis, they discussed the influence of rotation of the mixture on convection heat transfer analysis by [17, 18]. This study's objective is to examine the effects of rotation on heat transfer with inclination magnetohydrodynamics in a non-uniform channel containing a couple stress fluid. The equation for the governing equation is examined using low Reynolds approximations and long-wavelength assumptions, respectively. Graphs are used to show the impact of various factors on fluid flow. 2. mathematical Formulation Consider that the effect of a magnetic field and rotation on heat transfer can be explained by a porous medium with an inclined asymmetry of the couple stress fluid. Let's say π‘Œβˆ—Μ… =β„Ž1Μƒ (X Μƒ , t Μƒ ) and π‘Œβˆ—Μ… =β„Ž2Μƒ (X Μƒ, t Μƒ ) here is a representation of the channel's top and bottom walls. β„Ž1Μƒ (X Μƒ , t Μƒ ) =𝑑1 + ( οΏ½ΜƒοΏ½ βˆ’ 𝑐�̃�) tan οΏ½ΜƒοΏ½ + π‘Ž1 βˆ— cos [ 2πœ‹ πœ† (οΏ½ΜƒοΏ½ βˆ’ 𝑐�̃�)] (1) β„Ž2Μƒ (X Μƒ , t Μƒ ) =βˆ’π‘‘2 βˆ’ ( οΏ½ΜƒοΏ½ βˆ’ 𝑐�̃�) tan οΏ½ΜƒοΏ½ βˆ’ π‘Ž2 βˆ— cos [ 2πœ‹ πœ† (οΏ½ΜƒοΏ½ βˆ’ 𝑐�̃�) + πœ™Β°] (2) Where π‘Ž1 βˆ—π‘Žπ‘›π‘‘ π‘Ž2 βˆ— are the amplitudes of waves Ξ» is wavelength, οΏ½ΜƒοΏ½ is the time c is wave speed , (0 ≀ πœ™Β° ≀ πœ‹) the phase difference πœ™Β°between the walls of the channel the rectangular Cartesian coordinates are used οΏ½ΜƒοΏ½and οΏ½ΜƒοΏ½. The channel's axis is measured by οΏ½ΜƒοΏ½, and the transverse axis is measured by οΏ½ΜƒοΏ½, which is perpendicular to οΏ½ΜƒοΏ½. The constant heights of the upper and lower walls of the channel from the central line are denoted by 𝑑1π‘Žπ‘›π‘‘ 𝑑2, respectively. It's worth noting that πœ™Β° = 0 corresponds to an asymmetry with out-of-phase waves, whereas πœ™Β° = πœ‹ relates to waves that are in phase. Furthermore, 𝑑1 , 𝑑2, π‘Ž2 βˆ— , π‘Ž1 βˆ—and πœ™Β° satisfy the condition; π‘Ž1 βˆ—2 + π‘Ž2 βˆ—2 + 2π‘Ž1 βˆ—π‘Ž2 βˆ—π‘π‘œπ‘ πœ™Β° ≀ (𝑑1 + 𝑑2) 2. The governing equations. βˆ‚UΜƒ βˆ‚XΜƒ + βˆ‚VΜƒ βˆ‚YΜƒ = 0 (3) 𝜌 ( πœ•UΜƒ πœ•οΏ½ΜƒοΏ½ + UΜƒ πœ•UΜƒ πœ•οΏ½ΜƒοΏ½ + VΜƒ πœ•UΜƒ πœ•οΏ½ΜƒοΏ½ ) βˆ’ πœŒοΏ½Μ€οΏ½ (οΏ½Μ€οΏ½οΏ½ΜƒοΏ½ + 2 πœ•VΜƒ πœ•οΏ½ΜƒοΏ½ ) = βˆ’ πœ•PΜƒ πœ•XΜƒ + πœ‡βˆ‡2οΏ½ΜƒοΏ½ βˆ’ πœ‚βˆ‡4οΏ½ΜƒοΏ½ βˆ’ οΏ½ΜƒοΏ½π΅βˆ— 2 π‘π‘œπ‘  Ξ¦ (UΜƒ π‘π‘œπ‘  Ξ¦ βˆ’ VΜƒ 𝑠𝑖𝑛 Ξ¦) βˆ’ πœ‡ π‘˜Β° UΜƒ + 𝜌gοΏ½Μ‡οΏ½ (T βˆ’ TΒ°)𝑠𝑖𝑛�̃� + πœŒπ‘”π‘ π‘–π‘›Ξ±Μƒ (4) 𝜌 ( πœ•VΜƒ πœ•οΏ½ΜƒοΏ½ + UΜƒ βˆ‚VΜƒ βˆ‚XΜƒ + VΜƒ βˆ‚VΜƒ βˆ‚YΜƒ ) βˆ’ πœŒοΏ½Μ€οΏ½ (οΏ½Μ€οΏ½οΏ½ΜƒοΏ½ βˆ’ 2 πœ•UΜƒ πœ•οΏ½ΜƒοΏ½ ) = βˆ’ πœ•PΜƒ πœ•YΜƒ + πœ‡βˆ‡2VΜƒ βˆ’ πœ‚βˆ‡4VΜƒ + οΏ½ΜƒοΏ½π΅βˆ— 2 𝑠𝑖𝑛 Ξ¦ (UΜƒ π‘π‘œπ‘  Ξ¦ βˆ’ VΜƒ 𝑠𝑖𝑛 Ξ¦) βˆ’ πœ‡ π‘˜Β° VΜƒ βˆ’ πœŒπ‘”π‘π‘œπ‘ οΏ½ΜƒοΏ½ (5) πœŒπΆπ‘ ( πœ•T πœ•οΏ½ΜƒοΏ½ + UΜƒ πœ•T πœ•XΜƒ + VΜƒ πœ•T πœ•οΏ½ΜƒοΏ½ ) = KΜƒ ( βˆ‚2T βˆ‚οΏ½ΜƒοΏ½2 + βˆ‚2T βˆ‚οΏ½ΜƒοΏ½2 ) + πœ‡ [2 {( βˆ‚UΜƒ βˆ‚οΏ½ΜƒοΏ½ ) 2 + ( βˆ‚VΜƒ βˆ‚YΜƒ ) 2 } + ( βˆ‚UΜƒ βˆ‚οΏ½ΜƒοΏ½ + βˆ‚VΜƒ βˆ‚XΜƒ ) 2 ] + πœ‚ [( βˆ‚2UΜƒ βˆ‚XΜƒ2 + βˆ‚2UΜƒ βˆ‚οΏ½ΜƒοΏ½2 ) 2 + ( βˆ‚2VΜƒ βˆ‚οΏ½ΜƒοΏ½2 + βˆ‚2VΜƒ βˆ‚οΏ½ΜƒοΏ½2 ) 2 ] + οΏ½ΜƒοΏ½π΅βˆ— 2(UΜƒ π‘π‘œπ‘  Ξ¦ βˆ’ VΜƒ 𝑠𝑖𝑛 Ξ¦) 2 (6) IHJPAS. 36(2)2023 316 Where V′⃑⃑ ⃑=(οΏ½ΜƒοΏ½, VΜƒ, 0) be the velocity vector, Ξ©Μ€ is rotation, οΏ½Μ‡οΏ½ the Coefficient of thermal expansion , οΏ½ΜƒοΏ½ is the fluid pressure , 𝜌 is density of fluid , Ξ¦ is the inclination of the magnetic field angle, ΞΌ the dynamic viscosity , Ξ· is a constant linked to the couple stress, 𝐢𝑝 is the specific heat at constant pressure. impact Bβˆ—βƒ‘βƒ‘βƒ‘βƒ‘ =(π΅βˆ— 𝑠𝑖𝑛 Ξ¦ , π΅βˆ— π‘π‘œπ‘  Ξ¦ ,0) the magnetic field vector, π‘˜Β° is the permeability parameter ,T is the temperature , 𝑔 is the acceleration by gravity , οΏ½ΜƒοΏ½ is the fluids electrical conductivity ,KΜƒ is the thermal conductivity . The induced electric field is not taken into consideration at all, because assuming a low magnetic Reynolds number The fixed frame's(οΏ½ΜƒοΏ½ , οΏ½ΜƒοΏ½) flow field and the wave frame's(οΏ½Μ€οΏ½ , yΜ€) wave field are also considered the motions of an unsteady and steady-state . It's important to think about the relationship between the wave (οΏ½Μ€οΏ½ , yΜ€)and the fixed frames (οΏ½ΜƒοΏ½ , οΏ½ΜƒοΏ½) with a velocity of c as they move apart from one another as a result of the transformations below . vΜ€ = οΏ½ΜƒοΏ½ , yΜ€= YΜƒ , T = TΜƒ , xΜ€ = οΏ½ΜƒοΏ½ βˆ’ 𝑐�̃�, uΜ€ = οΏ½ΜƒοΏ½ βˆ’ 𝑐 , οΏ½Μ€οΏ½ = οΏ½ΜƒοΏ½ (7) In which (uΜ€, vΜ€) and (UΜƒ, VΜƒ)are the waves' and laboratories' velocities, respectively. the governing equations (3) ,(4) ,(5), and (6) be expressed in Wave frame as using the transformations mentioned above. βˆ‚uΜ€ βˆ‚xΜ€ + πœ•vΜ€ πœ•yΜ€ = 0 (8) 𝜌 ((uΜ€ + 𝑐) βˆ‚uΜ€ βˆ‚xΜ€ + vΜ€ πœ•uΜ€ πœ•yΜ€ ) βˆ’ πœŒοΏ½Μ€οΏ½ (𝛺 Μ€ (οΏ½Μ€οΏ½ + 𝑐) + 2 πœ•vΜ€ πœ•οΏ½ΜƒοΏ½ ) = βˆ’ πœ•οΏ½Μ€οΏ½ πœ•xΜ€ + πœ‡βˆ‡2uΜ€ βˆ’ πœ‚βˆ‡4uΜ€ βˆ’ οΏ½ΜƒοΏ½π΅βˆ— 2 π‘π‘œπ‘  Ξ¦ ((uΜ€ + 𝑐) π‘π‘œπ‘  Ξ¦ βˆ’ vΜ€ 𝑠𝑖𝑛 Ξ¦) βˆ’ πœ‡ π‘˜Β° (uΜ€ + 𝑐) + πœŒπ‘”οΏ½Μ‡οΏ½ (TΜƒ βˆ’ TΒ°)𝑠𝑖𝑛�̃� + πœŒπ‘”π‘ π‘–π‘›οΏ½ΜƒοΏ½ (9) 𝜌 ((uΜ€ + 𝑐) πœ•vΜ€ πœ•xΜ€ + vΜ€ πœ•vΜ€ πœ•yΜ€ ) βˆ’ πœŒοΏ½Μ€οΏ½ (𝛺 Μ€ vΜ€ βˆ’ 2 πœ•uΜ€ πœ•οΏ½ΜƒοΏ½ ) = βˆ’ πœ•οΏ½Μ€οΏ½ πœ•yΜ€ + πœ‡βˆ‡2vΜ€ βˆ’ πœ‚βˆ‡4vΜ€ + οΏ½ΜƒοΏ½π΅βˆ— 2 𝑠𝑖𝑛 Ξ¦ ((uΜ€ + 𝑐) π‘π‘œπ‘  Ξ¦ βˆ’ vΜ€ 𝑠𝑖𝑛 Ξ¦) βˆ’ πœ‡ π‘˜Β° vΜ€ βˆ’ πœŒπ‘”π‘π‘œπ‘ οΏ½ΜƒοΏ½ (10) πœŒπΆπ‘ ((uΜ€ + 𝑐) βˆ‚TΜƒ βˆ‚xΜ€ + vΜ€ βˆ‚TΜƒ βˆ‚yΜ€ ) = οΏ½ΜƒοΏ½ ( βˆ‚2TΜƒ βˆ‚xΜ€2 + βˆ‚2TΜƒ βˆ‚yΜ€2 ) + πœ‡ [2 {( βˆ‚uΜ€ βˆ‚xΜ€ ) 2 + ( βˆ‚vΜ€ βˆ‚yΜ€ ) 2 } + ( βˆ‚uΜ€ βˆ‚yΜ€ + βˆ‚vΜ€ βˆ‚xΜ€ ) 2 ] + πœ‚ [( βˆ‚2uΜ€ βˆ‚xΜ€2 + βˆ‚2uΜ€ βˆ‚y2 ) 2 + ( βˆ‚2vΜ€ βˆ‚xΜ€2 + βˆ‚2vΜ€ βˆ‚yΜ€2 ) 2 ] + οΏ½ΜƒοΏ½π΅βˆ— 2((uΜ€ + 𝑐) π‘π‘œπ‘  Ξ¦ βˆ’ vΜ€ 𝑠𝑖𝑛 Ξ¦) 2 (11) To reduce the number of additional parameters, we shall define the following non- dimensional quantities: π‘₯ = xΜ€ πœ† , 𝑦 = yΜ€ 𝑑1 , β„Ž1 βˆ—(π‘₯) = β„Ž1Μƒ (οΏ½Μ…οΏ½ ) 𝑑1 , β„Ž2 βˆ— (π‘₯) = β„Ž2Μƒ (οΏ½Μ…οΏ½ ) 𝑑1 ,πœƒΒ° = TΜƒβˆ’T0 T1βˆ’T0 , uβˆ— = uΜ€ 𝑐 , vβˆ— = πœ†vΜ€ 𝑐𝑑1 , tβˆ— = 𝑐�̃� πœ† ,𝑅𝑒 = π‘πœŒπ‘‘1 πœ‡ , 𝛿 = 𝑑1 πœ† , β„‹=Ξ’βˆ—π‘‘1√ οΏ½ΜƒοΏ½ πœ‡ , π‘ƒπ‘Ÿ = πœ‡ 𝐢𝑝 οΏ½ΜƒοΏ½ , 𝛾 = 𝑑1√ πœ‡ πœ‚ , π·π‘Ž = π‘˜πœŠ 𝑑1 2, πΉπ‘Ÿ = 𝑐2 𝑔𝑑1 (12) , 𝑑1 2 οΏ½Μ€οΏ½(οΏ½Μ€οΏ½) πœ†πœ‡π‘ = 𝑝 , π΅π‘Ÿ=π‘ƒπ‘Ÿ. 𝐸𝑐 , πΊπ‘Ÿ = 𝜌 𝑔(T1βˆ’T0) οΏ½Μ‡οΏ½ 𝑑1 πœ‡ 𝑐 , 𝐸𝑐 = 𝑐2 (T1βˆ’T0) 𝐢𝑝 . Where β„‹ is Hartmann number , 𝑅𝑒 is Reynolds number, 𝛿 is Wave number , 𝛾 is Couple stress parameter , π‘ƒπ‘Ÿ is Prandtl number , π·π‘Ž is Darcy number , πΉπ‘Ÿ is Froude number, π΅π‘Ÿ is Brinkman number , 𝐸𝑐 is Eckert number ,and πΊπ‘Ÿ is Grashof number . IHJPAS. 36(2)2023 317 According to equations (1) and (2), the dimensionless shape of the peristaltic channel walls may be shown in β„Ž1 βˆ—(π‘₯) and β„Ž2 βˆ—(π‘₯) β„Ž1 βˆ—(π‘₯) = 1 + π‘˜π‘₯ + π‘Ž cos(2πœ‹π‘₯) (13) β„Ž2 βˆ— (π‘₯) = βˆ’π‘‘ βˆ’ π‘˜π‘₯ βˆ’ 𝑏 cos(2πœ‹π‘₯ + πœ™Β°) (14) Where π‘Ž = π‘Ž1 βˆ— 𝑑1 , 𝑏 = π‘Ž2 βˆ— 𝑑1 , 𝑑 = 𝑑2 𝑑1 , π‘˜ = ( πœ† tan οΏ½ΜƒοΏ½ 𝑑1 ) is referred to as the channel's Non-uniform parameter and πœ™Β° the relation π‘Ž 2 + 𝑏2 + 2π‘Žπ‘π‘π‘œπ‘ πœ™Β° ≀ (1 + 𝑑) 2 Where(πœ“Β° ) stream function of velocity components u βˆ— and vβˆ— that is dimensionless uβˆ— = πœ•πœ“Β° πœ•π‘¦ and vβˆ— = βˆ’ πœ•πœ“Β° πœ•π‘₯ , respectively, and satisfy the continuity equation (8). In terms of stream function πœ“Β° , the dimensionless variables are specified in equations. (9), (10), and (11) were translated into the following equations. 𝑅𝑒. 𝛿 [( πœ•πœ“Β° πœ•π‘¦ . πœ• πœ•π‘₯ βˆ’ πœ•πœ“Β° πœ•π‘₯ . πœ• πœ•π‘¦ ) πœ•πœ“Β° πœ•π‘¦ + πœ•2πœ“Β° πœ•π‘₯πœ•π‘¦ ] βˆ’ πœŒΞ©Μ€2𝑑1 2 πœ‡ ( πœ•πœ“Β° πœ•π‘¦ + 1) + 2Ὼ𝑅𝑒𝛿 2 πœ• 2πœ“Β° πœ•π‘₯πœ• π‘‘βˆ— = βˆ’ πœ•π‘ πœ•π‘₯ + 𝛿2 πœ•3πœ“Β° πœ•π‘₯2πœ•π‘¦ + πœ•3πœ“Β° πœ•π‘¦3 βˆ’ 1 𝛾2 (𝛿4 πœ•5πœ“Β° πœ•π‘₯4πœ•π‘¦ + 2𝛿2 πœ•5πœ“Β° πœ•π‘₯2πœ•π‘¦3 + πœ•5πœ“Β° πœ•π‘¦5 ) βˆ’ β„‹2 π‘π‘œπ‘  Ξ¦ [( πœ•πœ“Β° πœ•π‘¦ + 1) π‘π‘œπ‘  Ξ¦ + πœ•πœ“Β° πœ•π‘₯ 𝛿 𝑠𝑖𝑛 Ξ¦] βˆ’ 1 π·π‘Ž ( πœ•πœ“Β° πœ•π‘¦ + 1) + 𝑅𝑒 πΉπ‘Ÿ sin Ξ±Μƒ + Gπ‘Ÿ ΞΈ sinΞ±Μƒ (15) 𝑅𝑒. 𝛿 3 [(βˆ’ πœ•πœ“Β° πœ•π‘¦ . πœ• πœ•π‘₯ + πœ•πœ“Β° πœ•π‘₯ . πœ• πœ•π‘¦ ) πœ•πœ“Β° πœ•π‘₯ βˆ’ πœ•2πœ“Β° πœ•π‘₯2 ] + πœŒΞ©Μ€2𝑑1 2 πœ‡ 𝛿2 πœ•πœ“Β° πœ•π‘₯ + 2Ὼ𝑅𝑒𝛿 2 πœ• 2πœ“Β° πœ•π‘¦πœ• π‘‘βˆ— = βˆ’ πœ•π‘ πœ•π‘¦ βˆ’ 𝛿2 (𝛿2 πœ•3πœ“Β° πœ•π‘₯3 + πœ•3πœ“Β° πœ•π‘¦2πœ•π‘₯ ) + 𝛿2 𝛾2 (𝛿4 πœ•5πœ“Β° πœ•π‘₯5 + 2𝛿2 πœ•5πœ“Β° πœ•π‘₯3πœ•π‘¦2 + πœ•5πœ“Β° πœ•π‘¦4πœ•π‘₯ ) + β„‹2 𝛿 𝑠𝑖𝑛 Ξ¦ [( πœ•πœ“Β° πœ•π‘¦ + 1) π‘π‘œπ‘  Ξ¦ + πœ•πœ“Β° πœ•π‘₯ 𝛿 𝑠𝑖𝑛 Ξ¦] + 𝛿2 π·π‘Ž . πœ•πœ“Β° πœ•π‘₯ βˆ’ 𝑅𝑒 πΉπ‘Ÿ 𝛿 π‘π‘œπ‘  οΏ½ΜƒοΏ½ (16) 𝑅𝑒. 𝛿. π‘ƒπ‘Ÿ ( πœ•πœ“Β° πœ•π‘¦ . πœ•πœƒΒ° πœ•π‘₯ + πœ•πœƒΒ° πœ•π‘₯ βˆ’ πœ•πœ“Β° πœ•π‘₯ . πœ•πœƒΒ° πœ•π‘¦ ) = (𝛿2 πœ•2πœƒΒ° πœ•π‘₯2 + πœ•2πœƒΒ° πœ•π‘¦2 ) + π΅π‘Ÿ [4𝛿 2 ( πœ•2πœ“Β° πœ•π‘₯πœ•π‘¦ ) 2 + ( πœ•2πœ“Β° πœ•π‘¦2 βˆ’ 𝛿 πœ•2πœ“Β° πœ•π‘₯2 ) 2 + 1 𝛾2 [(𝛿2 πœ•3πœ“Β° πœ•π‘₯2πœ•π‘¦ + πœ•3πœ“Β° πœ•π‘¦3 ) 2 + (𝛿2 πœ•3πœ“Β° πœ•π‘₯3 + πœ•3πœ“Β° πœ•π‘₯πœ•π‘¦2 ) 2 ]] + π΅π‘Ÿ β„‹ 2 [( πœ•πœ“Β° πœ•π‘¦ + 1) π‘π‘œπ‘  Ξ¦ + πœ•πœ“Β° πœ•π‘₯ 𝛿 𝑠𝑖𝑛 Ξ¦] 2 (17) Cross differentiation from dimensionless equations is used to remove the pressure term. (17), (18), and (19) may be formulated in the context of stream function differential equation and temperature under low Reynolds approximations and long-wavelength assumptions(Ξ΄<< 1) . πœ•6πœ“Β° πœ•π‘¦6 βˆ’ 𝛾2 πœ•4πœ“Β° πœ•π‘¦4 + 𝛾2 πœ•2πœ“Β° πœ•π‘¦2 [β„‹2 π‘π‘œπ‘ 2 Ξ¦ + 1 π·π‘Ž βˆ’ πœŒοΏ½Μ€οΏ½2𝑑1 2 πœ‡ ] = 0 (18) πœ•2ΞΈΒ° πœ•π‘¦2 + π΅π‘Ÿ [( πœ•2πœ“Β° πœ•π‘¦2 ) 2 + 1 𝛾2 ( πœ•3πœ“Β° πœ•π‘¦3 ) 2 ] + π΅π‘Ÿ β„‹ 2 π‘π‘œπ‘ 2 Ξ¦ ( πœ•πœ“Β° πœ•π‘¦ ) 2 = 0 (19) IHJPAS. 36(2)2023 318 The dimensionless boundary conditions in the wave frame are [5]: πœ•πœ“Β° πœ•π‘¦ + 𝛽 πœ•2πœ“Β° πœ•π‘¦2 = βˆ’1 π‘œπ‘› 𝑦 = β„Ž1 βˆ— πœ•πœ“Β° πœ•π‘¦ βˆ’ 𝛽 πœ•2πœ“Β° πœ•π‘¦2 = βˆ’1 π‘œπ‘› 𝑦 = β„Ž2 βˆ— πœ“Β° = 𝐹 2 , πœƒΒ° = 0 π‘œπ‘› 𝑦 = β„Ž1 βˆ— (20) πœ“Β° = βˆ’ 𝐹 2 , ΞΈΒ° = 1 π‘œπ‘› 𝑦 = β„Ž2 βˆ— πœ•3πœ“Β° πœ•π‘¦3 = 0 π‘œπ‘› 𝑦 = β„Ž1 βˆ—π‘Žπ‘›π‘‘ 𝑦 = β„Ž2 βˆ— As a result of solving equations (18) and (19), the associated boundary conditions (20) are satisfied. πœ“Β° = 2β…‡βˆ’π‘¦π‘Ž1𝑑1 π‘Ž3 + 2β…‡π‘¦π‘Ž1𝑑2 π‘Ž3 + 2β…‡βˆ’π‘¦π‘Ž2𝑑3 π‘Ž4 + 2β…‡π‘¦π‘Ž2𝑑4 π‘Ž4 + 𝑑5 + 𝑦𝑑6 (21) ΞΈΒ° = π‘Ÿ1 + π‘¦π‘Ÿ2 + 1 2𝛾2π‘Ž3 3π‘Ž4 3 (βˆ’ 1 2π‘Ž1 β…‡βˆ’2π‘¦π‘Ž1+3𝑦(π‘Ž1+π‘Ž2)βˆ’π‘¦(π‘Ž1+3π‘Ž2)(β„‹2 + 2β„‹2πΆπ‘œπ‘ [2𝛷] + β„‹2πΆπ‘œπ‘ [4Ξ¦] + 2𝑖ℋ2𝑆𝑖𝑛[2Ξ¦] + 𝑖ℋ2𝑆𝑖𝑛[4Ξ¦] + 4πΆπ‘œπ‘ [2Ξ¦]π‘Ž1 2 + 4𝑖𝑆𝑖𝑛[2Ξ¦]π‘Ž1 2). .. (22) It's possible to write the velocity as: W = βˆ’ 2π‘’βˆ’π‘¦π‘Ž1π‘Ž1𝑑1 π‘Ž3 + 2π‘’π‘¦π‘Ž1π‘Ž1𝑑2 π‘Ž3 βˆ’ 2π‘’βˆ’π‘¦π‘Ž2π‘Ž2𝑑3 π‘Ž4 + 2π‘’π‘¦π‘Ž2π‘Ž2𝑑4 π‘Ž4 + 𝑑6 (23) The axial pressure gradient can be calculated once we've identified the stream function. πœ•π‘ πœ•π‘₯ = πœ•3πœ“Β° πœ•π‘¦3 βˆ’ 1 𝛾2 . πœ•5πœ“Β° πœ•π‘¦5 βˆ’ β„‹2 π‘π‘œπ‘ 2 Ξ¦ [( πœ•πœ“Β° πœ•π‘¦ + 1)] βˆ’ 1 π·π‘Ž ( πœ•πœ“Β° πœ•π‘¦ + 1) + 𝑅𝑒 πΉπ‘Ÿ sin Ξ±Μƒ + Gπ‘ŸΞΈΒ° sinΞ±Μƒ + πœŒΞ©Μ€2𝑑1 2 πœ‡ ( πœ•πœ“Β° πœ•π‘¦ + 1) (24) πœ•π‘ πœ•π‘¦ = 0 (25) In non-dimensional form, the pressure rise per wavelength Ξ”π‘βˆ— is defined as Ξ”π‘βˆ— = ∫ πœ•π‘ πœ•π‘₯ 1 0 dx (26) 3.Volumetric flow rate In the laboratory frame, the volumetric flow rate is equal to οΏ½ΜƒοΏ½ = ∫ UΜƒ β„Ž1Μƒ β„Ž2Μƒ (XΜƒ , YΜƒ , tΜƒ )d YΜƒ (27) whereβ„Ž1Μƒ andβ„Ž2Μƒ are functions of οΏ½ΜƒοΏ½ and οΏ½ΜƒοΏ½ . In the wave frame, the volumetric flow rate is calculated: π‘žΒ° = ∫ uΜ€ β„Ž1Μƒ β„Ž2Μƒ (xΜ€ , yΜ€)d οΏ½Μ€οΏ½ (28) The relationship between 𝑄 and π‘ž can is calculated as follows: οΏ½ΜƒοΏ½ = π‘žΒ° + 𝑐(β„Ž1Μƒ βˆ’ β„Ž2Μƒ) (29) The time-mean flow over a span of time π‘‡βˆ— fixed in place οΏ½Μ…οΏ½ as 𝑄° = 1 π‘‡βˆ— ∫ �̃�𝑑𝑑 (30) π‘‡βˆ— 0 Using equation (29) in equation (30) the flow rate 𝑄° has the From 𝑄° = 1 π‘‡βˆ— ∫ π‘žΒ°π‘‘π‘‘ + π‘‡βˆ— 0 𝑐(β„Ž1Μƒ βˆ’ β„Ž2Μƒ) IHJPAS. 36(2)2023 319 = π‘žΒ° + 𝑐𝑑1 + 𝑐𝑑2 + 2𝑐π‘₯πœ† tan οΏ½ΜƒοΏ½ + π‘π‘Ž1 cos(2πœ‹π‘₯) + π‘π‘Ž2 cos(2πœ‹π‘₯ + πœ™Β°) (31) The non-dimensional of equation (28) is provided by πœ” = 𝐹 + 1 + 𝑑 + 2π‘˜π‘₯ + π‘Ž cos(2πœ‹π‘₯) + 𝑏 cos(2πœ‹π‘₯ + πœ™Β°) (32) where πœ” = 𝑄° cd1 and F = π‘žΒ° cd1 has the expression in the form 𝐹 = ∫ πœ•πœ“Β° πœ•π‘¦ β„Ž1 βˆ— β„Ž2 βˆ— dy = πœ“Β°(β„Ž1 βˆ—) βˆ’ πœ“Β°(β„Ž2 βˆ—) (33) 4. Results and Discussion This section focuses on " velocity"W, "temperature" ΞΈΒ°, " gradient of pressure " Ξ΄P βˆ—, "pressure rise" Ξ”π‘βˆ— , and "stream function" πœ“Β° . To get the numerical values corresponding to the above- mentioned analytical formulas, we utilized "MATHEMATICA " program. 4.1. The distribution of velocity Now, we'll look at the effect of axial velocity (W) variation across the canal on several parameters. Note that the velocity is parabolic. In the center, the axial velocity rises with increasing rotation parameter " οΏ½Μ€οΏ½", density "ρ", the width of the channel "𝑑1", Darcy number " π·π‘Ž" and the magnetic field inclination angle "Ξ¦", whereas the axial velocity reduces near the channel wall's edge, as seen in Figure 1 (a-e). According to Figure 1(f) "πœ™Β°", is shown to increase axial velocity in the middle of the canal while axial velocity lowers at one wall boundary and rises at the other. As can be seen in Figures 1(g-k), as " β„‹ ", "Ξ³", "Ξ²", viscosity "ΞΌ", and " k" increase, the axial velocity decreases in the channel's middle while increasing near the channel's wall border. (a) (b) (c ) (d) (e) (f) IHJPAS. 36(2)2023 320 (g) (h) (i) (j) (k) Figure 1.Variation the axial velocity "W" with different parameters {π·π‘Ž =0.5 , β„‹ = 3 , 𝛾 = 2 , π‘Ž = 0.6, πœ‡ = 0.1 , οΏ½Μ€οΏ½ = 1 , 𝑏 =0.7 , πœ™Β° = πœ‹ 6 , 𝑑 = 1 , 𝛽 =0.1 , Ξ¦ = πœ‹ 4 , π‘˜ =0.2 , π‘₯ = 1 , 𝜌 =0.5 , 𝐹 = 1 , 𝑑1 = 0.2} 4.2. Pumping characteristics In this subsection, we will analyze the pressure through the channel. 4.2.1. pressure gradient" π›…πβˆ— " Each of the figures in this section illustrates the pressure gradient and the axial axis of fluctuation along the canal at one wavelength π‘₯ ∈[0,1]. Figures like this show that flow is restricted in the narrowing portion of channel π‘₯ ∈[0.2,0.6]. As a result, a larger pressure gradient is needed to achieve a normal flow. Because of the smaller pressure gradient in the larger area of the channel π‘₯ ∈ [0,0.2]βˆͺ [0.6,1] fluid may pass readily. Figure 2(a-b) shows that when viscosity "πœ‡" and the Hartmann number" β„‹" raises, the pressure gradient also increases in size. This graphic shows that greater pressure is required to move some volume of fluid through the narrower region of the channel. When looking at channel parameters such as the magnetic field inclination angle "Ξ¦" , the inclination" 𝛼 Μƒ" of the channel, rotation parameter " οΏ½Μ€οΏ½" ,density "𝜌" ,width of the channel "𝑑1" , Grashof numbers "Gπ‘Ÿ" ,slip parameter"𝛽", Darcy number " π·π‘Ž" , Reynolds number"𝑅𝑒",couple stress "𝛾" , temperature "ΞΈΒ° ", the phase difference " πœ™Β°" and Non-uniformity "π‘˜" as depicted in Figures 2( c –o), the pattern is the opposite. Because of the inclination, less pressure is needed to move liquids. IHJPAS. 36(2)2023 321 4.2.2. pressure rise" πš«π©βˆ— " Figures 3(a-o) show the relationship between pressure rise and volumetric flow rate. The connection between pressure rise and the rate of volumetric flow for each wavelength is seen to be linear. The whole region is considered into five parts (1) the peristaltic pumping region where(βˆ†π‘βˆ— > 0, 𝐹 > 0) (2) when (βˆ†π‘βˆ— > 0 , 𝐹 < 0), then it is a retrograde pumping region (3) augmented pumping (co-pumping) region where (βˆ†π‘βˆ— < 0 , 𝐹 > 0) (4) There is a co-pumping region where (βˆ†π‘βˆ— < 0 , 𝐹 < 0) (5) (βˆ†π‘βˆ— = 0)corresponds to the free pumping region. Figure3 (a-b) shows the impact of viscosity "πœ‡" and Hartmann number " β„‹ "on βˆ†π‘βˆ— on It has been noticed in the retrograde pumping region. The pumping rate increases as Hartmann number "β„‹"increases. Co-pumping reduces when in this region and increases in " β„‹ "and "πœ‡" . Volumetric flow rate and pressure increase βˆ†π‘βˆ— are shown to be linearly related in Figures 3 (c - f ) for a variety of Grashof numbers "Gπ‘Ÿ" , "𝑅𝑒", " οΏ½ΜƒοΏ½" and "ΞΈΒ° ". We observed that a rise results in an increase in retrograde pumping rate and augmented pumping (co-pumping) region an increase in the pressure rise. Figures 3 (g - m ) Graph shows that with an increase in rotation parameter " οΏ½Μ€οΏ½" ,density "𝜌" ,width of the channel "d1", " π·π‘Ž", "𝛽", "𝛾" and" Ξ¦ " . the pumping rate decreases in the region of retrograde pumping while in the augmented pumping region found to increase. Figure 3 (n)shows an impact of channel non-uniform parameter "π‘˜"on βˆ†π‘βˆ—. It is observed that in a retrograde pumping region and a free pumping region (βˆ†π‘βˆ— = 0), the pumping rate decreases with an increase in "π‘˜". Figure 3 (o) depicts the effect of "πœ™Β°" on βˆ†π‘βˆ—. It is observed that in a retrograde pumping region and a free pumping region (βˆ†π‘βˆ— = 0), the pumping rate increases with an increase in"πœ™Β°" . )a) (b( )c) (d) )e) (f) IHJPAS. 36(2)2023 322 (g) (h( (i) (j) (k) (l) (m) (n) (o) Figure 2. Variation the pressure gradient" Ξ΄Pβˆ— with different parameters {π·π‘Ž =0.5 , β„‹ = 3 , 𝛾 = 2 , π‘Ž = 0.6, πœ‡ = 0.1 , οΏ½Μ€οΏ½ = 1 , 𝑏 =0.7 , πœ™Β° = πœ‹ 6 , 𝑑 = 1 , 𝛽 =0.1 , Ξ¦ = πœ‹ 4 , π‘˜ =0.2 , 𝑦 = 1 , 𝜌 =0.5 , 𝐹 = 0.1 , 𝑑1 = 0.2 , πΉπ‘Ÿ = 0.5 , οΏ½ΜƒοΏ½ = πœ‹ 6 , πΊπ‘Ÿ = 1 , Θ° = 1} IHJPAS. 36(2)2023 323 (a) (b) (c) (d) (e) (f) (g) (h) (i) (j) IHJPAS. 36(2)2023 324 (k) (l) (m) (n) (o) Figure 3 . Variation the pressure rise π›₯π‘βˆ— with different parameters {π·π‘Ž =0.5 , β„‹ = 3 , 𝛾 = 2 , π‘Ž = 0.6, πœ‡ = 0.1 , οΏ½Μ€οΏ½ = 1 , 𝑏 =0.7 , πœ™Β° = πœ‹ 6 , 𝑑 = 1 , 𝛽 =0.1 , Ξ¦ = πœ‹ 4 , π‘˜ =0.2 , 𝑦 = 1 , 𝜌 =0.5 , 𝐹 = 0.1 , 𝑑1 = 0.2 , πΉπ‘Ÿ = 0.5 , οΏ½ΜƒοΏ½ = πœ‹ 6 , πΊπ‘Ÿ = 1 , Θ° = 1} 4.3. temperature profile "𝛉° " An examination of the fluid temperature profile for a fixed value of x = 1 yields a parabolic temperature profile, with a higher graph in the middle. Fluids that have a high viscosity are more likely to convert kinetic energy into internal energy, which causes them to get hotter. There is no doubt about that. Its flow and movement resistance diminish with increasing temperature, a phenomenon caused by the tiny distances between molecules and the cohesive forces that exist between them. Figures 4 (a-g) show that the temperature increases values " οΏ½Μ€οΏ½" , "𝜌" , "d1" " π·π‘Ž" ," H " , "π‘˜"and "π΅π‘Ÿ"increase, so does the temperature in the channel's center and temperature parabolic. The increase in temperature is accompanied by "π΅π‘Ÿ". π΅π‘Ÿπ‘–π‘›π‘˜π‘šπ‘Žπ‘› number "π΅π‘Ÿ" of raised flow resistances given by shear. As parameter values "πœ‡" , " "Ξ¦ " "𝛽", "𝛾"and "πœ™Β°" increase, they show that the temperature decreases in Figures 4 (h-l ). (a) (b) IHJPAS. 36(2)2023 325 (c) (d) (e) (f) (g) (h) (i) (j) (k) (l) Figure 4. Variation the temperature "ΞΈΒ° " with different parameters {π·π‘Ž =0.5 , β„‹ = 3 , 𝛾 = 2 , π‘Ž = 0.6, πœ‡ = 0.1 , οΏ½Μ€οΏ½ = 1 , 𝑏 =0.7 , πœ™Β° = πœ‹ 6 , 𝑑 = 1 , 𝛽 =0.1 , Ξ¦ = πœ‹ 4 , π‘˜ =0.2 , π‘₯ = 1 , 𝜌 =0.5 , 𝐹 = 0.1 , 𝑑1 = 0.2 , π΅π‘Ÿ = 1} 4.4. The trapping phenomena In order to explain the trapping phenomena, the formation of a circulating bolus of fluid, which is a closed streamline region, at the speed of the wave. There will be points in the wave frame where the fluid's velocity is zero due to the trapping phenomenon. The volumetric flow rate via a line linking any two places is computed by taking into account the difference in stream function values at the two sites in question, which is why studying streamline patterns is so IHJPAS. 36(2)2023 326 important. Figures 5–15 indicate that bolus formation occurs from both sides of the center line in the extended region. Bigger and larger volumes of the trapped bolus can be extracted from the system by raising the strength of the magnetic field in Figures ( 5-9) (a, b, and c), as "Ξ¦ " , " οΏ½Μ€οΏ½", "𝜌" , "d1" and " π·π‘Ž". In Figures (10 and 11) (a ,b and c), as " πœ™Β°" and "πœ‡" changes, so does the variation in streamlines. According to our research, we've found that bolus sizes decrease"πœ‡" and " πœ™Β°" increase. The Figure 12(a ,b and c) shows that the wall draws fluid in the widest section of the duct, but this fluid is pushed away from the wall in the narrower section and the bolus disappears in the central part as "𝛽" increases. Graphing the non-uniformity parameter "π‘˜"of the asymmetric channel as shown in Figure 13(a, b, and c), when it is raised, the trapped bolus decreases in size and migrates downstream. These figures 14and15 (a, b, and c) demonstrate how In increasing the Hartman number " β„‹ " ,and couple stress "𝛾" , the incidence of trapped bolus diminishes in size and vanishes in the direction of downstream, Another effect that may help protect red blood cells and other elements is the tendency to reduce bolus volume. (a) (b) (c) Figure 5. Distribution of streamlines " πœ“Β°" for (a) "Ξ¦" = Ο€/4 (b) "Ξ¦" = Ο€/3 (c) "Ξ¦"= 2Ο€/5 (a) (b) (c) Figure 6. Distribution of streamlines " πœ“Β°" for (a) " οΏ½Μ€οΏ½" =1 (b) " οΏ½Μ€οΏ½" =2 (c) " οΏ½Μ€οΏ½" =4 (a) (b) (c) Figure 7.Distribution of streamlines " πœ“Β°" for (a) "𝜌" = 0.5 (b) "𝜌" = 2 (c) "𝜌" = 6 IHJPAS. 36(2)2023 327 (a) (b) (c) Figure 8. Distribution of streamlines " πœ“Β°" for (a) "𝑑1" =0.2 (b) "𝑑1" =0.8 (c) "𝑑1" =1 (a) (b) (c) Figure 9 . Distribution of streamlines" πœ“Β°" for (a) " π·π‘Ž" =0.5 (b) " π·π‘Ž" =2 (c) " π·π‘Ž" =6 (a) (b) (c) Figure 10 . Distribution of streamlines " πœ“Β°" for (a) "πœ‡" =0.1 (b)"πœ‡" =0.4 (c) "πœ‡" =1 (a) (b) (c) Figure 11. Distribution of streamlines " πœ“Β°" for (a) "πœ™Β°" = πœ‹ 6 (b) "πœ™Β°" = πœ‹ 3 (c) "πœ™Β°" = πœ‹ 2 IHJPAS. 36(2)2023 328 (a) (b) (c) Figure 12. Distribution of streamlines " πœ“Β°" for (a) "𝛽" =0.1 (b) "𝛽" =0.5 (c) "𝛽" =1 (a) (b) (c) Figure 13. Distribution of streamlines " πœ“Β°" for (a) "k" =0.2 (b) "π‘˜" = 0.4 (c) "π‘˜"=0.6 (a) (b) (c) Figure 14. Distribution of streamlines " πœ“Β°" for (a) " β„‹ " =3 (b) " β„‹ " = 4 (c) " β„‹ "=8 (a) (b) (c) Figure 15. Distribution of streamlines " πœ“Β°" for (a) "𝛾" =2 (b) "𝛾" =3 (c) "𝛾" =4 5. Conclusions In this research, we studied the effects of rotation and incline magnetohydrodynamics to investigate the effects of heat transfer and couple stress fluid as they move via an inclined asymmetric channel and porous medium under low Reynolds approximations and long- wavelength assumptions in the transport of bodily fluids by the use of non-Newtonian fluid models. Analytically, using Mathematica software. This investigation focused on studying the distribution of velocity, the pumping characteristics, the distribution of temperature, and the trapping phenomena. IHJPAS. 36(2)2023 329 1. It notes that the temperature and profile of velocity are parabolic. 2. There is a decrease in axial velocity "W" in the central region when increasing the viscosity "πœ‡" , "𝛾" , " β„‹ ","𝛽", and "π‘˜"", but there is a rise in velocity at the boundary of the channel wall. 3. There is an increase in axial velocity "W" in the central region when increasing the rotation parameter " οΏ½Μ€οΏ½", "πœ™Β°" , density "𝜌" , "Ξ¦ ", "d1" and " π·π‘Ž", but there is a decrease in velocity at the boundary of the channel wall. 4. When the viscosity "πœ‡" , and Hartmann number " β„‹ "are increased, the pressure gradient " Ξ΄Pβˆ— " increases, while " οΏ½Μ€οΏ½", "Ξ¦" , "Ξ²", " 𝛼 Μƒ", "Gπ‘Ÿ", " π·π‘Ž", "𝛾", "πœ™Β°", "𝜌", "π‘˜", "d1" , "𝑅𝑒" ,and "ΞΈΒ° " decrease. 5. The connection between pressure rise " Ξ”π‘βˆ— "and volumetric flow rate for each wavelength is seen to be linear. 6. In retrograde pumping, increases " Ξ”π‘βˆ— " pressure rise with the increasing values the viscosity "πœ‡" , "Gπ‘Ÿ","𝑅𝑒" , " H ", "ΞΈΒ° " ," 𝛼 Μƒ" and "πœ™Β°", whereas it decreases with the rising values the rotation parameter " οΏ½Μ€οΏ½", "Ξ¦", " π·π‘Ž" , "𝛾" , "𝛽" ,density "𝜌" , "d1" ,and" k". 7. The temperature "ΞΈΒ° " rises when the rotation parameter " οΏ½Μ€οΏ½", density "𝜌" , "d1" , "π‘˜" , " π·π‘Ž" , " β„‹" and Brinkman number"π΅π‘Ÿ" all go up. It goes decrease when the inclination magnetic field angle "Ξ¦", the slip parameter "𝛽" , couple-stress parameter"𝛾" , phase difference "πœ™Β°" , and the viscosity "πœ‡" all go up. 8. When the values of" β„‹"and "Ξ³" are increased, the trapped boluses are eliminated. The inclination magnetic field angle "Ξ¦", " οΏ½Μ€οΏ½", "𝜌" , "d1" and " π·π‘Ž" have a increasing impact on the bolus size. References 1. Mekheimer, Kh. S. Effect of induced magnetic field on peristaltic flow of a couple stress fluid. 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