A New Algorithm Based SLM to Find Critical Eigenvalue in the Rayleigh-Bénard-Brinkman Convection Problem with Boundary Conditions
|
|
- Sharlene Wheeler
- 5 years ago
- Views:
Transcription
1 Advances in Computational Sciences and Technology ISSN Volume 10, Number 6 (017) pp Research India Publications A New Algorithm Based SLM to Find Critical Eigenvalue in the Rayleigh-Bénard-Brinkman Convection Problem with Boundary Conditions Dr. Ashoka S. B. MCA., Ph.D. Department o Computer Science, MSCWB, Bangalore , India. Abstract An eigen boundary value problem is solved or the critical eigenvalue in the case o a Rayleigh-Bénard-Brinkman convection problem bounded by permeable walls with Robin boundary condition on temperature and general boundary condition on velocity. Unknown initial values and guess eigenvalue required to initiate the successive linearization method are obtained using the single-term Rayleigh-Ritz method. The local thermal non-equilibrium between the solid and luid phases in the Newtonian luid-saturated porous medium results in coupled partial dierential equations. It is shown that ive steps o the method results in a convergent solution with an accuracy o 6 decimal digits. Keywords: porous medium, local thermal non-equilibrium, convection, linear stability, successive linearization method 1. INTRODUCTION Convection in porous medium usually known as the Horton-Rogers-Lapwood problem has been the ocus o interest o many researchers over the past several decades. The study initiated by Horton and Rogers [1] and Lapwood [] is a porous medium version o Rayleigh-Bénard problem in a clear luid layer and has wide variety o practical applications. These include oil reservoir modeling, geothermal engineering, building thermal insulation, grain storage and nuclear waste repository
2 1558 Dr. Ashoka S. B. and so on. A comprehensive study on the convection in porous media is well documented in the books Ingham and Pop [3], Nield and Bejan [4] and Vaai [5]. Most o the studies in literature concerning Horton-Rogers-Lapwood problem assume that there is no temperature dierence between the luid and solid phases, at any location o the porous medium system. This is called as local thermal equilibrium (LTE) model. In many practical situations LTE model ails to comprehend the heat transport in porous medium. Hence it is important to assume that the solid and luid phases are not in local thermal equilibrium by considering two-ield model o the energy equation and this model is popularly non as the local thermal non-equilibrium (LTNE) model in the literature. Heat pipes, cooling o computer chips, ood processing, microwave heating are ew applications where LTNE eects are predominant. Vowing to these applications there have been number o works in literature concerning the LTNE model. Banu and Rees [6] were the irst amongst others to study the onset o Darcy-Bénard convection using a LTNE model and obtained the critical Rayleigh number as a unction o local thermal non-equilibrium parameters. Postelnicu and Rees [7] extended the work o Banu and Rees [6] to Darcy-Brinkman-Bénard convection by considering a orm-drag term, using a thermal non-equilibrium with stress-ree boundaries. It was shown that the inclusion o quadratic drag term in the momentum equation has no eect on stability criteria since the basic state being motionless. Further, they recovered LTE results by perorming asymptotic analysis or large inter-phase heat transer coeicient H. Malashetty, et. al. [8] studied the onset o Lapwood-Brinkman convection using a LTNE model and reiterated the results obtained by Postelnicu and Rees [7]. Nouri-Borujerdi et. al. [9] studied the eect local thermal non-equilibrium on conduction in a luid saturated porous channel with a uniorm heat source and obtained conditions under which the LTNE can be assumed. Postelnicu [10] extended the earlier work by Postelnicu and Rees [7] to rigid boundaries and gave a quantitative comparison between the results o stress-ree and rigid boundaries. Above-cited works concern Newtonian liquid as a working medium. In recent past non-newtonian luids are being used in place o their Newtonian counterparts as most o the industrially important luids exhibit non- Newtonian characteristics. With this view point researchers have extended the use o LTNE eects in non-newtonian luid saturated porous medium. For example, Shivakumara et. al. [11] studied the onset o convection in a viscoelastic luidsaturated sparsely packed porous layer using a thermal non-equilibrium model. They showed that viscoelastic eects enhance stabilizing eect o the interphase heat transer coeicient. Recently, Malashetty et. al. [1] studied the eect o thermal nonequilibrium on the onset o convection in a couple stress luid saturated porous layer and showed that interphase heat transer coeicient increases the critical Rayleigh number or the onset o convection with the increasing values o couple stress parameter. In literature there are works addressing the LTNE on the double diusive convection in a luid saturated porous layer. Double diusive convection in a porous
3 A New Algorithm Based SLM to Find Critical Eigenvalue layer using a thermal non-equilibrium model was studied by Malashetty et. al. [13] and they showed that interphase heat transer coeicient has a signiicant say on the stationary, oscillatory and inite amplitude double diusive convection in a luid saturated porous medium. Malashetty and Heera [14] and Malashetty et. al. [15] perormed linear and non-linear stability analyses o the double diusive convection in a rotating porous layer (tightly/sparsely packed) using a thermal non-equilibrium model. In these studies it was shown that the rotation increases the stabilizing eect o interphase heat transer coeicient in all the three modes o double diusive convection, namely, stationary, oscillatory and inite amplitude. Works o Malashetty et. al. [16] and Shivakumara et. al. [17] takes into account o thermal non-equilibrium eects on convective instability in an anisotropic porous layer. In all the studies mentioned so ar concerning LTNE either stress-ree or rigid boundaries with isothermal conditions are made use. But, the interace conditions (slip conditions) and the thermal boundary conditions o the third type are the most general and practical boundary conditions. To the best o authors knowledge there are no works concerning Rayleigh-Bénard-Brinkman convection with LTNE and two boundary condition. Hence, we propose to investigate the same in the present paper.. Mathematical Formulation We consider a layer o luid saturated porous medium o depth d which is heated rom below and cooled rom above, as depicted in Figure 1. The upper surace is held at a temperature T 0 while the lower one is at T 0 T. It is assumed that both orm-drag and boundary eects are signiicant, that the porous medium is isotropic but that local thermal equilibrium does not apply. Thus the governing equations, i.e., the continuity, momentum and energy equations, subject to the Boussinesq approximation, take the orm q t q 0, (1) 1 q q p q q K e T c c q. T k T hts T, t s 1 c 1 ks Ts hts T s T t 0 g T T k ˆ, (), (3) (4)
4 1560 Dr. Ashoka S. B. Fig. 1. Schematic diagram o the physical coniguration. where, q u, v is the velocity vector, t is time, is the density, is the porosity o the porous, medium, p is the pressure, e is the eective viscosity, K is the permeability o the porous medium, is the coeicient o thermal expansion, g is acceleration due to gravity, c is speciic heat at constant pressure, T is the temperature, k is the thermal conductivity, h is the inter-phase heat transer coeicient. Further, the properties o luid phase are indicated with the subscript and those o solid phase are denoted by the subscript s. The ollowing velocity boundary conditions at the permeable walls are made use (see, Siddheshwar [18]): u 1 v 0, u at y 0, y K u v 0, u at y d. y K (5) Here, 1 and are dimensionless quantities depending on the material parameters which characterizes the structure o the permeable boundary membranes. We deine the ollowing dimensionless variables
5 A New Algorithm Based SLM to Find Critical Eigenvalue c d,,,, d k * * * x y x y t t k,,, c d c d * * * q u v u v q k * e k T T0 Ts T0 p p,,. c K T T (6) Using (6) in equations (1) - (4) and dropping asterisks or simplicity, we obtain Da Pr q 0, (7) q 1 ˆ q q p q q Ra j, (8) t q. H t M t, (9) H. (10) The non-dimensional numbers appearing in equations (7) - (10) are: Da e K d the Darcy number, Pr c k e the Prandtl number, gkdt Ra the Darcy-Rayleigh number, k hd H k the inter-phase heat transer parameter, k (1 ) k s the porosity-scaled conductivity ratio and M ( c) ( c) s k k s the diusivity ratio.
6 156 Dr. Ashoka S. B. The usual Rayleigh number, which is based on the mean properties o the porous medium, is given by 1 * Ra R. We now introduce the steam unction xy, that takes care o continuity equation (7) as ollows u, v. y x (11) We substitute equation (11) into equations (8) - (10) and eliminating pressure rom the momentum equation we get the ollowing equations: Da, 4 Da Pr t x, y Ra, x, H t x, y M t (1), (13) H. (14) The basic state is assumed to be quiescent and the heat transport takes place through conduction alone and hence we have 0, 1 y, 1 y. (15) b b b We now superimpose a small perturbation on the basic state as ollows, 1 y, 1 y. (16)
7 A New Algorithm Based SLM to Find Critical Eigenvalue Substituting equation (16) in equations (1) - (14) and linearizing we obtain Da Pr t t Ra, (17) x Da 4 x H M t, (18) H. (19) It can be easily proved that equations (17) - (19) obey the principal o exchange o stabilities and hence the time derivative terms in those equations can be neglected to get 0 Da Ra x y x y x, (0) x H 0 x y y x H 0, (1). () The boundary conditions or the perturbed variables are assumed in the ollowing orm 0, Ds 0, 0 L BiL y y y y * and BiL 0 at y 0 0, Ds 0, 0 U BiU y y y y * and BiU 0 at y 1, (3). (4) Here, DsL 1d K is the slip Darcy number at the lower surace, DsU d K is the slip Darcy number at the upper surace, Bi, Bi are the Biot numbers o the luid L U
8 1564 Dr. Ashoka S. B. * * phase at lower and upper suraces respectively, Bi, Bi are the Biot numbers o the solid phase at lower and upper suraces respectively. Equations (0) () admit solutions in the orm L U x, y cos kx y x, y sin kx y x, y sin kx y (5) where k is the horizontal wave number. By substituting equation (5) into equations (0) - (4) the ollowing set o equations is obtained: Da D k 1 D k Rak 0, (6) D k k H 0, (7) D k H 0, (8) 0, D DsLD 0, D BiL 0 * and D BiL 0 at y 0, (9) 0, D DsUD 0, D Bi U 0 * and U 0 at 1 D Bi y. (30) Equations (6) - (30) are solved using successive linearization method by treating Ra as an extra variable. The details o the method are discussed in the paper by Narayana et al. [19]. The initial solutions or the successive linearization method were obtained through single-term Galerkin method in the ollowing orm: 4 3 y y a1 y a y a3 y, y y a4y a5, y y a6y a7, (31) where, 1 5DsL 3DsU DsLDsU a1 1 4 Ds Ds Ds Ds L U L U,
9 A New Algorithm Based SLM to Find Critical Eigenvalue DsL 6 DsU a 1 4 Ds Ds Ds Ds L U L U U 6Ds a3 1 4 Ds Ds Ds Ds L U L U,, a a U 4 Bi Bi a, a L 4 5 BiU BiL BiLBiU BiL * * BiL BiU a6 6, a * * * * 7 * BiU BiL BiLBiU BiL,. It should be noted here that DsL, DsU 0represents stress-ree boundaries and DsL, DsU represents rigid boundaries. Similarly, the case BiL, BiU 0 represents adiabatic type temperature boundary condition while BiL, BiU represents isothermal type boundary condition. Other combinations o boundary conditions are obtained or some particular choice o values o these parameters. 3. RESULTS AND DISCUSSION A semi-analytical study is made o the linear stability analysis or the Rayleigh- Bénard-Brinkman convective instability problem that assumes local thermal nonequilibrium between the luid and solid phases and that considers general boundary conditions on velocity and temperatures. The governing equations result in a twopoint eigen boundary value problem with third type boundary conditions. It is the boundary conditions that pose obstacles in obtaining an analytical expression or the eigen value Rac (critical Rayleigh number). The most general ormulation o the problem acilitates the handling o limiting case problems which at the present time are being tackled as -independent problems. The integrated approach to the convective instability problem gives a new direction to the investigation o such problems. The main diiculty in solving such EBVP' s with generalized boundary conditions concerns convergence o the schemes, iterative or otherwise. In this paper we propose the successive linearization method (SLM). The method when used in the original orm does pose problems in the case o general boundary conditions. The usual problems encountered are the ollowing: 1. Sensitivity o the convergence o the solution to the choice o initial unknown guess values and eigen values.. Extreme values o the parameters many a time slow down convergence and warrant use o acceleration procedures.
10 1566 Dr. Ashoka S. B. 3. Greater accuracy i required or the eigen values would mean greater the intensity o the above two problems. 4. Choice o basis unctions also makes contributions to all the three computational problems noted above. In the present problem we have circumvented all the above hurdles by adopting the ollowing scientiic procedure: The elegance in the SLM method can be appreciated only when it is implemented in an automated way in the chosen computer program. Since MATLAB implements algorithms mostly through matrices, the SLM based procedure that leans heavily on matrix based concepts is ideally suited or Chebyshev-based spectral SLM method. SciLab is another such package (open source) that provides natural support or implementation o SLM procedure STRESS-FREE BOUNDARIES RIGID BOUNDARIES Da = 0, H = 10 -, = 1 35 Ra c Bi L, Bi U Fig.. Critical Rayleigh number as a unction o Biot numbers o luid phase. We now move on to discuss some o the important results obtained through the computation. It is observed that the critical eigen value o permeable surace lies in between those o the stress-ree and rigid boundaries, i.e., (Rac)Free (Rac)Permeable (Rac)Rigid. These results are in line with those reported by Siddheshwar [18]. Also, the critical Raleigh number corresponding to the Robin type temperature boundary conditions lies in between those o isothermal and adiabatic type o temperature boundary conditions, i.e., (Rac)Adiabatic (Rac)Robin (Rac)Isothermal.
11 A New Algorithm Based SLM to Find Critical Eigenvalue Figure airms the above statement or both stress-ree and rigid boundaries. As mentioned earlier, the case BiL, BiU 0 represents adiabatic type temperature boundary condition, while BiL, BiU represents isothermal type boundary condition and the intermediate values o BiL, BiU represent Robin type boundary condition. It is evident rom Figure that or intermediate values o BiL, BiU the critical Rayleigh number is sandwiched between those o adiabatic and isothermal cases. Fig.3: Error plots or dierent values o Da, with CF = 0.005, = 1, Re = 10 and initial solutions. Figures 3 show the error plots or various values o Reynolds number or initial velocities we see that the Reynolds number appears in the nonlinear term and hence it would require one or two additional iterations to achieve convergence than it usually require. In the present problem, the non-boundary parameters that aect the critical Rayleigh number are the Darcy number Da, the inter-phase heat transer parameter H and the porosity-scaled conductivity ratio γ. We now discuss eects o these parameters on the onset o convection with upper and lower stress-ree-isothermal (FIFI) boundaries and upper and lower rigid-isothermal (RIRI) boundaries. Table 1 gives the critical Rayleigh number and the critical wave number or dierent values o Da, γ and LogH. It is clear that increasing values o LogH results in increasing the critical Rayleigh number indicating that the inter-phase heat transer parameter has a stabilizing eect on the onset o convection in the case o stress-ree-isothermal (FIFI) and rigid-isothermal (RIRI) boundaries. It is observed that the critical Rayleigh number is a decreasing unction o the parameter γ which mean that
12 1568 Dr. Ashoka S. B. convection sets in much earlier than expected or higher values γ vowing to its destabilizing eect in both FIFI and RIRI cases. Further, the Darcy number also increases the critical Rayleigh number in FIFI and RIRI case. Hence it has a stabilizing eect on the system considered. Results o the other mixed combinations o boundary conditions like rigid-stress-ree, isothermal-adiabatic are obtained as special cases o the general boundary conditions considered in the paper. We omit the discussion o the same or reasons o space. Table 1. Critical Rayleigh number and critical wave number or dierent values o Da, γ and LogH Da γ LogH FIFI RIRI kc Rac kc Rac
13 A New Algorithm Based SLM to Find Critical Eigenvalue CONCLUSIONS In this paper we presented a semi-analytical study o the linear stability analysis or the Rayleigh-Bénard-Brinkman convective instability problem that assumes local thermal non-equilibrium between the luid and solid phases and that considers general boundary conditions on velocity and temperatures. The eigen boundary value problem was solved using the successive linearization method with the help o singleterm Galerkin method or initial solutions. The analysis predicts the critical Rayleigh number corresponding to the third kind temperature boundaries to be between those o adiabatic and isothermal cases. Further, the Darcy number and the inter-phase heat transer parameter have stabilizing eect on the system while the opposite is true in the case o porosity-scaled conductivity ratio. REFERENCES [1] C.W. Horton and F.T. Rogers, Convection currents in a porous medium, Journal o Applied Physics 16, (1945). [] E.R. Lapwood, Convection o a luid in a porous medium, Proceeding o the Cambridge Philosophical Society 44, (1948). [3] D.B. Ingham and I. Pop, Transport phenomena in porous media (Pergamon, Oxord, 1998). [4] D.A. Nield and A. Bejan, Convection in porous media (Springer-Verlag, New York, 1999). [5] K. Vaai, Handbook o porous media (Marcel Dekker, New York, 000). [6] N. Banu and D.A.S. Rees, Onset o Darcy-Bénard convection using a thermal nonequilibrium model, International Journal o Heat and Mass Transer 45, 1-8 (00). [7] A. Postelnicu and D.A.S. Rees, The onset o a Darcy-Brinkman convection using a thermal nonequilibrium model-part I: stress-ree boundaries, International Journal o Energy Research 7, (003). [8] M.S. Malashetty, I.S. Shivakumara and S. Kulkarni, The onset o Lapwood- Brinkman convection using a thermal non-equilibrium model, International Journal o Heat and Mass Transer 48, (005). [9] A. Nouri-Borujerdi, A.R. Noghrehabadi and D.A.S. Rees, The eect o local thermal non-equilibrium on conduction in porous channels with a uniorm heat source, Transport in Porous Media 69, (007). [10] A. Postelnicu, The onset o a Darcy Brinkman convection using a thermal nonequilibrium model. Part II, International Journal o Thermal Sciences 47,
14 1570 Dr. Ashoka S. B (008). [11] M.S. Malashetty, I.S. Shivakumara and S. Kulkarni, The onset o convection in a couple stress luid saturated porous layer using a thermal non-equilibrium model, Physics Letters A 373, (009). [1] I.S. Shivakumara, M.S. Malashetty and K.B. Chavaraddi, Onset o convection in a viscoelastic luid-saturated sparsely packed porous layer using a thermal nonequilibrium model, Candian Journal o Physics 84, (006). [13] M.S. Malashetty, M. Swamy, R. Heera, Double diusive convection in a porous layer using a thermal non-equilibrium model, International Journal o Thermal Sciences 47, (008). [14] M.S. Malashetty and R. Heera, Linear and non-linear double diusive convection in a rotating porous layer using a thermal non-equilibrium model, International Journal o Non-Linear Mechanics 43, (008). [15] M.S. Malashetty, I. Pop and R. Heera, Linear and nonlinear double diusive convection in a rotating sparsely packed porous layer using a thermal nonequilibrium model, Continuum Mechanics and Thermodynics 1, (009). [16] M.S. Malashetty, I.S. Shivakumara and S. Kulkarni, The onset o convection in an anisotropic porous layer using a thermal non-equilibrium model, Transport in Porous Media 60, (005). [17] I.S. Shivakumara, J. Lee, A.L. Mamatha and M. Ravisha, Boundary and thermal non-equilibrium eects on convective instability in an anisotropic porous layer, Journal o Mechanical Science and Technology 5, (011). [18] P.G. Siddheshwar, Convective instability o erromagnetic luids bounded by luid-permeable, magnetic boundaries, Journal o Magnetism and Magnetic Materials 149, (1995). [19] M. Narayana, S.S. Motsa and P. Sibanda, On a piecewise linearization solution o an eigen BVP and chaotic system due to magneto-convection in a two dimensional rectangular box, to be communicated (014).
Analysis of Non-Thermal Equilibrium in Porous Media
Analysis o Non-Thermal Equilibrium in Porous Media A. Nouri-Borujerdi, M. Nazari 1 School o Mechanical Engineering, Shari University o Technology P.O Box 11365-9567, Tehran, Iran E-mail: anouri@shari.edu
More informationControlling the Heat Flux Distribution by Changing the Thickness of Heated Wall
J. Basic. Appl. Sci. Res., 2(7)7270-7275, 2012 2012, TextRoad Publication ISSN 2090-4304 Journal o Basic and Applied Scientiic Research www.textroad.com Controlling the Heat Flux Distribution by Changing
More informationCONVECTIVE HEAT TRANSFER CHARACTERISTICS OF NANOFLUIDS. Convective heat transfer analysis of nanofluid flowing inside a
Chapter 4 CONVECTIVE HEAT TRANSFER CHARACTERISTICS OF NANOFLUIDS Convective heat transer analysis o nanoluid lowing inside a straight tube o circular cross-section under laminar and turbulent conditions
More informationNON-SIMILAR SOLUTIONS FOR NATURAL CONVECTION FROM A MOVING VERTICAL PLATE WITH A CONVECTIVE THERMAL BOUNDARY CONDITION
NON-SIMILAR SOLUTIONS FOR NATURAL CONVECTION FROM A MOVING VERTICAL PLATE WITH A CONVECTIVE THERMAL BOUNDARY CONDITION by Asterios Pantokratoras School o Engineering, Democritus University o Thrace, 67100
More informationNatural convection in a vertical strip immersed in a porous medium
European Journal o Mechanics B/Fluids 22 (2003) 545 553 Natural convection in a vertical strip immersed in a porous medium L. Martínez-Suástegui a,c.treviño b,,f.méndez a a Facultad de Ingeniería, UNAM,
More informationINFLUENCE OF VARIABLE PERMEABILITY ON FREE CONVECTION OVER VERTICAL FLAT PLATE EMBEDDED IN A POROUS MEDIUM
INFLUENCE OF VARIABLE PERMEABILITY ON FREE CONVECTION OVER VERTICAL FLAT PLATE EMBEDDED IN A POROUS MEDIUM S. M. M. EL-Kabeir and A. M. Rashad Department of Mathematics, South Valley University, Faculty
More information2015 American Journal of Engineering Research (AJER)
American Journal o Engineering Research (AJER) 2015 American Journal o Engineering Research (AJER) e-issn: 2320-0847 p-issn : 2320-0936 Volume-4, Issue-7, pp-33-40.ajer.org Research Paper Open Access The
More informationTemperature and Internal Heat Generation in a Porous Medium
TECHNISCHE MECHANIK, Band 21, Heft 4, (20011313318 Manuskripteingang: 20. September 200] Free Convection over 3 Vertical Flat Plate with a Variable Wall Temperature and Internal Heat Generation in a Porous
More informationBuoyancy Driven Heat Transfer of Water-Based CuO Nanofluids in a Tilted Enclosure with a Heat Conducting Solid Cylinder on its Center
July 4-6 2012 London U.K. Buoyancy Driven Heat Transer o Water-Based CuO Nanoluids in a Tilted Enclosure with a Heat Conducting Solid Cylinder on its Center Ahmet Cihan Kamil Kahveci and Çiğdem Susantez
More informationLinear and Weak Nonlinear Double Diffusive Convection in a Viscoelastic Fluid Saturated Anisotropic Porous Medium with Internal Heat Source
Journal of Applied Fluid Mechanics, Vol. 11, No. 1, pp. 65-77, 018. Available online at www.jafmonline.net, ISSN 1735-357, EISSN 1735-3645. DOI: 10.18869/acadpub.jafm.73.44.7519 Linear and Weak Nonlinear
More informationCHAPTER-III CONVECTION IN A POROUS MEDIUM WITH EFFECT OF MAGNETIC FIELD, VARIABLE FLUID PROPERTIES AND VARYING WALL TEMPERATURE
CHAPER-III CONVECION IN A POROUS MEDIUM WIH EFFEC OF MAGNEIC FIELD, VARIABLE FLUID PROPERIES AND VARYING WALL EMPERAURE 3.1. INRODUCION Heat transer studies in porous media ind applications in several
More informationMAGNETOHYDRODYNAMIC GO-WATER NANOFLUID FLOW AND HEAT TRANSFER BETWEEN TWO PARALLEL MOVING DISKS
THERMAL SCIENCE: Year 8, Vol., No. B, pp. 383-39 383 MAGNETOHYDRODYNAMIC GO-WATER NANOFLUID FLOW AND HEAT TRANSFER BETWEEN TWO PARALLEL MOVING DISKS Introduction by Mohammadreza AZIMI and Rouzbeh RIAZI
More informationBoundary-Layer Flow over a Porous Medium of a Nanofluid Past from a Vertical Cone
Boundary-Layer Flow over a Porous Medium o a Nanoluid Past rom a Vertical Cone Mohammad Mehdi Keshtkar 1 and jamaladin hadizadeh 2 1 Assistant Proessor, Department o Mechanical Engineering, 2 MSc. Student,
More informationNUMERICAL ANALYSIS OF FORCED CONVECTION HEAT TRANSFER FROM TWO TANDEM CIRCULAR CYLINDERS EMBEDDED IN A POROUS MEDIUM
THERMAL SCIENCE, Year 2017, Vol. 21, No. 5, pp. 2117-2128 2117 Introduction NUMERICAL ANALYSIS OF FORCED CONVECTION HEAT TRANSFER FROM TWO TANDEM CIRCULAR CYLINDERS EMBEDDED IN A POROUS MEDIUM by Habib-Ollah
More informationOnset of convection of a reacting fluid layer in a porous medium with temperature-dependent heat source
AMERICAN JOURNAL OF SCIENTIFIC AND INDUSTRIAL RESEARCH 2011, Science Huβ, http://www.scihub.org/ajsir ISSN: 2153-649X doi:10.5251/ajsir.2011.2.6.860.864 Onset of convection of a reacting fluid layer in
More informationEffect of Gravity Modulation and Internal Heat Generation on Rayleigh-Bénard Convection in Couple Stress Fluid with Maxwell-Cattaneo Law
Effect of Gravity Modulation and Internal Heat Generation on Rayleigh-Bénard Convection in Couple Stress Fluid with Maxwell-Cattaneo Law Maria Thomas Research scholar, Department of Mathematics, CHRIST
More informationCOMPARISON OF THERMAL CHARACTERISTICS BETWEEN THE PLATE-FIN AND PIN-FIN HEAT SINKS IN NATURAL CONVECTION
HEFAT014 10 th International Conerence on Heat Transer, Fluid Mechanics and Thermodynamics 14 6 July 014 Orlando, Florida COMPARISON OF THERMA CHARACTERISTICS BETWEEN THE PATE-FIN AND PIN-FIN HEAT SINKS
More informationFree convection in a porous cavity filled with nanofluids
Free convection in a porous cavity illed with nanoluids GROSAN TEODOR, REVNIC CORNELIA, POP IOAN Faculty o Mathematics and Computer Sciences Babes-Bolyai University Cluj-Napoca ROMANIA tgrosan@math.ubbcluj.ro,
More informationEffects of Viscous Dissipation on Unsteady Free Convection in a Fluid past a Vertical Plate Immersed in a Porous Medium
Transport in Porous Media (2006) 64: 1 14 Springer 2006 DOI 10.1007/s11242-005-1126-6 Effects of Viscous Dissipation on Unsteady Free Convection in a Fluid past a Vertical Plate Immersed in a Porous Medium
More informationScienceDirect. Heat transfer and fluid transport of supercritical CO 2 in enhanced geothermal system with local thermal non-equilibrium model
Available online at www.sciencedirect.com ScienceDirect Energy Procedia 63 (2014 ) 7644 7650 GHGT-12 Heat transer and luid transport o supercritical CO 2 in enhanced geothermal system with local thermal
More informationPERFORMANCE OF NANOFLUID IN FREE CONVECTIVE HEAT TRANSFER INSIDE A CAVITY WITH NON-ISOTHERMAL BOUNDARY CONDITIONS
Proceedings o the International Conerence on Mechanical Engineering and Renewable Energy 2015 (ICMERE2015) 26 29 November, 2015, Chittagong, Bangladesh ICMERE2015-PI-058 PERFORMANCE OF NANOFUID IN FREE
More informationVisualization of Natural Convection in Enclosure. Filled with Porous Medium by Sinusoidally. Temperature on the One Side
Applied Mathematical Sciences, Vol., 2012, no. 97, 801-812 Visualization of Natural Convection in Enclosure Filled with Porous Medium by Sinusoidally Temperature on the One Side Paweena Khansila Department
More informationBOUNDARY LAYER ANALYSIS ALONG A STRETCHING WEDGE SURFACE WITH MAGNETIC FIELD IN A NANOFLUID
Proceedings o the International Conerence on Mechanical Engineering and Reneable Energy 7 (ICMERE7) 8 December, 7, Chittagong, Bangladesh ICMERE7-PI- BOUNDARY LAYER ANALYSIS ALONG A STRETCHING WEDGE SURFACE
More informationCombined Effect of Magnetic field and Internal Heat Generation on the Onset of Marangoni Convection
International Journal of Fluid Mechanics & Thermal Sciences 17; 3(4): 41-45 http://www.sciencepublishinggroup.com/j/ijfmts doi: 1.11648/j.ijfmts.1734.1 ISSN: 469-815 (Print); ISSN: 469-8113 (Online) ombined
More informationEffect of Variable Viscosity on Convective Heat and Mass Transfer by Natural Convection from Vertical Surface in Porous Medium
Effect of Variable Viscosity on Convective Heat and Mass Transfer by Natural Convection from Vertical Surface in Porous Medium M.B.K.MOORTHY, K.SENTHILVADIVU Department of Mathematics, Institute of Road
More informationENTROPY GENERATION IN HEAT AND MASS TRANSFER IN POROUS CAVITY SUBJECTED TO A MAGNETIC FIELD
HEFAT 9 th International Conference on Heat Transfer, Fluid Mechanics and Thermodynamics 6 8 July Malta ENTROPY GENERATION IN HEAT AND MASS TRANSFER IN POROUS CAVITY SUBJECTED TO A MAGNETIC FIELD Nawaf
More informationRadiation Effects on MHD Free Convective Heat and Mass Transfer Flow Past a Vertical Porous Flat Plate with Suction
International Journal o Science, Engineering and Technology Research (IJSETR), Volume 3, Issue 5, May 4 Radiation Eects on MHD Free Convective Heat and Mass Transer Flow Past a Vertical Porous Flat Plate
More informationAdv. Theor. Appl. Mech., Vol. 7, 2014, no. 1, 1-20 HIKARI Ltd,
Adv. Theor. Appl. Mech., Vol. 7, 2014, no. 1, 1-20 HIKARI Ltd, www.m-hikari.com http://dx.doi.org/10.12988/atam.2014.31124 Magneto-Hydrodynamic Eect with Temperature Dependent Viscosity on Natural Convection
More informationANALYTICAL STUDY OF DDC IN A BINARY FLUID SATURATED ANISOTROPIC POROUS LAYER
Bulletin of the Marathwada Mathematical Society Vol. 13, No. 2, December 2012, Pages 37 47. ANALYTICAL STUDY OF DDC IN A BINARY FLUID SATURATED ANISOTROPIC POROUS LAYER S. N. Gaikwad 1 and S. S. Kamble
More informationEffect of Variable Viscosity on Convective Heat and Mass Transfer by Natural Convection from Horizontal Surface in Porous Medium
Effect of Variable Viscosity on Convective Heat and Mass Transfer by Natural Convection from Horizontal Surface in Porous Medium M. B. K. MOORTHY, K. SENTHILVADIVU Department of Mathematics, Institute
More informationCOMPUTATIONAL STUDY OF CHEMICALLY REACTING HYPERSONIC FLOW
COMPUTATIONAL STUDY OF CHEMICALLY REACTING HYPERSONIC FLOW Yoshiuru Funahashi Department o Aeronautics and Astronautics, Graduate School o Engineering, The University o Tokyo, Tokyo, JAPAN Keywords: Hypersonic
More informationNatural Convection in Vertical Channels with Porous Media and Adiabatic Extensions
Natural Convection in Vertical Channels with Porous Media and Adiabatic Extensions Assunta Andreozzi 1,a, Bernardo Buonomo 2,b, Oronzio Manca 2,c and Sergio Nardini 2,d 1 DETEC, Università degli Studi
More informationForced Convection in a Cylinder Filled with Porous Medium, including Viscous Dissipation Effects
Journal of Applied Fluid Mechanics, Vol. 9, Special Issue 1, pp. 139-145, 016. Selected papers from the 7 th International Exergy, Energy and Environment Symposium, IEEE7-015 Available online at www.jafmonline.net,
More informationConvective effects in air layers bound by cellular honeycomb arrays *
Journal o Scientiic & Industrial Research Vol. 64, August 5, pp. 6-61 Convective eects in air layers bound by cellular honeycomb arrays * Pawan Kumar 1 and N D Kaushika, * 1 Centre or Energy Studies, Indian
More informationAnalysis of Least Stable Mode of Buoyancy Assisted Mixed Convective Flow in Vertical Pipe Filled with Porous Medium
Proceedings of the World Congress on Engineering 2 Vol I WCE 2, July 6-8, 2, London, U.K. Analysis of Least Stable Mode of Buoyancy Assisted Mixed Convective Flow in Vertical Pipe Filled with Porous Medium
More informationKabita Nath Department of Mathematics Dibrugarh University Dibrugarh, Assam, India
Influence of Chemical Reaction, Heat Source, Soret and Dufour Effects on Separation of a Binary Fluid Mixture in MHD Natural Convection Flow in Porous Media B.R.Sharma Department of Mathematics Dibrugarh
More informationAn Improved Expression for a Classical Type of Explicit Approximation of the Colebrook White Equation with Only One Internal Iteration
International Journal o Hydraulic Engineering 06, 5(): 9-3 DOI: 0.593/j.ijhe.06050.03 An Improved Expression or a Classical Type o Explicit Approximation o the Colebrook White Equation with Only One Internal
More informationDouble diffusive reaction-convection in viscous fluid layer
Available online at http://ijim.srbiau.ac.ir/ Int. J. Industrial Mathematics (ISSN 2008-5621) Vol. 6, No. 4, 2014 Article ID IJIM-00488, 12 pages Research Article Double diffusive reaction-convection in
More informationA Semi-Analytical Solution for a Porous Channel Flow of a Non-Newtonian Fluid
Journal o Applied Fluid Mechanics, Vol. 9, No. 6, pp. 77-76, 6. Available online at www.jamonline.net, ISSN 735-357, EISSN 735-3645. A Semi-Analytical Solution or a Porous Channel Flow o a Non-Newtonian
More informationTHE study of convective flow in modulated fluid layers or
Nonlinear Stability of Convection in a Thermally Modulated Anisotropic Porous Medium M. Meenasaranya, S. Saravanan Abstract Conditions corresponding to the unconditional stability of convection in a mechanically
More informationA REPORT ON PERFORMANCE OF ANNULAR FINS HAVING VARYING THICKNESS
VOL., NO. 8, APRIL 6 ISSN 89-668 ARPN Journal o Engineering and Applied Sciences 6-6 Asian Research Publishing Networ (ARPN). All rights reserved. A REPORT ON PERFORMANCE OF ANNULAR FINS HAVING VARYING
More informationINFLUENCE OF POROSITY AND RADIATION IN A VISCO ELASTIC FLUID OF SECOND ORDER FLUID WITHIN A CHANNEL WITH PERMEABLE WALLS
International Journal o Physics and Mathematical Sciences ISSN: 77- (Online) Vol. () January-March, pp.8-9/murthy and Rajani INFLUENCE OF POROSITY AND RADIATION IN A VISCO ELASTIC FLUID OF SECOND ORDER
More information3D Numerical Modelling of Convective Heat Transfer through Two-sided Vertical Channel Symmetrically Filled with Metal Foams
P Periodica Polytechnica Mechanical Engineering P 60(4), pp. 193-202, 2016 DOI: 10.3311/PPme.8511 Creative Commons Attribution b 3D Numerical Modelling o Convective Heat Transer through Two-sided Vertical
More informationNon-Isothermal Displacements with Step-Profile Time Dependent Injections in Homogeneous Porous Media
Proceedings o the World Congress on Mechanical, Chemical, and Material Engineering (MCM 015) Barcelona, Spain July 0-1, 015 Paper No. 93 Non-Isothermal Displacements with Step-Proile Time Dependent Injections
More informationEntropy 2011, 13, ; doi: /e OPEN ACCESS
Entropy 011, 13, 1446-1464; doi:10.3390/e13081446 OPEN ACCESS entropy ISSN 1099-4300 www.mdpi.com/journal/entropy Article Second Law Analysis or Variable Viscosity Hydromagnetic Boundary Layer Flow with
More informationKuldeep Rawat*, Ayushman Srivastav* *Assistant Professor, Shivalik College of Engineering, Dehradun.
International Journal o Scientiic & Engineering search, Volume 7, Issue 12, December-16 348 ISSN 2229-18 NUMERICAL INVESTIGATION OF HEAT TRANSFER ENHANCEMENT OVER RECTANGULAR PERFORATED FIN Abstract Kuldeep
More informationFully developed mixed convection through a vertical porous channel with an anisotropic permeability: case of heat flux
Stud. Univ. Babeş-Bolyai Math. 60(2015), No. 2, 341 350 Fully developed mixed convection through a vertical porous channel with an anisotropic permeability: case of heat flux Diana Andrada Filip, Radu
More informationNumerical Study of Steady MHD Plane Poiseuille Flow and Heat Transfer in an Inclined Channel
Numerical Study of Steady MHD Plane Poiseuille Flow and Heat Transfer in an Inclined Channel Muhim Chutia Department of Mathematics, Mariani College, Assam-785634, India ABSTRACT: In this paper, a numerical
More informationMechanical Engineering Research Journal BUOYANT FLOW OF NANOFLUID FOR HEAT-MASS TRANSFER THROUGH A THIN LAYER
Dept. o Mech. Eng. CUET Published Online March 2015 (http://www.cuet.ac.bd/merj/index.html) Mechanical Engineering Research Journal Vol. 9, pp. 712, 2013 M E R J ISSN: 1990-5491 BUOYANT FLOW OF NANOFLUID
More informationRotating Flow of Magnetite-Water Nanofluid over a Stretching Surface Inspired By Non-Linear Thermal Radiation and Mass Transfer
International Journal o Mathematics Research. ISSN 0976-5840 Volume 9, Number (017), pp. 89-97 International Research Publication House http://www.irphouse.com Rotating Flow o Magnetite-Water Nanoluid
More information39.1 Gradually Varied Unsteady Flow
39.1 Gradually Varied Unsteady Flow Gradually varied unsteady low occurs when the low variables such as the low depth and velocity do not change rapidly in time and space. Such lows are very common in
More informationSIMILARITY SOLUTION FOR DOUBLE NATURAL CONVECTION WITH DISPERSION FROM SOURCES IN AN INFINITE POROUS MEDIUM
Proceedings NZ GeothermalWorkshop SIMILARITY SOLUTION FOR DOUBLE NATURAL CONVECTION WITH DISPERSION FROM SOURCES IN AN INFINITE POROUS MEDIUM A.V. and A. F. Geothermal Institute, The University of Auckland,
More informationIOSR Journal of Mathematics (IOSR-JM) e-issn: , p-issn: X.Volume12,Issue 1 Ver. III (Jan.-Feb.2016)PP
IOSR Journal o Mathematics (IOSR-JM) e-issn:78-578, p-issn: 39-765X.Volume,Issue Ver. III (Jan.-Feb.6)PP 88- www.iosrjournals.org Eect o Chemical Reaction on MHD Boundary Layer Flow o Williamson Nanoluid
More informationIterative Methods for Stokes/Darcy Coupling
Iterative Methods or Stokes/Darcy Coupling Marco Discacciati Ecole Polytechnique Fédérale de Lausanne Institut d Analyse et Calcul Scientiique Chair o Modelling and Scientiic Computing marco.discacciati@epl.ch
More informationA solid-fluid mixture theory of porous media
A solid-luid mixture theory o porous media I-Shih Liu Instituto de Matemática, Universidade Federal do Rio de Janeiro Abstract The theories o mixtures in the ramework o continuum mechanics have been developed
More informationComments on Magnetohydrodynamic Unsteady Flow of A Non- Newtonian Fluid Through A Porous Medium
Comments on Magnetohydrodynamic Unsteady Flow o A Non- Newtonian Fluid Through A Porous Medium Mostaa A.A.Mahmoud Department o Mathematics, Faculty o Science, Benha University (358), Egypt Abstract The
More informationNumerical Study of Natural Convection in. an Inclined L-shaped Porous Enclosure
Adv. Theor. Appl. Mech., Vol. 5, 2012, no. 5, 237-245 Numerical Study of Natural Convection in an Inclined L-shaped Porous Enclosure S. M. Moghimi 1 *, G. Domairry 2, H. Bararnia 2, Soheil Soleimani 2
More informationEffect of Buoyancy Force on the Flow Field in a Square Cavity with Heated from Below
International Journal of Discrete Mathematics 017; (): 43-47 http://www.sciencepublishinggroup.com/j/dmath doi: 10.11648/j.dmath.01700.13 Effect of Buoyancy Force on the Flow Field in a Square Cavity with
More informationInfluence of chemical reaction, Soret and Dufour effects on heat and mass transfer of a binary fluid mixture in porous medium over a rotating disk
IOSR Journal of Mathematics (IOSR-JM) e-issn: 2278-5728, p-issn: 2319-765X. Volume 10, Issue 6 Ver. III (Nov - Dec. 2014), PP 73-78 Influence of chemical reaction, Soret and Dufour effects on heat and
More informationLecture 25: Heat and The 1st Law of Thermodynamics Prof. WAN, Xin
General Physics I Lecture 5: Heat and he 1st Law o hermodynamics Pro. WAN, Xin xinwan@zju.edu.cn http://zimp.zju.edu.cn/~xinwan/ Latent Heat in Phase Changes Latent Heat he latent heat o vaporization or
More informationSIMULATION OF A FLOW THROUGH A RIGID POROUS MEDIUM SUBJECTED TO A CONSTRAINT
SIMULATION O A LOW THROUGH A RIGID POROUS MEDIUM SUBJECTED TO A CONSTRAINT R. M. Saldanha da Gama a, J. J. Pedrosa ilho a, and M. L. Martins-Costa b a Universidade do Estado do Rio de Janeiro Departamento
More informationOPTIMALLY STAGGERED FINNED CIRCULAR AND ELLIPTIC TUBES IN FORCED CONVECTION
OPTIMALLY STAGGERED FINNED CIRCULAR AND ELLIPTIC TUBES IN FORCED CONVECTION R. S. Matos a, T. A. Laursen b, J. V. C. Vargas a, and A. Bejan c, a Universidade Federal do Paraná Departamento de Engenharia
More informationAvailable online at ScienceDirect. Procedia Engineering 105 (2015 )
Available online at www.sciencedirect.com ScienceDirect Procedia Engineering 105 (2015 ) 388 397 6th BSME International Conerence on Thermal Engineering (ICTE 2014) Eect o tilt angle on pure mixed convection
More informationNon-newtonian Rabinowitsch Fluid Effects on the Lubrication Performances of Sine Film Thrust Bearings
International Journal o Mechanical Engineering and Applications 7; 5(): 6-67 http://www.sciencepublishinggroup.com/j/ijmea doi:.648/j.ijmea.75.4 ISSN: -X (Print); ISSN: -48 (Online) Non-newtonian Rabinowitsch
More informationBIOCONVECTION HEAT TRANSFER OF A NANOFLUID OVER A STRETCHING SHEET WITH VELOCITY SLIP AND TEMPERATURE JUMP
THERMAL SCIENCE: Year 017, Vol. 1, No. 6A, pp. 47-56 47 BIOCONVECTION HEAT TRANSFER OF A NANOFLUID OVER A STRETCHING SHEET WITH VELOCITY SLIP AND TEMPERATURE JUMP by Bingyu SHEN a, Liancun ZHENG a*, Chaoli
More information6.6 Rayleigh-Darcy (or Horton-Rogers-Lapwood) instability
1 Lecture Notes on Fluid Dynamics (1.63J/.1J) by Chiang C. Mei, 6.6 Rayleigh-Darcy (or Horton-Rogers-Lapwood) instability in a porous layer 6-6-Lapwood.tex May 11, 3 Nield & Bejan, Chapter 6 Convection
More information8. INTRODUCTION TO STATISTICAL THERMODYNAMICS
n * D n d Fluid z z z FIGURE 8-1. A SYSTEM IS IN EQUILIBRIUM EVEN IF THERE ARE VARIATIONS IN THE NUMBER OF MOLECULES IN A SMALL VOLUME, SO LONG AS THE PROPERTIES ARE UNIFORM ON A MACROSCOPIC SCALE 8. INTRODUCTION
More informationKeywords: Finite element method; Nanofluid; Inclined magnetic field; Natural convection; Square enclosure; Brownian motion
Columbia International Publishing American Journal o Heat and Mass Transer doi:10.7726/ajhmt.2016.1012 Research Article Finite Element Analysis o Unsteady Natural Convective Heat Transer and Fluid Flow
More informationNUMERICAL STUDY ON THE EFFECT OF INCLINATION ANGLE ON HEAT TRANSFER PERFORMANCE IN BACK-WARD FACING STEP UTILIZING NANOFLUID
NUMERICAL STUDY ON THE EFFECT OF INCLINATION ANGLE ON HEAT TRANSFER PERFORMANCE IN BACK-WARD FACING STEP UTILIZING NANOFLUID Saleh Etaig*, Etaig.Mahmoud@Northumbria.ac.uk Reaz Hasan, Reaz.Hasan@Northumria.ac.uk
More informationOn steady hydromagnetic flow of a radiating viscous fluid through a horizontal channel in a porous medium
AMERICAN JOURNAL OF SCIENTIFIC AND INDUSTRIAL RESEARCH 1, Science Huβ, http://www.scihub.org/ajsir ISSN: 153-649X doi:1.551/ajsir.1.1..33.38 On steady hydromagnetic flow of a radiating viscous fluid through
More informationPrediction of Well Bore Temperatures during Ultra-Deep Drilling
Prediction o Well Bore Temperatures during Ultra-Deep Drilling Fanhe Meng, Aiguo Yao*, Shuwei Dong Faculty o Engineering China University o Geosciences Wuhan, Hubei, 430074, China Abstract In order to
More informationHeat and Fluid Flow of Gases in Porous Media with Micropores: Slip Flow Regime
16 Heat and Fluid Flow o Gases in Porous Media with Micropores: Slip Flow Regime Moghtada Mobedi, Murat Barisik, and A. Nakayama CONTENTS 16.1 Introduction...407 16. VAM Motion and Heat Transer Equations...409
More informationThe Study of Natural Convection Heat Transfer in a Partially Porous Cavity Based on LBM
Send Orders for Reprints to reprints@benthamscience.ae 88 The Open Fuels & Energy Science Journal, 014, 7, 88-93 Open Access The Study of Natural Convection Heat Transfer in a Partially Porous Cavity Based
More informationNatural Convection and Entropy Generation in Partially Heated Porous Wavy Cavity Saturated by a Nanofluid
Proceedings o the 5 th International Conerence o Fluid Flow, Heat and Mass Transer (FFHMT'18) Niagara Falls, Canada June 7 9, 2018 Paer No. 123 DOI: 10.11159/hmt18.123 Natural Convection and Entroy Generation
More informationRayleigh-Bénard Convection in A Horizontal Layer Of Porous Medium Saturated With A Thermally Radiating Dielectric Fluid
IOSR Journal of Mathematics (IOSR-JM) e-issn: 78-578, p-issn: 319-765X. Volume 11, Issue 3 Ver. III (May - Jun. 015), PP 01-10 www.iosrjournals.org Rayleigh-Bénard Convection in A Horizontal Layer Of Porous
More informationAvailable online at ScienceDirect. Procedia Materials Science 10 (2015 )
Available online at www.sciencedirect.com ScienceDirect Procedia Materials Science 10 (2015 ) 563 571 2nd International Conference on Nanomaterials and Technologies (CNT 2014) Effect of viscous dissipation,
More informationThroughflow and Gravity Modulation Effects on Heat Transport in a Porous Medium
Journal of Applied Fluid Mechanics Vol. 9 No. 3 pp. 115-1113 16. Available online at www.jafmonline.net ISSN 1735-357 EISSN 1735-3645. DOI: 1.18869/acadpub.jafm.68.8.468 Throughflow and Gravity Modulation
More informationFINITE ELEMENT ANALYSIS OF MIXED CONVECTION HEAT TRANSFER ENHANCEMENT OF A HEATED SQUARE HOLLOW CYLINDER IN A LID-DRIVEN RECTANGULAR ENCLOSURE
Proceedings of the International Conference on Mechanical Engineering 2011 (ICME2011) 18-20 December 2011, Dhaka, Bangladesh ICME11-TH-014 FINITE ELEMENT ANALYSIS OF MIXED CONVECTION HEAT TRANSFER ENHANCEMENT
More informationEFFECTS OF VISCOUS DISSIPATION ON FREE CONVECTION BOUNDARY LAYER FLOW TOWARDS A HORIZONTAL CIRCULAR CYLINDER
EFFECTS OF VISCOUS DISSIPATION ON FREE CONVECTION BOUNDARY LAYER FLOW TOWARDS A HORIZONTAL CIRCULAR CYLINDER Muhammad Khairul Anuar Mohamed 1, Norhaizah Md Sari 1, Abdul Rahman Mohd Kasim 1, Nor Aida Zuraimi
More informationViscosity and Fluid Suction/Injection Effects on Free Convection Flow from a Vertical Plate in a Porous Medium Saturated with a Pseudoplastic Fluid
ISSN 749-3889 (print), 749-3897 (online) International Journal of Nonlinear Science Vol.8(4) No.,pp.7-38 Viscosity and Fluid Suction/Injection Effects on Free Convection Flow from a Vertical Plate in a
More informationNATURAL CONVECTION IN INCLINED RECTANGULAR POROUS CAVITY SUBJECT TO HEAT FLUXES ON THE LONG SIDE WALLS
Proceedings of 4 th ICCHMT May 7 0, 005, Paris-Cachan, FRANCE ICCHMT 05-53 NATURAL CONVECTION IN INCLINED RECTANGULAR POROUS CAVITY SUBJECT TO HEAT FLUXES ON THE LONG SIDE WALLS L. Storesletten*, D.A.S.
More informationInfluence of the Order of Chemical Reaction and Soret Effect on Mass Transfer of a Binary Fluid Mixture in Porous Media
Influence of the Order of Chemical Reaction and Soret Effect on Mass Transfer of a Binary Fluid Mixture in Porous Media B.R.Sharma, Debozani Borgohain Department of Mathematics, Dibrugarh University, Dibrugarh-786004,
More informationSecond Order Slip Flow of Cu-Water Nanofluid Over a Stretching Sheet With Heat Transfer
Second Order Slip Flow o Cu-Water Nanoluid Over a Stretching Sheet With Heat Transer RAJESH SHARMA AND ANUAR ISHAK School o Mathematical Sciences, Faculty o Science and Technology Universiti Kebangsaan
More informationDescription of a One-Dimensional Numerical Model of an Active Magnetic Regenerator Refrigerator
This is a 1D model o an active magnetic regenerative rerigerator (AMRR) that was developed in MATLAB. The model uses cycle inputs such as the luid mass low and magnetic ield proiles, luid and regenerator
More informationInternational Journal of Innovative Research in Science, Engineering and Technology. (An ISO 3297: 2007 Certified Organization)
ISSN(Online): 239-8753 Influence of Chemical Reaction, Heat Source, Soret and Dufour Effects on Heat And Mass Transfer in Boundary Layer Flow Over a Stretching Cylinder Embedded in a Porous Medium using
More information6.6 Horton-Rogers-Lapwood instability in a porous layer
1 November, Notes on 1.63 Advanced Environmental Fluid Mechanics Instructor: C. C. Mei, ccmei@mit.edu, 1 617 53 994 6.6 Horton-Rogers-Lapwood instability in a porous layer Nield & Bejan, Chapter 6 Convection
More informationEFFECTS OF CHEMICAL REACTION ON MHD BOUNDARY LAYER FLOW OVER AN EXPONENTIALLY STRETCHING SHEET WITH JOULE HEATING AND THERMAL RADIATION
International Research Journal o Engineering and Technology (IRJET) e-issn: 395-56 Volume: Issue: 9 Dec-5.irjet.net p-issn: 395-7 EFFECTS OF CHEMICAL REACTION ON MHD BOUNDARY LAYER FLOW OVER AN EXPONENTIALLY
More informationMIXED CONVECTION FLOW OF JEFFREY FLUID ALONG AN INCLINED STRETCHING CYLINDER WITH DOUBLE STRATIFICATION EFFECT
MIXED CONVECION FLOW OF JEFFREY FLUID ALONG AN INCLINED SRECHING CYLINDER WIH DOUBLE SRAIFICAION EFFEC by asawar HAYA a,b,sajid QAYYUM a, Muhammad FAROOQ a Ahmad ALSAEDI b and Muhammad AYUB a a Department
More informationMHD Free convection flow of couple stress fluid in a vertical porous layer
Available online at www.pelagiaresearchlibrary.com Advances in Applied Science Research,, (6:5- ISSN: 976-86 CODEN (USA: AASRFC MHD Free convection flow of couple stress fluid in a vertical porous layer
More informationHYDROMAGNETIC DIVERGENT CHANNEL FLOW OF A VISCO- ELASTIC ELECTRICALLY CONDUCTING FLUID
Rita Choudhury et al. / International Journal o Engineering Science and Technology (IJEST) HYDROAGNETIC DIVERGENT CHANNEL FLOW OF A VISCO- ELASTIC ELECTRICALLY CONDUCTING FLUID RITA CHOUDHURY Department
More informationThe Effects of Viscous Dissipation on Convection in a Porus Medium
Mathematica Aeterna, Vol. 7, 2017, no. 2, 131-145 The Effects of Viscous Dissipation on Convection in a Porus Medium T Raja Rani Military Technological College, Ministry of Defence, Sultanate of Oman.
More informationFORCED CONVECTION IN A SELF HEATING POROUS CHANNEL: LOCAL THERMAL NONEQUILIBIUM MODEL
FORCED CONVECTION IN A SELF HEATING POROUS CHANNEL: LOCAL THERMAL NONEQUILIBIUM MODEL by Azzedine ABDEDOU 1,2*, Khedidja BOUHADEF 2 and Rachid BENNACER 3 1 Département du Génie Mécanique, Faculté de Génie
More informationNUMERICAL STUDY OF MIXED CONVECTION HEAT TRANSFER IN LID-DRIVEN CAVITY UTILIZING NANOFLUID: EFFECT OF TYPE AND MODEL OF NANOFLUID
NUMERICAL STUDY OF MIXED CONVECTION HEAT TRANSFER IN LID-DRIVEN CAVITY UTILIZING NANOFLUID: EFFECT OF TYPE AND MODEL OF NANOFLUID by Nader POURMAHMOUD 1,a, Ashkan GHAFOURI 1,b,*, Iraj MIRZAEE 1,c 1 Department
More informationCOMBINED EFFECTS OF RADIATION AND HEAT GENERATION ON MHD NATURAL CONVECTION FLOW ALONG A VERTICAL FLAT PLATE IN PRESENCE OF HEAT CONDUCTION
BRAC University Journal, vol.vi, no., 9, pp 11- COMBINED EFFECTS OF RADIATION AND HEAT GENERATION ON MHD NATURAL CONVECTION FLOW ALONG A VERTICAL FLAT PLATE IN PRESENCE OF HEAT CONDUCTION Mohammad Mokaddes
More informationAmerican Journal of Modern Energy
American Journal o Modern Energy 2015; 1(1): 1-16 Published online June 15, 2015 (http://www.sciencepublishinggroup.com/j/ajme) doi: 10.11648/j.ajme.20150101.11 Heat Generation/Absorption Eect on Natural
More informationUnsteady Magnetohydrodynamic Free Convective Flow Past a Vertical Porous Plate
International Journal of Applied Science and Engineering 2013. 11, 3: 267-275 Unsteady Magnetohydrodynamic Free Convective Flow Past a Vertical Porous Plate Murali Gundagania,*, Sivaiah Sheria, Ajit Paulb,
More informationFree convection modeling over a vertical flat plate embedded in saturated porous medium with a variable heat source and radiation flux
ISSN 1 746-7233, England, UK World Journal of Modelling and Simulation Vol. 9 (2013) No. 3, pp. 163-172 Free convection modeling over a vertical flat plate embedded in saturated porous medium with a variable
More informationReceived: 28 August 2017; Accepted: 29 September 2017; Published: 8 October 2017
fluids Article Convective Flow in an Aquifer Layer Dambaru Bhatta * and Daniel Riahi School of Mathematical and Statistical Sciences, University of Texas Rio Grande Valley, Edinburg, TX 78539-999, USA;
More informationFALLING FILM FLOW ALONG VERTICAL PLATE WITH TEMPERATURE DEPENDENT PROPERTIES
Proceedings of the International Conference on Mechanical Engineering 2 (ICME2) 8-2 December 2, Dhaka, Bangladesh ICME-TH-6 FALLING FILM FLOW ALONG VERTICAL PLATE WITH TEMPERATURE DEPENDENT PROPERTIES
More informationNumerical Analysis of Laminar flow of Viscous Fluid Between Two Porous Bounding walls
Numerical Analysis of Laminar flow of Viscous Fluid Between Two Porous Bounding walls Ramesh Yadav Department of Mathematics Babu Banarasi Das National Institute of Technology & Management Lucknow Uttar
More information