MYcsvtu Notes HEAT TRANSFER BY CONVECTION

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www.mycsvtunotes.in HEAT TRANSFER BY CONVECTION

CONDUCTION Mechanism of heat transfer through a solid or fluid in the absence any fluid motion. CONVECTION Mechanism of heat transfer through a fluid in the presence of bulk fluid motion Natural (free) Convection Forced Convection (depending on how the fluid motion is initiated) www.mycsvtunotes.in

CLASSIFICATION OF FLUID FLOWS Viscous-inviscid Internal flow- External flow Open-closed channel Compressible- Incompressible Laminar- Turbulent Natural- Forced Steady- Unsteady One-,two-,threedimensional www.mycsvtunotes.in

www.mycsvtunotes.in VISCOSITY When two fluid layers move relative to each other, a friction force develops between them and the slower layer tries to slow down the faster layer. internal resistance to flow cohesive forces between the molecules in liquid molecular collisions in gases. Viscous flows: viscous effects are significant Inviscid flow regions: viscous forces are negligibly small compared to inertial or pressure forces. measure of stickness or resistance to deformation 1. Kinematic viscosity 2. Dynamic viscosity

VISCOSITY DEPENDS ON TEMPERATURE PRESSURE For liquids dependence of pressure is negligible For gases kinematic viscosity depends on pressure since its relation to density Dynamic viscosity (kg/m.s or poise) Kinematic viscosity, m 2 /s or stroke www.mycsvtunotes.in

www.mycsvtunotes.in Convection heat transfer - Dynamic viscosity - Thermal conductivity - Density - Specific heat - Fluid velocity - Geometry - Roughness - Type of fluid flow

www.mycsvtunotes.in NEWTON S LAW OF COOLING Q h conv ha S ( T T ) S (W) Convection heat transfer coefficient (W/m 2. 0 C) The rate of heat transfer between a solid surface and a fluid per unit surface area per unit temperature difference

www.mycsvtunotes.in GENERAL THERMAL ANALYSIS Q conv ha S ( T T ) S Q mc p( Te Ti )

www.mycsvtunotes.in FORCED CONVECTION

LAMINAR FLOW Smooth streamlines Highly- ordered motion (highly viscous fluids in small pipes) TURBULENT FLOW Velocity fluctuations Highly-disordered motion TRANSITIONAL FLOW www.mycsvtunotes.in

REYNOLDS NUMBER Flow Regime: Geometry Surface roughness Flow velocity Surface temperature type of fluid v Ratio of the inertial forces to viscous forces in the fluid m D Re / www.mycsvtunotes.in md md v Mean flow velocity Characteristic length of the geometry Kinematic viscosity

Definition of Reynolds number Critical Reynolds number (Re cr ) for flow in a round pipe Re < 2300 laminar 2300 Re 4000 transitional Re > 4000 turbulent Note that these values are approximate. For a given application, Re cr depends upon Pipe roughness Vibrations Upstream fluctuations, disturbances (valves, elbows, etc. that may disturb the flow) www.mycsvtunotes.in

HYDRAULIC DIAMETER For non-round pipes, the hydraulic diameter D h = 4A c /P A c = cross-section area P = wetted perimeter www.mycsvtunotes.in

www.mycsvtunotes.in Velocity No-slip condition

www.mycsvtunotes.in THERMAL BOUNDARY LAYER Flow region over the surface in which the temperature variation in the direction normal to the surface Velocity profile influences temperature profile

VELOCITY A flow field is best characterized by the velocity distribution, and velocity may vary in three dimension ( x, y, z) in rectangular ( r,, z) in cylinderical coordinates One dimensional flow in a circular pipe In which direction does the velocity change in this figure??? www.mycsvtunotes.in

www.mycsvtunotes.in NUSSELT NUMBER (Dimensionless number) Nu q cond hl k c T k L q conv ht q q conv cond ht kt / L hl k Nu

www.mycsvtunotes.in PRANDTL NUMBER Boundary layer theory Pr C p k Pr molecular diffusivity of molecular diffusivity of momentum heat C k p Pr<<1 heat diffuses very quickly in liquid metals, tbl thicker Pr>>1 heat diffuses very slowly in oils relative to momentum, tbl thinner than vbl

PARALLEL FLOW OVER FLAT PLATES www.mycsvtunotes.in 5 10 5 Re cr cr x 5 3 1/ 0.5 10 5 Re Pr Re.664 0 L L k hl Nu 7 5 3 1/ 0.8 10 Re 10 5 60 Pr 0.6 Pr Re 0.037 L L k hl Nu laminar turbulent

www.mycsvtunotes.in NATURAL CONVECTION

www.mycsvtunotes.in CONVECTIVE HEAT TRANSFER COEFFICIENT Coefficient of volume expansion Grashof number Gr L g ( T s T 2 ) L 3 C Rayleigh number Prandtl number Ra L Gr L Pr viscosity Nusselt number Nu hl k C CRa n L Table 20-1

www.mycsvtunotes.in Free Convection A free convection flow field is a self-sustained flow driven by the presence of a temperature gradient. (As opposed to a forced convection flow where external means are used to provide the flow.) As a result of the temperature difference, the density field is not uniform also. Buoyancy will induce a flow current due to the gravitational field and the variation in the density field. In general, a free convection heat transfer is usually much smaller compared to a forced convection heat transfer. It is therefore important only when there is no external flow exists. cold T r T r hot Flow is unstable and a circulatory pattern will be induced.

www.mycsvtunotes.in Basic Definitions Buoyancy effect: Surrounding fluid, cold, r Hot plate Warm, r Net force=(r - r)gv The density difference is due to the temperature difference and it can be characterized by ther volumetric thermal expansion coefficient, b: 1 r 1 r r 1 r b ( ) P r T r T T r T r bt

www.mycsvtunotes.in Grashof Number and Rayleigh Number Define Grashof number, Gr, as the ratio between the buoyancy force and the viscous force: 3 Gr gbtl gb ( T T ) L 3 S 2 2 Grashof number replaces the Reynolds number in the convection correlation equation. In free convection, buoyancy driven flow sometimes dominates the flow inertia, therefore, the Nusselt number is a function of the Grashof number and the Prandtle number alone. Nu=f(Gr, Pr). Reynolds number will be important if there is an external flow. (see chapter 11.5, combined forced and free convection. In many instances, it is better to combine the Grashof number and the Prandtle number to define a new parameter, the Rayleigh number, Ra=GrPr. The most important use of the Rayleigh number is to characterize the laminar to turbulence transition of a free convection boundary layer flow. For example, when Ra>10 9, the vertical free convection boundary layer flow over a flat plate becomes turbulent.

Example www.mycsvtunotes.in Determine the rate of heat loss from a heated pipe as a result of natural (free) convection. T =0 C D=0.1 m T s =100C Film temperature( T f ): averaged boundary layer temperature T f =1/2(T s +T )=50 C. k f =0.03 W/m.K, Pr=0.7, =210-5 m 2 /s, b=1/t f =1/(273+50)=0.0031(1/K) gb ( TS T ) L (9.8)(0.0031)(100 0)(0.1) Ra (2 10 ) Nu D 3 3 6 Pr (0.7) 7.6 10. 2 5 2 0.387Ra [1 (0.559 / Pr) ] 1/ 6 {0.6 2 } 9 /16 8/ 27 26.0 (equation 11.15 in Table 11.1) k f 0.03 (26) 7.8( / 2 h NuD W m K ) D 0.1 q ha( T T ) (7.8)( )( 0.1)(1)(100 0) 244.9( W ) S Can be significant if the pipe are long.