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Published byHeather Dennis Modified over 9 years ago
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INTRODUCTION What is Heat Transfer ? Continuum Hypothesis
Local Thermodynamic Equilibrium Conduction Radiation Convection Energy Conservation
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WHAT IS HEAT ? In a solid body
Crystal : a three-dimensional periodic array of atoms Oscillation of atoms about their various positions of equilibrium (lattice vibration): The body possesses heat. Conductors: free electrons ↔ Dielectics
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Vibration of crystals with an atom
Longitudinal polarization vs. Transverse polarization us-1 us us+1 us+2 s s+1 s+2 s+3 s-1 us-1 us us+1 us+2 us+3 The energy of the oscillatory motions: the heat-energy of the body More vigorous oscillations: the increase in temperature of the body
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Internuclear separation distance
In a gas The storage of thermal energy: molecular translation, vibration and rotation change in the electronic state intermolecular bond energy average kinetic energy kB = × J/K Internuclear separation distance (diatomic molecule) Energy dissociation energy for state 1 dissociation energy for state 2 electronic state 2 vibrational state rotational state electronic state 1 at T = 300 K, air M = kg/kmol = m/s
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HEAT TRANSFER Heat transfer is the study of thermal energy transport within a medium or among neighboring media by Molecular interaction: conduction Fluid motion: convection Electromagnetic wave: radiation resulting from a spatial variation in temperature. Energy carriers: molecule, atom, electron, ion, phonon (lattice vibration), photon (electro-magnetic wave)
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CONTINUUM HYPOTHESIS Ex) density microscopic uncertainty
macroscopic uncertainty local value of density (3×107 molecules at sea level, 15°C, 1atm)
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microscopic uncertainty
due to molecular random motion macroscopic uncertainty due to the variation associated with spatial distribution of density In continuum, velocity and temperature vary smoothly. → differentiable Mean free path of air at STP (20°C, 1atm) lm = 66 nm, bulk motion vs molecular random motion
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LOCAL THERMODYNAMIC EQUILIBRIUM
hot wall at Th adibatic wall L adibatic wall gas cold wall at Tc a) lm << L : normal pressure b) lm ~ L : rarefied pressure c) lm >> L
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CONDUCTION Gases and Liquids Due to interactions of
atomic or molecular activities Net transfer of energy by random molecular motion Molecular random motion→ diffusion Transfer by collision of random molecular motion
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Solids Due to lattice waves induced by atomic motion In non-conductors (dielectrics): exclusively by lattice waves In conductors: translational motion of free electrons as well
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Fourier’s Law heat flux [J/(m2s) = W/m2]
k: thermal conductivity [W/m·K] As Dx → 0,
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Notation Q : amount of heat transfer [J] q : heat transfer rate [W],
: heat transfer rate per unit area [W/m2] : heat transfer rate per unit length [W/m]
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Heat Flux vector quantity
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Ex) T = constant line or surface: isothermal lines or surfaces (isotherms)
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temperature : driving potential of
heat flow heat flux : normal to isotherms along the surface of T(x, y, z) = constant T(x, y, z) = constant
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Steady-State One Dimensional Conduction
T = T(x) only steady-state
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or As Dx → 0, When k = const.,
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RADIATION Thermal Radiation
visible 0.4 0.7 ultra violet infrared thermal radiation
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Characteristics of Thermal Radiation
Independence of existence and temperature of medium Ex) ice lens black carbon paper ice lens
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2. Acting at a distance Ex) sky radiation electromagnetic wave or photon photon mean free path ballistic transport diffusion volume or integral phenomena conduction fluid: molecular random motion free electron solid: lattice vibration (phonon) diffusion or differential phenomena as long as continuum holds
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Blackbody spectral emissive power
3. Spectral and Directional Dependence quanta history of path Blackbody spectral emissive power surface emission
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Two Points of View Electromagnetic wave
Maxwell’s electromagnetic theory Useful for interaction between radiation and matter 2. Photons Planck’s quantum theory Useful for the prediction of spectral properties of absorbing, emitting medium
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Radiating Medium Transparent medium ex: air Participating medium
emitting, absorbing and scattering ex: CO2, H2O Opaque material
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Stefan-Boltzmann’s law
Blackbody: a perfect absorber Blackbody emissive power Stefan by experiment (1879): Boltzmann by theory (1884):
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Planck’s law spectral distribution of hemispherical
(The Theory of Heat Radiation, Max Planck, 1901) spectral distribution of hemispherical emissive power of a blackbody in vacuum h: Planck constant: ×10-34 J•s C0: speed of light in vacuum: ×108 m/s k: Boltzmann constant: ×10-23 J/K
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Blackbody spectral emissive power
El,b (W/m2.mm) For a real surface, Wavelength, l (mm) e : emissivity Blackbody spectral emissive power
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Ray-tracing method vs Net-radiation method
Surface Radiation Ray-tracing method vs Net-radiation method G J G: irradiation [W/m2] J: radiosity [W/m2] r : reflectivity e diffuse-gray surface at T a : absorptivity Kirchihoff’s law
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aG esT4 e diffuse-gray surface at T
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Ex) a body in an enclosure
[W] T2, e2, A2 q1 T1, e1, A1 when Tsur Ts, e, a, A q e = a Surrounding can be regarded as a blackbody.
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A1 A2 Why is the irradiation on the small object the same as ?
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A1 A2 F: view factor Reciprocity:
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CONVECTION energy transfer due to bulk or macro- scopic motion of fluid bulk motion: large number of molecules moving collectively convection: random molecular motion + bulk motion advection: bulk motion only
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solid wall hydrodynamic (or velocity) boundary layer thermal (or temperature) boundary layer at y = 0, velocity is zero: heat transfer only by molecular random motion
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solid wall When radiation is negligible, h : convection heat transfer coefficient [W/m2.K] Newton’s Law of Cooling
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Convection Heat Transfer Coefficient
not a property: depends on geometry and fluid dynamics forced convection free (natural) convection external flow Internal flow laminar flow turbulent flow
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First law of thermodynamics
ENERGY CONSERVATION First law of thermodynamics control volume (open system) material volume (closed system) control volume In a time interval Dt: steady-state:
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Surface Energy Balance
Ex) sur.
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Example 1.2 air Find: Surface emissive power E and irradiation G
Pipe heat loss per unit length, Assumptions: Steady-state conditions Radiation exchange between the pipe and the room is between a small surface in a much larger enclosure. Surface emissivity = absorptivity
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air 1. Surface emissive power and irradiation
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air 2. Heat loss from the pipe
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Conduction does not take place ?
Example 1.2 air Q: Why not ? Conduction does not take place ?
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T r air
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Example 1.4 Hydrogen-air Proton Exchange Membrane (PEM) fuel cell
Three-layer membrane electrode assembly (MEA) Anode: Cathode: (exothermic) Role of electrolytic membrane transfer hydrogen ions serve as a barrier to electron transfer Membrane needs a moist state to conduct ions. Liquid water in cathode: block oxygen from reaching cathode reaction site → need to control Tc The convection heat coefficient, h
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Find: The required cooling air velocity, V, needed to maintain steady state operation at Tc = 56.4ºC. Assumptions: Steady-state conditions Negligible temperature variations within the fuel cell Large surroundings Insulated edge of fuel cell Negligible energy flux by the gas or liquid flows
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Energy balance on the fuel cell
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Example 1.5 section A-A A A cubical cavity
ice of mass M at the fusion temperature Find: Expression for time needed to melt the ice, tm Assumptions: 1) Inner surface of wall is at through the process. 2) Constant properties 3) Steady-states, 1-D conduction through each wall 4) Conduction area of one wall =
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section A-A : latent heat of fusion
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Example 1.7 air Coating to be cured Find: 1) Cure temperature T for
2) Effect of air flow on the cure temperature for Value of h for which the cure temperature is 50°C. Assumptions: Steady-state conditions Negligible heat loss from back surface of plate Plate is very thin and a small object in large surroundings, coating absorptivity w.r.t. irradiation from the surroundings
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air coating
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air T y Coating to be cured
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Heat Transfer WHY HEAT TRANSFER ? Natural System Bio-System
Environment Sensors & Actuators Heat Transfer Energy Conversion Process Electrical & Electronics Manufac-turing
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Natural System / Temperature Distribution in the Earth
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