Thermal Systems Design MARYLAND. Fundamentals of heat transfer Radiative equilibrium Surface properties Nonideal effects


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1 Thermal Systems Design Fundamentals of heat transfer Radiative equilibrium Surface properties Nonideal effects Internal power generation Environmental temperatures Conduction Thermal system components 2006 David L. Akin  All rights reserved
2 Classical Methods of Heat Transfer Convection Heat transferred to cooler surrounding gas, which creates currents to remove hot gas and supply new cool gas Don t (in general) have surrounding gas or gravity for convective currents Conduction Direct heat transfer between touching components Primary heat flow mechanism internal to vehicle Radiation Heat transferred by infrared radiation Only mechanism for dumping heat external to vehicle
3 Ideal Radiative Heat Transfer Planck s equation gives energy emitted in a specific frequency by a black body as a function of temperature e λb = 2 2πhC 0 λ 5 exp hc 0 1 λkt (Don t worry, we won t actually use this equation for anything )
4 The Solar Spectrum Ref: V. L. Pisacane and R. C. Moore, Fundamentals of Space Systems Oxford University Press, 1994
5 Ideal Radiative Heat Transfer Planck s equation gives energy emitted in a specific frequency by a black body as a function of temperature e λb = StefanBoltzmann equation integrates Planck s equation over entire spectrum P rad =σt 4 σ = 5.67x10 8 W m 2 K 4 2 2πhC 0 λ 5 exp hc 0 1 λkt (Don t worry, we won t actually use this equation for anything ) ( StefanBoltzmann Constant )
6 Thermodynamic Equilibrium First Law of Thermodynamics Q W = du dt heat in heat out = work done internally Heat in = incident energy absorbed Heat out = radiated energy Work done internally = internal power used (negative work in this sense  adds to total heat in the system)
7 Radiative Equilibrium Temperature Assume a spherical black body of radius r Heat in due to intercepted solar flux Q in = I s π r 2 Heat out due to radiation (from total surface area) Q out = 4π r 2 σt 4 For equilibrium, set equal I s π r 2 = 4π r 2 σt 4 I s = 4σT 4 T eq = I s 4σ 1 AU: I s =1394 W/m 2 ; T eq =280 K 1 4
8 Effect of Distance on Equilibrium Temp Mercury Venus Earth Mars Asteroids Jupiter Saturn Uranus Neptune Pluto
9 Shape and Radiative Equilibrium A shape absorbs energy only via illuminated faces A shape radiates energy via all surface area Basic assumption made is that black bodies are intrinsically isothermal (perfect and instantaneous conduction of heat internally to all faces)
10 Effect of Shape on Black Body Temps
11 Incident Radiation on NonIdeal Bodies Kirchkoff s Law for total incident energy flux on solid bodies: Q Incident = Q absorbed + Q reflected + Q transmitted Q absorbed Q Incident + Q reflected Q Incident + Q transmitted Q Incident =1 α Q absorbed Q Incident ; where ρ Q reflected Q Incident ; α =absorptance (or absorptivity) ρ =reflectance (or reflectivity) τ =transmittance (or transmissivity) τ Q transmitted Q Incident
12 NonIdeal Radiative Equilibrium Temp Assume a spherical black body of radius r Heat in due to intercepted solar flux Q in = I s απ r 2 Heat out due to radiation (from total surface area) Q out = 4π r 2 εσt 4 For equilibrium, set equal (ε = emissivity  efficiency of surface at radiating heat) I s απr 2 = 4π r 2 εσt 4 I s = 4 ε α σt 4 T eq = α I s ε 4σ 1 4
13 Effect of Surface Coating on α = absorptivity ε = emissivity
14 NonIdeal Radiative Heat Transfer Full form of the StefanBoltzmann equation! where T env =environmental temperature (=4 K for space) ( ) P rad =εσa T 4 4 T env Also take into account power used internally ( ) I s α A s + P int =εσa rad T 4 4 T env
15 Example: AERCam/SPRINT 30 cm diameter sphere α=0.2; ε=0.8 P int =200W T env =280 K (cargo bay below; Earth above) Analysis cases: Free space w/o sun Free space w/sun Earth orbit w/o sun Earth orbit w/sun
16 AERCam/SPRINT Analysis (Free Space) A s = m 2 ; A rad = m 2 Free space, no sun 200W P int = εσa rad T 4 T = W m 2 K m 2 ( ) 1 4 = 354 K
17 AERCam/SPRINT Analysis (Free Space) A s = m 2 ; A rad = m 2 Free space with sun I s α A s + P int = εσa rad T 4 T = I sα A s + P int εσa rad 1 4 = 362 K
18 AERCam/SPRINT Analysis (LEO Cargo T env =280 K LEO cargo bay, no sun P int =εσa rad T 4 4 ( T env ) T = 200W W m 2 m 2 K 4 ( ) + (280 K)4 1 4 = 384 K LEO cargo bay with sun I s α A s + P int =εσa rad T 4 4 T env ( ) T = I sα A s + P int εσa rad T env = 391 K
19 Radiative Insulation Thin sheet (mylar/kapton with surface coatings) used to isolate panel from solar flux Panel reaches equilibrium with radiation from sheet and from itself reflected from sheet I s T insulation T wall Sheet reaches equilibrium with radiation from sun and panel, and from itself reflected off panel
20 MultiLayer Insulation (MLI) I s Multiple insulation layers to cut down on radiative transfer Gets computationally intensive quickly Highly effective means of insulation Biggest problem is existence of conductive leak paths (physical connections to insulated components)
21 Emissivity Variation with MLI Layers Ref: D. G. Gilmore, ed., Spacecraft Thermal Control Handbook AIAA, 2002
22 MLI Thermal Conductivity Ref: D. G. Gilmore, ed., Spacecraft Thermal Control Handbook AIAA, 2002
23 Effect of Ambient Pressure on MLI Ref: D. G. Gilmore, ed., Spacecraft Thermal Control Handbook AIAA, 2002
24 1D Conduction Basic law of onedimensional heat conduction (Fourier 1822) where K=thermal conductivity (W/m K) A=area Q = KA dt dx dt/dx=thermal gradient
25 3D Conduction General differential equation for heat flow in a solid where 2 T r,t ( ) + g(r g(r,t)=internally generated heat ρ=density (kg/m 3 ) r,t) K c=specific heat (J/kg K) K/ρc=thermal diffusivity = ρc K T( r,t) t
26 Simple Analytical Conduction Model Heat flowing from (i1) into (i) T i1 T i T i+1 Q in = KA T i T i 1 Δx Heat flowing from (i) into (i+1) Q out = KA T i+1 T i Δx Heat remaining in cell Q out Q in = ρc K T i ( j +1) T i ( j) Δt
27 Finite Difference Formulation Timemarching solution T n+1 i = T n i + d(t n i+1 2T n i + T n i 1) where d = α t x 2 α = k ρc v = thermal diffusivity For solution stability, t < x2 2α
28 Heat Pipe Schematic
29 Shuttle Thermal Control Components
30 Shuttle Thermal Control System
31 ISS Radiator Assembly
Thermal Systems Design
Thermal Systems Design Fundamentals of heat transfer Radiative equilibrium Surface properties Nonideal effects Internal power generation Environmental temperatures Conduction Thermal system components
More informationThermal Systems Design MARYLAND. Fundamentals of heat transfer Radiative equilibrium Surface properties Nonideal effects
Fundamentals of heat transfer Radiative equilibrium Surface properties Nonideal effects Internal power generation Environmental temperatures Conduction Thermal system components 2002 David L. Akin  All
More informationMARYLAND. Fundamentals of heat transfer Radiative equilibrium Surface properties Nonideal effects. Conduction Thermal system components
Fundamentals of heat transfer Radiative equilibrium Surface properties Nonideal effects Internal power generation Environmental temperatures Conduction Thermal system components 2003 David L. Akin  All
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