Thermal RadiationIntroduction and ContextThermal radiation is the transfer of energy by electromagnetic waves or photons as a result of the temperature of matter. Unlike conduction and convection, radiation does not require a material medium; energy can travel through a vacuum. Radiation therefore controls heat transfer between spacecraft and their surroundings, influences furnace and boiler design, affects building energy performance, and becomes dominant at high temperatures. All bodies above absolute zero emit radiation. The amount and spectral distribution depend primarily on temperature and, for real surfaces, on surface properties such as emissivity. A rigorous analysis requires both the thermal condition of a surface and the geometrical relationship between surfaces. This chapter develops blackbody theory, surface radiation properties, view factors, enclosure analysis, radiation networks, participating media, and radiation shields. Learning ObjectivesBy the end of this chapter, you should be able to: - Explain blackbody radiation and apply Planck’s, Stefan–Boltzmann, and Wien’s laws.
- Distinguish emissive power, intensity, irradiation, radiosity, absorptivity, reflectivity, transmissivity, and emissivity.
- Apply Kirchhoff’s law under appropriate thermal-equilibrium conditions.
- Calculate view factors using reciprocity and summation relations.
- Analyze radiation exchange between diffuse-gray surfaces using radiation networks.
- Explain gas radiation and the role of participating media.
- Evaluate radiation shields and identify assumptions and limitations in enclosure models.
1. Nature of Thermal RadiationThermal radiation occupies a broad range of electromagnetic wavelengths. Engineering thermal radiation is concentrated mainly in the infrared region, although visible and ultraviolet radiation become important at high temperatures. Radiation propagates at the speed of light in vacuum and transports energy without bulk mass motion. The wavelength λ and frequency ν are related by c = λν where c is the speed of light in vacuum, approximately 2.998 × 10⁸ m/s. Wavelength is measured in metres and frequency in hertz. The radiative energy emitted by a surface depends on temperature and wavelength, so radiation is inherently spectral. A surface may emit, absorb, reflect, and transmit incident radiation. For irradiation G incident on a surface, the fractions absorbed, reflected, and transmitted are represented by α, ρ, and τ: α + ρ + τ = 1 This relation is an energy balance for incident radiation. For an opaque surface, τ = 0, so α + ρ = 1. The symbols α, ρ, and τ are dimensionless. 2. Blackbody RadiationA blackbody is an ideal surface that absorbs all incident radiation at every wavelength and direction. Thus α = 1, ρ = 0, and τ = 0. It is also the maximum possible emitter at a specified temperature. The total blackbody emissive power, E_b, is given by the Stefan–Boltzmann law: Eb = σT⁴ Here E_b is the emitted power per unit area in W/m², T is absolute temperature in kelvin, and σ = 5.670 × 10⁻⁸ W/(m²·K⁴) is the Stefan–Boltzmann constant. The law applies to total emission integrated over all wavelengths and directions. For a real surface with emissivity ε, the total emissive power is E = εσT⁴ where ε is the total hemispherical emissivity, 0 ≤ ε ≤ 1. Emissivity may depend on wavelength, direction, temperature, surface condition, and viewing direction. Treating it as a constant is the diffuse-gray approximation. Planck’s spectral distribution lawPlanck’s law gives the blackbody spectral emissive power per unit wavelength: Ebλ = (C₁)/(λ⁵[exp(C₂/(λT)) − 1]) where E_{bλ} is in W/(m²·length), λ is wavelength, T is absolute temperature, C₁ = 3.742 × 10⁻¹⁶ W·m², and C₂ = 1.439 × 10⁻² m·K. The units of E_{bλ} must be consistent with the chosen unit for λ. Integration over all wavelengths gives E_b = σT⁴. Planck’s law shows that increasing temperature both raises total emission and shifts the spectrum toward shorter wavelengths. Wien’s displacement lawThe wavelength at which blackbody spectral emission is maximum is λmaxT = 2898 μm·K This is useful for selecting infrared detectors, estimating furnace radiation, and interpreting thermal-imaging data. For example, a surface at 1000 K has λ_max ≈ 2.90 μm, in the infrared region. Directional distribution and intensityA diffuse emitter has direction-independent intensity when measured per unit projected area. For a diffuse blackbody, the total emissive power and intensity I_b are related by Eb = πIb The factor π results from integration over the hemisphere. Radiation intensity has units W/(m²·sr), where sr denotes steradian. The cosine dependence of projected area is called Lambert’s cosine law. 3. Surface Radiation PropertiesFour properties are central to surface analysis: | Property | Symbol | Meaning |
|---|
| Absorptivity | α | Fraction of incident radiation absorbed | | Reflectivity | ρ | Fraction reflected | | Transmissivity | τ | Fraction transmitted | | Emissivity | ε | Emission relative to a blackbody at the same temperature |
Properties may be spectral or total, and directional or hemispherical. A polished metal often has low absorptivity and emissivity in the infrared, whereas an oxidized or roughened surface generally has higher emissivity. For an opaque surface, α + ρ = 1. A blackbody has α = ε = 1. A transparent medium can have significant τ, while most engineering solids are treated as opaque to thermal infrared radiation. Kirchhoff’s lawAt thermal equilibrium, for a given wavelength and direction, ελ,θ = αλ,θ Thus a good absorber is a good emitter under the same spectral and directional conditions. For a diffuse-gray surface, this commonly becomes ε = α. Kirchhoff’s law should not be applied carelessly when the source and surface temperatures differ substantially, when properties are strongly spectral, or when directional effects are important. The rigorous equality is between corresponding spectral-directional properties, not necessarily between arbitrary total properties. Gray and diffuse surfacesA gray surface has properties independent of wavelength over the relevant band. A diffuse surface has properties independent of direction. A diffuse-gray surface is a useful engineering idealization, but real surfaces can be selective, specular, semitransparent, rough, or directionally dependent. 4. Net Radiation ExchangeFor a small surface exposed to large black surroundings at temperature T_sur, the net radiative heat transfer from the surface is Q̇ = εAσ(Ts⁴ − Tsur⁴) where Q̇ is in watts, A is surface area in m², T_s and T_sur are absolute temperatures in kelvin, and ε is the surface emissivity. The surroundings must behave approximately as a large isothermal black enclosure. Positive Q̇ denotes net heat loss from the surface. The fourth-power dependence makes radiation increasingly important at high temperature. Temperatures must always be expressed in kelvin; using degrees Celsius directly in T⁴ is invalid. Worked Example 1: Surface exchange with large surroundingsA blackened surface of area 0.50 m² is at 500 K inside a large enclosure at 300 K. Estimate its net radiative heat loss. For a black surface, ε = 1: Q̇ = (1)(0.50)(5.670 × 10⁻⁸)(500⁴ − 300⁴) Since 500⁴ = 6.25 × 10¹⁰ and 300⁴ = 8.10 × 10⁹ K⁴, Q̇ = 0.50 × 5.670 × 10⁻⁸ × 5.44 × 10¹⁰ ≈ 1543 W The surface loses approximately 1.54 kW. The result assumes a black, isothermal enclosure and negligible convection. 5. View FactorsRadiation exchange depends on geometry. The view factor F_{i→j} is the fraction of radiation leaving surface i that directly reaches surface j. It is dimensionless and lies between zero and one. For two differential areas dA_i and dA_j separated by distance R, dFi→j = (cosθi cosθj)/(πR²) dAj where θ_i and θ_j are the angles between the connecting line and the outward normals. This differential relation applies to diffuse emission in a nonparticipating medium with unobstructed line of sight. For finite surfaces, Fi→j = (1/Ai) ∫Ai∫Aj (cosθi cosθj)/(πR²) dAj dAi The two most important view-factor relations are reciprocity and summation. Reciprocity relationAiFi→j = AjFj→i This relation allows an unknown factor to be calculated from a known factor and the two areas. Summation relationFor a surface in an enclosure, ∑j Fi→j = 1 The summation includes all surfaces visible from i, including itself where self-view is possible. A plane or convex surface has F_{i→i} = 0. A concave surface can have a nonzero self-view factor. Worked Example 2: View-factor calculationSurface 1 has area 2 m² and surface 2 has area 5 m². If F_{1→2} = 0.30, find F_{2→1}. Using reciprocity, F2→1 = (A1/A2)F1→2 = (2/5)(0.30) = 0.12 Thus 12% of radiation leaving surface 2 reaches surface 1. The result is geometrically consistent because the larger surface 2 views the smaller surface 1 less extensively. 6. Radiation Exchange Between Black SurfacesFor two black surfaces in an enclosure, the net exchange between surfaces i and j is Q̇i→j = AiFi→jσ(Ti⁴ − Tj⁴) The expression assumes black surfaces, diffuse emission, a nonparticipating medium, and direct exchange represented by the view factor. In a multi-surface enclosure, the net heat transfer from surface i is the sum of exchanges with all other surfaces: Q̇i = ∑j AiFi→jσ(Ti⁴ − Tj⁴) For real surfaces, reflection causes multiple reflections, so the black-surface expression is generally insufficient. 7. Diffuse-Gray Enclosures and Radiation NetworksFor an opaque diffuse-gray surface, the radiosity J_i is the total radiation leaving the surface per unit area. It consists of emitted radiation plus reflected irradiation: Ji = εiσTi⁴ + ρiGi For an opaque gray surface, ρ_i = 1 − ε_i. Therefore, Ji = εiσTi⁴ + (1 − εi)Gi The net heat flux leaving surface i is qi = Ji − Gi Combining these equations gives the surface resistance form: Q̇i = [Ebi − Ji]/[(1 − εi)/(εiAi)] where E_{bi} = σT_i⁴. The denominator is the surface resistance, measured in m⁻² when used with total power and area as shown. The space resistance between surfaces i and j is Rij = 1/(AiFi→j) For a two-surface enclosure, the net exchange is Q̇1→2 = [σ(T1⁴ − T2⁴)] / [(1 − ε1)/(ε1A1) + 1/(A1F1→2) + (1 − ε2)/(ε2A2)] This formula assumes two diffuse-gray, opaque, isothermal surfaces enclosing a nonparticipating medium. It includes surface and space resistances. If both surfaces are black, the surface resistances vanish. Worked Example 3: Two-surface gray enclosureTwo large parallel plates each have area 1 m². Plate 1 is at 800 K with ε₁ = 0.80; plate 2 is at 500 K with ε₂ = 0.60. For large facing plates, F_{1→2} = 1. Find the net exchange. The blackbody emissive-power difference is σ(T1⁴ − T2⁴) = 5.670 × 10⁻⁸(800⁴ − 500⁴) ≈ 20,083 W/m² The total resistance is R = (1 − 0.80)/(0.80 × 1) + 1/(1 × 1) + (1 − 0.60)/(0.60 × 1) R = 0.25 + 1 + 0.667 = 1.917 m⁻² Therefore, Q̇1→2 = 20,083/1.917 ≈ 10,475 W The net heat transfer is approximately 10.5 kW from plate 1 to plate 2. The gray-surface result is substantially lower than the blackbody result because both surfaces resist emission and absorption. 8. Radiation ShieldsA radiation shield is a low-emissivity surface inserted between hot and cold surfaces to reduce radiative heat transfer. For two large parallel black surroundings with N identical, thin, low-emissivity shields, each shield introduces two surface resistances. If all surfaces have emissivity ε and the areas are equal, the net exchange can be written Q̇ = Aσ(Th⁴ − Tc⁴)/[(N + 1)/ε − N] For N = 0, this reduces to the two-surface result for equal-emissivity surfaces. The expression assumes large parallel surfaces, equal areas, diffuse-gray opaque shields, negligible conduction through supports, and a nonparticipating medium. Radiation shields are used in cryogenic systems, vacuum insulation, spacecraft thermal control, and high-temperature equipment. Practical designs must account for shield supports, contact conduction, gas conduction, surface contamination, and imperfect geometry. A shiny shield may have low infrared emissivity but can lose performance when oxidized or coated with dust. 9. Participating MediaA nonparticipating medium neither absorbs, emits, nor scatters thermal radiation appreciably. Vacuum and many clean, short gas paths can often be treated this way. A participating medium interacts with radiation through absorption, emission, and scattering. Combustion gases containing CO₂ and H₂O, soot, dust, smoke, and semitransparent solids are important examples. For a uniform, non-scattering absorbing-emitting medium, the spectral intensity changes along a path according to the radiative transfer equation: dI_λ/ds = −κ_λI_λ + κ_λIbλ Here I_λ is spectral intensity, s is path length, κ_λ is the absorption coefficient, and I_{bλ} is blackbody spectral intensity at the local medium temperature. The first term represents attenuation of radiation and the second represents emission by the medium. For a constant-property, isothermal medium with no incident radiation at the far end, the solution is I_λ(s) = Ibλ[1 − exp(−κ_λs)] The quantity κ_λs is the spectral optical thickness. Small optical thickness indicates a nearly transparent medium; large optical thickness indicates strong absorption and emission. Real gases are highly spectral rather than gray, so band models, weighted-sum-of-gray-gases methods, and numerical radiation solvers are often required. Radiation through participating media is important in furnaces, gas turbines, engines, atmospheric science, and fire safety. Surface-only enclosure methods are not adequate when the medium itself emits or absorbs significant energy. 10. Practical Analysis ProcedureA reliable enclosure calculation can follow this sequence: - Draw the enclosure and identify all surfaces, temperatures, areas, and surface properties.
- Decide whether the medium is nonparticipating or participating.
- Determine whether surfaces are black, gray, diffuse, opaque, isothermal, or semitransparent.
- Obtain view factors from geometry, tables, analytical relations, or numerical methods.
- Check reciprocity and summation relations.
- Use blackbody exchange equations for black surfaces and radiosity networks for gray surfaces.
- Use kelvin for all absolute-temperature powers.
- Check energy conservation: in a closed steady enclosure, the sum of net surface heat rates is zero unless there is an internal source or sink.
- Compare the result with limiting cases, such as ε → 1 or T₁ = T₂.
Applied Case: Thermal Control of a Vacuum FurnaceBackgroundAn illustrative industrial case concerns a steel heat-treatment furnace operating at 1100 K. The furnace walls are at 700 K, and the workpiece is initially at 500 K. Because the chamber is evacuated, convection is negligible. The workpiece receives radiation from the walls and hot internal heating surfaces. ProblemThe furnace designer must estimate radiative heating and decide whether a low-emissivity shield near the door will reduce heat loss without excessively increasing heating time. AnalysisThe chamber is first modeled as a diffuse-gray enclosure. The workpiece, walls, door, and heating elements are assigned areas, temperatures, and emissivities. View factors are generated from the geometry and checked using reciprocity. Since the workpiece is not black, its radiosity includes reflected irradiation. A radiation-network solution is therefore more appropriate than a simple blackbody exchange equation. The door is identified as a major loss path because it has a relatively large area and views the colder surroundings. Installing a low-emissivity shield on the inner door reduces the effective radiative coupling. However, the shield must be supported, and its supports create conductive heat leaks. Oxidation can also increase emissivity during service. Approach and outcomeThe design team compares three cases: no shield, one polished metal shield, and two shields with thermally isolated supports. The predicted radiative loss decreases strongly with each additional shield, but the improvement from the second shield is smaller when support conduction is included. The selected design uses one replaceable shield, a reflective surface protected from oxidation, and temperature instrumentation near the door. Learning pointsThe case illustrates that radiation design is not based on emissivity alone. Geometry, view factors, spectral surface condition, conduction through supports, participating gases, and maintenance environment all affect performance. A mathematically ideal shield can perform poorly if its low-emissivity surface is contaminated or if its supports bypass the intended thermal resistance. Limitations, Safety, and Contemporary PracticeRadiation calculations can be inaccurate when real surfaces are treated as gray despite strong spectral selectivity, when temperatures are nonuniform, or when reflections are specular rather than diffuse. View-factor errors can also dominate the result. In combustion systems, ignoring gas radiation may substantially underpredict wall heat flux. Radiation is non-ionizing in most heat-transfer applications, but high-temperature equipment presents severe burn, fire, and eye hazards. Furnace and laser systems require shielding, interlocks, suitable materials, and compliance with occupational and equipment safety standards. Thermal cameras must be calibrated and must use correct emissivity settings; a camera reading from a polished metal surface can be seriously misleading because reflected surroundings may dominate the signal. Modern practice increasingly combines infrared measurements, computational view-factor methods, Monte Carlo ray tracing, finite-volume radiation solvers, and spectral gas models. Artificial intelligence can assist with surrogate modeling, fault detection, and inverse estimation of emissivity, but it does not remove the need for energy balances, calibrated data, physical validation, and clear uncertainty estimates. Chapter SummaryThermal radiation is electromagnetic energy emitted by matter because of temperature and can transfer heat through a vacuum. A blackbody is the ideal absorber and emitter. Planck’s law describes spectral emission, Wien’s law locates the peak wavelength, and the Stefan–Boltzmann law gives total emission as σT⁴. Real-surface behavior is described by absorptivity, reflectivity, transmissivity, and emissivity. For opaque surfaces, α + ρ = 1; at thermal equilibrium, Kirchhoff’s law gives the corresponding spectral-directional equality ε = α. View factors describe geometric coupling and obey reciprocity and summation rules. Black-surface exchange can be calculated directly using view factors. Diffuse-gray enclosure problems require radiosity, irradiation, surface resistances, and space resistances. Radiation shields reduce exchange by adding resistance, although conduction through supports and surface degradation limit performance. Participating media absorb, emit, and scatter radiation, requiring radiative-transfer methods rather than surface-only models. Key TermsBlackbody: Ideal absorber and maximum emitter at a specified temperature. Blackbody emissive power: Total radiation emitted per unit area by a blackbody. Planck’s law: Relation describing blackbody spectral emission as a function of wavelength and temperature. Stefan–Boltzmann law: Relation E_b = σT⁴ for total blackbody emission. Wien’s displacement law: Relation locating the wavelength of maximum blackbody emission. Emissivity: Ratio of a surface’s emission to blackbody emission at the same temperature. Absorptivity: Fraction of incident radiation absorbed by a surface. Reflectivity: Fraction of incident radiation reflected. Transmissivity: Fraction of incident radiation transmitted. Kirchhoff’s law: Equality of corresponding emissivity and absorptivity at thermal equilibrium. Irradiation: Radiation incident on a surface per unit area. Radiosity: Total radiation leaving a surface per unit area. View factor: Fraction of radiation leaving one surface that directly reaches another. Reciprocity relation: A_iF_{i→j} = A_jF_{j→i}. Diffuse surface: Surface whose radiation properties are independent of direction. Gray surface: Surface whose properties are approximated as independent of wavelength. Participating medium: Medium that absorbs, emits, or scatters radiation. Optical thickness: Measure of attenuation along a radiative path, commonly κs. Radiation shield: Intermediate low-emissivity surface used to reduce radiative exchange. Review QuestionsShort Answer Questions- Why can thermal radiation transfer energy through a vacuum?
- Define emissivity and absorptivity.
- State the Stefan–Boltzmann law and identify its variables.
- What is a view factor, and why must it satisfy a summation relation?
- Distinguish irradiation from radiosity.
Long Answer Questions- Explain Planck’s law, Wien’s displacement law, and the Stefan–Boltzmann law and describe how they are related.
- Derive the two-surface diffuse-gray radiation-exchange equation using surface and space resistances.
- Explain Kirchhoff’s law and discuss why spectral and directional qualifications are important.
- Describe the assumptions behind a radiation network for a diffuse-gray enclosure.
- Explain how participating gases differ from nonparticipating media and identify engineering applications of each model.
Analytical / Application Questions- Two parallel plates are at 900 K and 400 K, with emissivities 0.75 and 0.50. Develop the radiation-network equation for their net exchange and identify every resistance.
- A concave furnace wall views itself as well as a heating element. Explain how the self-view factor affects the summation relation and the enclosure calculation.
- A cryogenic vessel uses three polished shields. Evaluate qualitatively how oxidation, support conduction, and residual gas pressure could change the predicted performance.
Multiple Choice Questions with AnswersQuestion 1Which law gives the total blackbody emissive power? A. Wien’s displacement law B. Stefan–Boltzmann law C. Kirchhoff’s law D. Fourier’s law Correct Answer: B. Stefan–Boltzmann law Question 2A blackbody has which property combination? A. ε = 0 and α = 0 B. ε = 1 and α = 0 C. ε = 1 and α = 1 D. ε = 0 and α = 1 Correct Answer: C. ε = 1 and α = 1 Question 3For two surfaces, which relation expresses view-factor reciprocity? A. F₁→₂ = F₂→₁ B. A₁F₁→₂ = A₂F₂→₁ C. A₁F₂→₁ = A₂F₁→₂ D. F₁→₂ + F₂→₁ = 1 Correct Answer: B. A₁F₁→₂ = A₂F₂→₁ Question 4What is the correct temperature scale for the term σT⁴? A. Celsius B. Fahrenheit C. Kelvin D. Any linear temperature scale Correct Answer: C. Kelvin Question 5For an opaque surface, which relation is correct? A. α + ρ + τ = 0 B. α + ρ = 1 C. α = ρ = τ D. ε + α = 1 Correct Answer: B. α + ρ = 1 Question 6A surface at 1000 K has a blackbody peak wavelength closest to: A. 0.29 μm B. 2.90 μm C. 29.0 μm D. 290 μm Correct Answer: B. 2.90 μm Question 7In a diffuse-gray radiation network, the space resistance between surfaces i and j is: A. 1/(A_iF_i→j) B. (1 − ε_i)/(ε_iA_i) C. ε_iA_iF_i→j D. A_i/A_j Correct Answer: A. 1/(A_iF_i→j) Question 8Which statement best describes radiosity? A. Radiation incident on a surface B. Radiation absorbed by a surface C. Total radiation leaving a surface D. Radiation transmitted through a surface Correct Answer: C. Total radiation leaving a surface Question 9Which medium is participating? A. Ideal vacuum B. Clean, transparent short air path under suitable conditions C. Combustion gas containing CO₂ and H₂O D. Perfectly nonabsorbing space Correct Answer: C. Combustion gas containing CO₂ and H₂O Question 10The principal purpose of a low-emissivity radiation shield is to: A. Increase convection B. Add radiative resistance between hot and cold surfaces C. Increase the view factor to the cold surface D. Convert radiation into mass transfer Correct Answer: B. Add radiative resistance between hot and cold surfaces
|