Thermal Emittance: Infrared Radiative Property
Thermal emittance (ε) describes how effectively a real surface emits thermal radiation compared with an ideal blackbody at the same temperature. Values range from 0 to 1, with higher emittance indicating stronger radiative heat loss. Emittance complements absorptance, reflectance, and transmittance in characterising surface energy balance.
This article explores the definition of thermal emittance, surveys historical research on emissive materials, explains conceptual relationships with spectral quantities, outlines measurement techniques, and highlights applications in architecture, manufacturing, and aerospace. Pair emittance insights with the thermal conductivity explainer to evaluate combined heat transfer modes.
Definition and Energy Balance
Emittance is defined as the ratio of the radiant exitance of a surface to that of a blackbody at the same absolute temperature: ε = M / M_b. Radiant exitance M has units of W·m⁻². A blackbody emits M_b = σT⁴, where σ is the Stefan–Boltzmann constant (5.670374419 × 10⁻⁸ W·m⁻²·K⁻⁴). Emittance may be total—integrated over all wavelengths—or spectral, varying with wavelength and direction.
In engineering calculations, emittance often refers to hemispherical total emittance, assuming uniform properties over the hemisphere of outgoing radiation. Energy balance equations combine emittance with convection and conduction terms to predict surface temperatures, particularly when surfaces exchange heat with cold skies or deep space.
Kirchhoff’s law links emittance and absorptance: at thermal equilibrium, ε equals absorptance at each wavelength and direction. Materials that efficiently absorb solar radiation also tend to emit strongly in the thermal infrared, a principle harnessed in passive cooling coatings and selective emitters.
Historical Development
Research into thermal radiation dates to the 19th century with Gustav Kirchhoff’s formulation of emission and absorption laws and Josef Stefan’s empirical relationship between radiant power and temperature. Ludwig Boltzmann derived the theoretical underpinning, establishing the Stefan–Boltzmann law that anchors emittance today.
The 20th century saw rapid development of emissivity measurements for aerospace and industrial applications. Ceramic coatings, black paints, and anodised aluminium surfaces were characterised to manage spacecraft heat loads. Building scientists evaluated roofing materials, leading to cool roof standards that specify both solar reflectance and thermal emittance.
Standards organisations such as ASTM and ISO codified measurement methods, including ASTM E408 for roofing materials and ISO 20473 for thermal radiation terminology. Contemporary research extends to nanostructured surfaces and metamaterials that tailor emittance for radiative cooling or thermophotovoltaic devices.
Conceptual Relationships
Emittance can be directional, spectral, or band-averaged. Spectral emittance ε(λ) describes emission efficiency at wavelength λ, while directional emittance accounts for angular dependence. Integrating ε(λ) with the Planck distribution yields total emittance, linking the metric to spectral radiance and other radiometric quantities.
Surfaces often exhibit selective behavior: low emittance in the solar spectrum (to limit heat gain) and high emittance in the thermal infrared (to promote cooling). Designers evaluate these trade-offs alongside conductive metrics like the U-value to balance radiation, convection, and conduction.
Emittance vs. Reflectance and Absorptance
For opaque materials, absorptance plus reflectance equals one. Because ε equals absorptance in thermal equilibrium, specifying either property effectively defines the other. Low-emittance (low-e) coatings reduce heat loss through windows by reflecting long-wave infrared radiation back into conditioned spaces.
Measurement Techniques
Laboratories measure thermal emittance using emissometers, integrating spheres, or calorimetric methods. Hemispherical emittance is often determined by heating a sample to a known temperature and comparing emitted radiation with a reference blackbody. Spectral measurements employ Fourier-transform infrared (FTIR) spectrometers with directional accessories to resolve wavelength-dependent behavior.
Accurate results require accounting for surface roughness, oxidation, and temperature dependence. Calibration relies on reference materials with certified emittance values. Data processing includes correcting for reflected ambient radiation and ensuring that samples reach steady-state temperature before measurement.
Practitioners document instrument configuration, detector type, and spectral range. Integrating emittance data with system models often involves the heat exchanger NTU calculator or whole-building simulations that weigh radiative and convective fluxes simultaneously.
Applications and Strategic Importance
In building science, high thermal emittance roofing materials enable nocturnal radiative cooling, lowering HVAC loads. Cool roof programs evaluate both solar reflectance and ε to certify products. Designers compare emittance with ground-loop performance using the geothermal heat pump evaluator when optimising energy retrofits.
Aerospace engineers specify emittance for spacecraft radiators, thermal blankets, and re-entry shields to manage extreme heat fluxes. Manufacturing sectors employ controlled emittance in furnaces, thermal spray coatings, and additive manufacturing to regulate component temperatures.
Policy frameworks addressing urban heat islands and energy efficiency incorporate emittance metrics alongside U-values and solar reflectance. Understanding ε equips professionals to select materials, design thermal systems, and justify investments in energy-saving technologies documented with tools like the data center heat reuse calculator.