Heat Radiation

Also found in: Dictionary, Medical.
Related to Heat Radiation: Heat convection

Heat radiation

The energy radiated by solids, liquids, and gases as a result of their temperature. Such radiant energy is in the form of electromagnetic waves and covers the entire electromagnetic spectrum, extending from the radio-wave portion of the spectrum through the infrared, visible, ultraviolet, x-ray, and gamma-ray portions. From most hot bodies on Earth this radiant energy lies largely in the infrared region. See Electromagnetic radiation, Infrared radiation

Radiation is one of the three basic methods of heat transfer, the other two methods being conduction and convection. See Conduction (heat), Convection (heat), Heat transfer

A hot plate at 260°F (400 K) may show no visible glow; but a hand which is held over it senses the warming rays emitted by the plate. A temperature of more than 1300°F (1000 K) is required to produce a perceptible amount of visible light. At this temperature a hot plate glows red and the sensation of warmth increases considerably, demonstrating that the higher the temperature of the hot plate the greater the amount of radiated energy. Part of this energy is visible radiation, and the amount of this visible radiation increases with increasing temperature. A steel furnace at 2800°F (1800 K) shows a strong yellow glow. If a tungsten wire (used as the filament in incandescent lamps) is raised by resistance heating to a temperature of 4600°F (2800 K), it emits a bright white light. As the temperature of a substance increases, additional colors of the visible portion of the spectrum appear, the sequence being first red, then yellow, green, blue, and finally violet. The violet radiation is of shorter wavelength than the red radiation, and it is also of higher quantum energy. In order to produce strong violet radiation, a temperature of almost 5000°F (3000 K) is required. Ultraviolet radiation necessitates even higher temperatures. The Sun emits considerable ultraviolet radiation; its temperature is about 10,000°F (6000 K). Such temperatures have been produced on Earth in gases ionized by electrical discharges. The mercury-vapor lamp and the fluorescent lamp emit large amounts of ultraviolet radiation. Temperatures up to 36,000°F (20,000 K), however, are still much too low to produce x-rays or gamma radiation. A gas maintained at temperatures above 2 × 10F (1 × 106 K), encountered in nuclear fusion experiments, emits x-rays and gamma rays. See Nuclear fusion, Ultraviolet radiation

A blackbody is defined as a body which emits the maximum amount of heat radiation. Although there exists no perfect blackbody radiator in nature, it is possible to construct one on the principle of cavity radiation. See Blackbody

Graphs of Planck's law for various temperaturesenlarge picture
Graphs of Planck's law for various temperatures

A cavity radiator is usually understood to be a heated enclosure with a small opening which allows some radiation to escape or enter. The escaping radiation from such a cavity has the same characteristics as blackbody radiation.

Kirchhoff's law correlates mathematically the heat radiation properties of materials at thermal equilibrium. It is often called the second law of thermodynamics for radiating systems. Kirchhoff's law can be expressed as follows: The ratio of the emissivity of a heat radiator to the absorptivity of the same radiator is a function of frequency and temperature alone. This function is the same for all bodies, and it is equal to the emissivity of a blackbody. A consequence of Kirchhoff's law is the postulate that a blackbody has an emissivity which is greater than that of any other body. See Kirchhoff's laws of electric circuits

Planck's radiation law represents mathematically the energy distribution of the heat radiation from 1 cm2 of surface area of a blackbody at any temperature. Formulated by Max Planck early in the twentieth century, it laid the foundation for the advance of modern physics and the advent of quantum theory.

Equation (1) is the mathematical expression of Planck's radiation law, where Rλ is the total energy radiated from the body measured in watts per square centimeter per unit wavelength, at the wavelength λ. The wavelength in this formula is measured in micrometers. The quantity T is the temperature in kelvins, and e is the base of the natural logarithms. The illustration presents graphs of Planck's law for various temperatures and shows substances which attain these temperatures. It should be noted that these substances will not radiate as predicted by Planck's law since they are not blackbodies themselves.

The Stefan-Boltzmann law states that the total energy radiated from a hot body increases with the fourth power of the temperature of the body. This law can be derived from Planck's law by the process of integration and is expressed mathematically as Eq. (2), where RT is the total amount of energy radiat

ed from a blackbody in watts per square centimeter. When RT is multiplied by the total emissivity, the total energy radiated from a real heat radiator is obtained.

McGraw-Hill Concise Encyclopedia of Physics. © 2002 by The McGraw-Hill Companies, Inc.
The following article is from The Great Soviet Encyclopedia (1979). It might be outdated or ideologically biased.

Heat Radiation


a form of electromagnetic radiation emitted by a substance as a result of its internal energy. Heat radiation is contrasted, for example, to luminescence, which results from external energy sources. Heat radiation has a continuous spectrum whose maximum is a function of the temperature of the substance. As the temperature increases, the total energy of the emitted heat radiation grows, and the maximum shifts toward shorter wavelengths. Examples of emitters of heat radiation are the surface of an incandescent metal and the earth’s atmosphere.

Heat radiation is characteristic of all nonradiative processes exhibiting detailed balancing—that is, various types of particle collisions in gases and plasma and the exchange of energy between the electronic and vibrational motions in solids. (SeeDETAILED BALANCING, PRINCIPLE OF.) The equilibrium state of a substance at each point in space, called the state of local thermodynamic equilibrium, is expressed as a temperature; moreover, the heat radiation of the substance at any given point is a function of this temperature.

In the general case of a system of bodies in which only local thermodynamic equilibrium exists and different points have different temperatures, the heat radiation is not in thermodynamic equilibrium with the substance. Hot bodies radiate more than they absorb, and the reverse is true for colder bodies. Radiative transfer from the hotter bodies to the colder bodies takes place. Maintenance of a steady state, in which the temperature distribution in the system is preserved, requires that heat be supplied to the hotter bodies and be drawn off from the colder bodies. This may occur either under natural conditions, as in the earth’s atmosphere, or artificially, as in incandescent lamps.

In complete thermodynamic equilibrium, all parts of a system of bodies have the same temperature, and the energy of the heat radiation emitted by each body is balanced by the energy of the heat radiation absorbed from other bodies. In this case the heat radiation is in thermodynamic equilibrium with the substance and is called equilibrium radiation; an example is the thermal radiation of a blackbody. The spectrum of equilibrium radiation is independent of the nature of the substance and is determined by Planck’s radiation law.

In the general case, the thermal radiation of heated bodies satisfies Kirchhoff s radiation law, which relates the bodies’ emissivity and absorptance to the emissivity of a blackbody.

Radiative transfer processes can be studied by applying Kirchhoff’s and Planck’s radiation laws to the emission and absorption of heat radiation in gases and plasma, assuming local thermodynamic equilibrium. This approach is widely used in astrophysics, particularly in the theory of stellar atmospheres.


Planck, M. Teoriia teplovogo izlucheniia. Leningrad-Moscow, 1935. (Translated from German.)
Sobolev, V. V. Perenos luchistoi energii v atmosferakh zvezd i planet. Moscow, 1956.
Bosworth, R. C. L. Protsessy teplovogo perenosa. Moscow, 1957. (Translated from English.)
El’iashevich, M. A. Atomnaia i molekuliarnaia spektroskopiia. Moscow, 1962.


The Great Soviet Encyclopedia, 3rd Edition (1970-1979). © 2010 The Gale Group, Inc. All rights reserved.

heat radiation

[′hēt ‚rād·ē′ā·shən]
The energy radiated by solids, liquids, and gases in the form of electromagnetic waves as a result of their temperature. Also known as thermal radiation.
McGraw-Hill Dictionary of Scientific & Technical Terms, 6E, Copyright © 2003 by The McGraw-Hill Companies, Inc.
References in periodicals archive ?
Thus, physics loses nothing of the Planck and Boltzmann constants, h and k, which were born from the study of heat radiation [1, 8].
Kirchhoff's results can never be validated by experiments, and Stewart, as an expert in heat radiation, must have recognized this to be the case [82].
Spectral rendering delivers thermal heat radiation and infrared identification for both thermal and night-vision in-game imaging.
The Walki Wall Tight FR G A2 can be used in walls and ceiling as a construction membrane, preventing heat radiation and moisture transfer.
13, 2018), "Heat Radiation Sheet and Heat Radiation Device," Noriji Tashiro, Michiaki Yajima, Tomonori Seki, Atsushi Fujita, Tooru Yoshikawa, and Rei Yamamoto (Hitachi Chemical Co., Ltd., Tokyo)
Therefore, those LIBs require efficient heat radiation.
Another challenge came in the form of the electronic wiring -- most cables would melt from exposure to heat radiation at such close proximity to the Sun.
Max Planck attempted to prove the validity of Kirchhoff's law in the opening sections of The Theory of Heat Radiation [14, [section]1-52].
It also acts as a reflector to increase the heat radiation into the room.
"CIRS acts as a remote-sensing thermometer and as a chemical probe, picking out the heat radiation emitted by individual gases in an atmosphere," said F.
His topics include seismic waves and evidence of Earth's interior structure, tectonic plate theory, climate and heat radiation, energy-balance equations and the greenhouse effect, energy production and consumption, and source rocks and seismology.