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In physics, a 'black body' is an object that absorbs all electromagnetic radiation that falls onto it. No radiation passes through it and none is reflected. It is this lack of both transmission and reflection to which the name refers. These properties make black bodies ideal sources of thermal radiation. That is, the amount and wavelength (color) of electromagnetic radiation they emit is directly related to their temperature. Black bodies below around 700 K (430 °C) produce very little radiation at visible wavelengths and appear black (hence the name). Black bodies above this temperature however, produce radiation at visible wavelengths starting at red, going through orange, yellow, and white before ending up at blue as the temperature increases.
The term "black body" was introduced by Gustav Kirchhoff in 1860. The light emitted by a black body is called 'black-body radiation' (or cavity radiation), and has a special place in the history of quantum mechanics.^[1]

Contents

Explanation

Equations governing black bodies

Planck's law of black-body radiation

Wien's displacement law

Stefan-Boltzmann law

Radiation emitted by a human body

Temperature relation between a planet and its star

Factors

Assumptions

Derivation

The result

Temperature of the Sun

See also

References

Other textbooks

External links

Explanation

In the laboratory, a black body radiation is approximated by the radiation from a small hole entrance to a large cavity, a hohlraum. Any light entering the hole would have to reflect off the walls of the cavity multiple times before it escaped, in which process it is nearly certain to be absorbed. This occurs regardless of the wavelength of the radiation entering (as long as it is small compared to the hole). The hole, then, is a close approximation of a theoretical black body and, if the cavity is heated, the spectrum of the hole's radiation (i.e., the amount of light emitted from the hole at each wavelength) will be continuous, and will not depend on the material in the cavity (compare with emission spectrum). By a theorem proved by Kirchhoff, this curve depends ''only'' on the temperature of the cavity walls.^[2]
Calculating this curve was a major challenge in theoretical physics during the late nineteenth century. The problem was finally solved in 1901 by Max Planck as Planck's law of black-body radiation.^[3]
By making changes to Wien's Radiation Law (not to be confused with Wien's displacement law) consistent with Thermodynamics and Electromagnetism, he found a mathematical formula fitting the experimental data in a satisfactory way. To find a physical interpretation for this formula, Planck had then to assume that the energy of the oscillators in the cavity was quantized (i.e., integer multiples of some quantity). Einstein built on this idea and proposed the quantization of electromagnetic radiation itself in 1905 to explain the photoelectric effect. These theoretical advances eventually resulted in the superseding of classical electromagnetism by quantum electrodynamics. Today, these quanta are called photons and the black body cavity may be thought of as containing a gas of photons. In addition, it led to the development of quantum versions of statistical mechanics, called Fermi-Dirac statistics and Bose-Einstein statistics, each applicable to a different class of particles. ''See also'' fermion ''and'' boson.

The wavelength at which the radiation is strongest is given by Wien's displacement law, and the overall power emitted per unit area is given by the Stefan-Boltzmann law. So, as temperature increases, the glow color changes from red to yellow to white to blue. Even as the peak wavelength moves into the ultra-violet enough radiation continues to be emitted in the blue wavelengths that the body will continue to appear blue. It will never become invisible — indeed, the radiation of visible light increases monotonically with temperature.^[4]
The radiance or observed intensity is not a function of direction. Therefore a black body is a perfect Lambertian radiator.
Real objects never behave as full-ideal black bodies, and instead the emitted radiation at a given frequency is a fraction of what the ideal emission would be. The emissivity of a material specifies how well a real body radiates energy as compared with a black body. This emissivity depends on factors such as temperature, emission angle, and wavelength. However, it is typical in engineering to assume that a surface's spectral emissivity and absorptivity do not depend on wavelength, so that the emissivity is a constant. This is known as the 'grey body' assumption.
Although Planck's formula predicts that a black body will radiate energy at all frequencies, the formula is only applicable when many photons are being measured. For example, a black body at room temperature (300 K) with one square meter of surface area will emit a photon in the visible range once every thousand years or so, meaning that for most practical purposes, the black body does not emit in the visible range.
When dealing with non-black surfaces, the deviations from ideal black body behavior are determined by both the geometrical structure and the chemical composition, and follow Kirchhoff's Law: emissivity equals absorptivity, so that an object that does not absorb all incident light will also emit less radiation than an ideal black body.

In astronomy, objects such as stars are frequently regarded as black bodies, though this is often a poor approximation. An almost perfect black-body spectrum is exhibited by the cosmic microwave background radiation. Hawking radiation is black-body radiation emitted by black holes.

Equations governing black bodies

Planck's law of black-body radiation

Main articles: Planck's law of black-body radiation

::$I($
u) = rac{2 h
u^{3}}{c^2}rac{1}{e^{rac{h
u}{kT}}-1}
where
:
★ $I($
u)d
u , is the amount of energy per unit surface area per unit time per unit solid angle emitted in the frequency range between ν and ν+dν;
:
★ $T\; ,$ is the temperature of the black body;
:
★ $h\; ,$ is Planck's constant;
:
★ $c\; ,$ is the speed of light; and
:
★ $k\; ,$ is Boltzmann's constant.

Wien's displacement law

Main articles: Wien's displacement law

The relationship between the temperature ''T'' of a 'black body', and wavelength $lambda\_\{max\}$ at which the intensity of the radiation it produces is at a maximum is
:$T\; lambda\_mathrm\{max\}\; =\; 2.898...\; imes\; 10^6\; mathrm\{nm\; K\}.\; ,$
The nanometer is a convenient unit of measure for optical wavelengths. Note that 1 nanometer is equivalent to 10⁻⁹ meters.

Stefan-Boltzmann law

Main articles: Stefan-Boltzmann law

The total energy radiated per unit area per unit time $j^\{star\}$ (in watts per square meter) by a 'black body' is related to its temperature ''T'' (in kelvins) and the Stefan-Boltzmann constant $sigma$ as follows:
::$j^\{star\}\; =\; sigma\; T^4.,$

Radiation emitted by a human body

Much of a person's energy is radiated away in the form of infrared energy. Some materials are transparent to infrared light, while opaque to visible light (note the trash bag). Other materials are transparent to visible light, while opaque to the infrared (note the glasses of the person).

Black-body laws can be applied to human beings. For example, some of a person's energy is radiated away in the form of electromagnetic radiation, most of which is infrared.
The net power radiated is the difference between the power emitted and the power absorbed:
:$P\_\{net\}=P\_\{emit\}-P\_\{absorb\}\; ,$
Applying the Stefan-Boltzmann law,
:$P\_\{net\}=Asigma\; epsilon\; left(\; T^4\; -\; T\_\{0\}^4$
ight) ,.
The total surface area of an adult is about 2 m², and the mid- and far-infrared emissivity of skin and most clothing is near unity, as it is for most nonmetallic surfaces.^[5][6] Skin temperature is about 33°C,^[7] but clothing reduces the surface temperature to about 28°C when the ambient temperature is 20°C.^[8] Hence, the net radiative heat loss is about
:$P\_\{net\}\; =\; 100\; mathrm\{W\}\; ,$.
The total energy radiated in one day is about 9 MJ (million joules), or 2000 kcal (food calories). Basal metabolic rate for a 40-year-old male is about 35 kcal/(m²·h),^[9] which is equivalent to 1700 kcal per day assuming the same 2 m² area. However, the mean metabolic rate of sedentary adults is about 50% to 70% greater than their basal rate.^[10]
There are other important thermal loss mechanisms, including convection and evaporation. Conduction is negligible since the Nusselt number is much greater than unity. Evaporation (perspiration) is only required if radiation and convection are insufficient to maintain a steady state temperature. Free convection rates are comparable, albeit somewhat lower, than radiative rates.^[11] Thus, radiation accounts for about 2/3 of thermal energy loss in cool, still air. Given the approximate nature of many of the assumptions, this can only be taken as a crude estimate. Ambient air motion, causing forced convection, or evaporation reduces the relative importance of radiation as a thermal loss mechanism.
Also, applying Wien's Law to humans, one finds that the peak wavelength of light emitted by a person is
:.
This is why thermal imaging devices designed for human subjects are most sensitive to 7-14 micrometers wavelength.

Temperature relation between a planet and its star

Here is an application of black-body laws. It is a rough derivation that gives an order of magnitude answer. See p. 380-382 of ''Planetary Science'', for further discussion.^[12]

Factors

The surface temperature of a planet depends on a few factors:

★ Incident radiation (from the Sun, for example)

★ Emitted radiation (for example Earth's infrared glow)

★ The albedo effect (the fraction of light a planet reflects)

★ The greenhouse effect (for planets with an atmosphere)

★ Energy generated internally by a planet itself (This is more important for planets like Jupiter)
For the inner planets, incident and emitted radiation have the most significant impact on surface temperature. This derivation is concerned mainly with that.

Assumptions

If we assume the following:
:# The Sun and the Earth both radiate as spherical black bodies in thermal equilibrium ''with themselves''.
:# The Earth absorbs all the solar energy that it intercepts from the Sun.
then we can derive a formula for the relationship between the Earth's 'surface' temperature and the Sun's 'surface' temperature.

Derivation

To begin, we use the Stefan-Boltzmann law to find the total power (energy/second) the Sun is emitting:

::$P\_\{S\; emt\}\; =\; left(\; sigma\; T\_\{S\}^4$
ight) left( 4 pi R_{S}^2
ight) qquad qquad (1)
:where
::$sigma\; ,$ is the Stefan-boltzmann constant,
::$T\_S\; ,$ is the surface temperature of the Sun, and
::$R\_S\; ,$ is the radius of the Sun.
The Sun emits that power equally in ''all'' directions. Because of this, the Earth is hit with only a tiny fraction of it. This is the power from the Sun that the Earth absorbs:
::
ight) qquad qquad (2)
:where
::$R\_\{E\}\; ,$ is the radius of the Earth and
::$D\; ,$ is the distance between the Sun and the Earth.
Even though the earth only absorbs as a circular area $pi\; R^2$, it emits equally in all directions as a sphere:
::$P\_\{E\; emt\}\; =\; left(\; sigma\; T\_\{E\}^4$
ight) left( 4 pi R_{E}^2
ight) qquad qquad (3)
:where $T\_\{E\}$ is the surface temperature of the earth.
Now, in the first assumption the earth is in thermal equilibrium, so the power absorbed must equal the power emitted:
::$P\_\{E\; abs\}\; =\; P\_\{E\; emt\},$
:So plug in equations 1, 2, and 3 into this and we get
::$left(\; sigma\; T\_\{S\}^4$
ight) left( 4 pi R_{S}^2
ight) left( rac{pi R_{E}^2}{4 pi D^2}
ight) = left( sigma T_{E}^4
ight) left( 4 pi R_{E}^2
ight).,
Many factors cancel from both sides and this equation can be greatly simplified.

The result

After canceling of factors, the final result is
::{|cellpadding="2" style="border:2px solid #ccccff"
|align="center" |
|-
|where
|-
|$T\_S\; ,$ is the surface temperature of the Sun,
|-
|$R\_S\; ,$ is the radius of the Sun,
|-
|$D\; ,$ is the distance between the Sun and the Earth, and
|-
|$T\_E\; ,$ is the average surface temperature of the Earth.
|}
In other words, the temperature of the Earth only depends on the surface temperature of the Sun, the radius of the Sun, and the distance between the Earth and the Sun.

Temperature of the Sun

If we substitute in the measured values for Earth,
::
::$R\_\{S\}\; =\; 6.96\; imes\; 10^8\; mathrm\{m\},$
::$D\; =\; 1.5\; imes\; 10^\{11\}\; mathrm\{m\},$
we'll find the effective temperature of the Sun to be
::
This is within three percent of the standard measure of 5780 kelvins which makes the formula valid for most scientific and engineering applications.

See also

★ Effective temperature

★ Color temperature

★ Infrared thermometer

★ Photon polarization

★ Ultraviolet catastrophe

References

1. When used as a compound adjective, the term is typically hyphenated, as in "black-body radiation", or combined into one word, as in "blackbody radiation". The hyphenated and one-word forms should not generally be used as nouns.
2. Statistical Mechanics, , Kerson, Huang, John Wiley & Sons, 1967,
3. On the Law of Distribution of Energy in the Normal Spectrum, , Max, Planck, Annalen der Physik,
4. Statistical Physics, , L. D., Landau, Butterworth-Heinemann, 1996,
5. Emissivity Values for Common Materials Infrared Services
6. Emissivity of Common Materials Omega Engineering
7. Temperature of a Healthy Human Elert, G. (ed.)
8. Theoretical Prediction and Measurement of the Fabric Surface Apparent Temperature in a Simulated Man/Fabric/Environment System Lee, B.
9. A Biometric Study of Human Basal Metabolism., Harris J, Benedict F, , , Proc Natl Acad Sci U S A, 1918
10. Nonexercise activity thermogenesis (NEAT): environment and biology, Levine, J, , , Am J Physiol Endocrinol Metab, 2004
11. Heat Transfer and the Human Body DrPhysics.com
12. Planetary Science: The Science of Planets Around Stars (1st ed.), Cole, George H. A.; Woolfson, Michael M., , , Institute of Physics Publishing, 2002, ISBN 0-7503-0815-X

Other textbooks

★ Thermal Physics (2nd ed.), Kroemer, Herbert; Kittel, Charles, , , W. H. Freeman Company, 1980, ISBN 0-7167-1088-9

★ Modern Physics (4th ed.), Tipler, Paul; Llewellyn, Ralph, , , W. H. Freeman, 2002, ISBN 0-7167-4345-0

External links

★ Cooling Mechanisms for Human Body - From Hyperphysics

★ Descriptions of radiation emitted by many different objects

★ Black Body Emission Calculator

★ Black Body Emission Applet