How We Measure the Radiation of Heat

This is one of the fundamental relationships of modern physics:

_Q__body = ε_A_σ_T_⁴.

It was discovered experimentally by Josef Stefan in 1879, and verified

theoretically by Ludwig Boltzmann; it is known as the _Stefan-Boltzmann

Law_. This formula tells us the amount of radiant energy, Q_body, that

will be emitted by a body having the surface area _A_ when it is at the

temperature _T_. Temperature, here, is measured in degrees Rankine (°R),

or Fahrenheit temperature above absolute zero (to calculate degrees

Rankine, add 460 to the temperature in degrees Fahrenheit). The

expression ε_A_ is used to show that only a certain fraction of the

energy that would leave a perfect black body of area _A_ will actually

leave a real body of the same size; the size of this fraction is

determined by the body’s emissivity. The symbol σ is a quantity we call

the _Stefan-Boltzmann constant_.

We can also calculate the heat from the sun that will be absorbed by a

body. If we let _S_ be the total amount of solar energy that would be

absorbed by a perfect black body, α_S_ will be the amount that is

actually absorbed by a body with an absorptivity of α for solar

radiation. If our body is a spherical satellite, the sun’s rays will

only strike it from a single direction. Thus only an area equivalent to

the sphere’s cross-section (largest inscribed circle) will receive

energy at any one time. Since, _as shown in the sketch_, this area (_a_

= π_r_²) is one-fourth that of the sphere’s total surface area (_A_ =

4π_r_²), we know that the radiant energy from the sun that is absorbed

will be

_Q__sun = (_A_)/(4)α_S_.

A man-made satellite’s position relative to the earth is very like that

of the earth in relation to the sun; the earth, after all, is itself a

satellite of the sun. And during most of its useful life a satellite

will be in _thermal equilibrium_—it will be losing just as much heat

energy by its own radiation into space as it will be gaining from other

sources, primarily the sun. Since the total amount of energy it absorbs

is equal to the amount of energy it emits, _Q__body is equal to _Q__sun.

This means that we have the equality

ε_A_σ_T_⁴ = (_A_)/(4)α_S_.

Satellite Communications Physics · 第 33 / 75 题