“ Elastic Solid Theory.—In the earlier days of the wave theory it was supposed that the whole of space was filled with something which acted like an elastic solid material in which the vibrations of the atoms of a luminous body started waves in all directions, just as the vibrations of a marble embedded in a jelly would send out waves through the jelly. ”
Percy Phillips
Summary
"Radiation," a scientific treatise by Percy Phillips, examines the principles of wave theory, energy transfer, and electromagnetic spectrum dynamics. Focusing on the interplay between light, heat, and matter, the work explores resonance, electron oscillations, and the effects of radiation on orbital mechanics.
Phillips analyzes how radiation influences temperature, pressure, and energy distribution across wavelengths, using examples like Prévost's theory of exchanges and the behavior of celestial bodies under light pressure. The text synthesizes classical wave theories with empirical observations, clarifying the mechanisms of heat emission and the role of resonance in energy conveyance. Phillips' work underscores the intricate relationship between radiation, energy distribution, and the physical properties of matter.
Quotes from Radiation (Percy Phillips)
“ We now believe that white light is an irregular wave, and that the prism manufactures from it the Fourier's series of waves to which it is equivalent. It is supposed that the manufacture is effected by means of the principle of resonance. As an example of resonance let a small tap be given to a pendulum just as it commences each swing. Then because the taps are so timed that each of them increases the swing of the pendulum by a small amount, they will very soon cause the pendulum to swing very violently even though the effect of a single tap can scarcely be detected at all. ”
“ We will further assume that the heat radiated out by the earth is exactly equal to the heat which it receives from the sun. This is scarcely an assumption, but rather an experimental fact, for experiment shows that heat is conducted from the interior of the earth to the exterior, and so is radiated, but at such a small rate that it is perfectly negligible compared with the rate at which the earth is receiving heat from the sun. ”
