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nydus/The Theory of Heat RadiationPublic

This text examines the physical distinction between heat conduction and heat radiation, noting that radiation is independent of the medium through which it passes. It establishes that heat rays are physically identical to light rays and applies the principles of experimental optics to the study of thermal radiation.

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Table of Contents

185.

We now turn to the discussion of the second principle, the principle of the increase of entropy, and follow closely the above discussion regarding the energy. When there is no oscillator in the field, every one of the elementary pencils, infinite in number,

retains during rectilinear propagation both its specific intensity and its entropy without change, even when reflected at the surface, assumed as plane and reflecting, which bounds the field. The system of oscillators, however, produces a change in the incident pencils and hence also a change in the entropy of the radiation propagated in the field. For the calculation of this change we need to investigate only those monochromatic rays which lie close to the natural frequency ν of the oscillators, since the rest are not altered at all by the system.

The system of oscillators is struck in the direction (θ,ϕ) within the conical element dΩ converging toward the system by a pencil polarized in some arbitrary way, the spectral intensity of which is given by the sum of the two principal intensities 𝖪 and 𝖪 with the azimuth of vibration ψ and π2+ψ respectively, which are assumed to be non-coherent. According to [eqn:(141)] (141) and [sect:182.] Sec. 182 this pencil conveys the entropy qΔν[𝖫(𝖪)+𝖫(𝖪)]dΩdt\Label[eqn](345)\upshape (345) to the system of oscillators in the time dt, where the function 𝖫(𝖪) is given by [eqn:(278)] (278). Hence this amount of entropy is taken from the field of radiation on the side of the rays arriving within dΩ. In compensation a pencil starts from the system on the other side in the same direction (θ,ϕ) within dΩ having the components 𝖪 and 𝖪 with the azimuth of vibration π2 and 0 respectively, but its entropy radiation is not represented by 𝖫(𝖪)+𝖫(𝖪), since 𝖪 and 𝖪 are not non-coherent, but by 𝖫(𝖪0)+𝖫(𝖪0)\Label[eqn](346)\upshape (346) where 𝖪0 and 𝖪0 represent the principal intensities of the pencil.

For the calculation of 𝖪0 and 𝖪0 we make use of the fact that, according to [eqn:(330)] (330) and [eqn:(335)] (335), the radiation 𝖪 and 𝖪, of which the component 𝖪 vibrates in the azimuth 0, consists of the following three components, non-coherent with one another:

𝖪1=𝖪sin2ψ+𝖪cos2ψ(1βsin2θ)=𝖪(1βsin2θcos2ψ) with the azimuth of vibration tg2ψ1=tg2ψ1βsin2θ,

𝖪2=𝖪cos2ψ+𝖪sin2ψ(1βsin2θ)=𝖪(1βsin2θsin2ψ) with the azimuth of vibration tg2ψ2=cot2ψ1βsin2θ, and, 𝖪3=βsin2θ𝖪e with the azimuth of vibration tgψ3=0.

According to [eqn:(147)] (147) these values give the principal intensities 𝖪0 and 𝖪0 required and hence the entropy radiation [eqn:(346)] (346). Thereby the amount of entropy qΔν[𝖫(𝖪0)+𝖫(𝖪0)]dΩdt\Label[eqn](347)\upshape (347) is added to the field of radiation in the time dt. All told, the entropy change of the field of radiation in the time dt, as given by subtraction of the expression [eqn:(345)] (345) from [eqn:(347)] (347) and integration with respect to dΩ, is dtΔνqdΩ[𝖫(𝖪0)+𝖫(𝖪0)𝖫(𝖪)𝖫(𝖪)].\Label[eqn](348)\upshape (348)

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