Why is ##\text{flux} = \pi\text{intensity}##

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SUMMARY

The discussion focuses on the derivation and implications of the equation ##F = \pi B##, which describes the flux at a surface of uniform brightness ##B## from a sphere of isotropic radiation. The derivation involves integrating the specific intensity over solid angles, leading to the conclusion that when the distance ##r## equals the radius ##R## of the sphere, the flux simplifies to ##F = \pi B##. Participants express concerns about the validity of the approximation used in the derivation and the physical interpretation of the result, particularly regarding the solid angle contributions.

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1632904653656.png

Textbook Derivation
Flux at an arbitrary distance from a sphere of uniform brightness ##B## (that is, all rays leaving the sphere have the same brightness). Such a sphere is clearly an isotropic source. At ##P##, the specific intensity is ##B## if the ray intersects the sphere and zero otherwise (see Fig. 1.6). Then,
$$
F=\int I \cos \theta d \Omega=B \int_{0}^{2 \pi} d \phi \int_{0}^{\theta_{c}} \sin \theta \cos \theta d \theta
$$
where ##\theta_{c}=\sin ^{-1} R / r## is the angle at which a ray from ##P## is tangent to the sphere. It follows that
$$
F=\pi B\left(1-\cos ^{2} \theta_{c}\right)=\pi B \sin ^{2} \theta_{c}
$$
or
$$
F=\pi B\left(\frac{R}{r}\right)^{2}
$$

Setting ##r=R:##
$$
F=\pi B
$$
That is, the flux at a surface of uniform brightness ##B## is simply ##\pi B##.

My worries
1. How is the equation valid when ##r=R##? The author made an approximation that ##\theta_{c}=\sin ^{-1} R / r##, and r is not the hypotenuse of the triangle, hence the approximation is only valid when ##r >> R## or ##\text{leg} \approx hypotenuse##. Rather, r is a leg. In this case, doesn't the approximation fail and vitiate the result that ##F=\pi B##?

2. Actually, which case does ##r=R## refer to? Diagram 2 or 3 below?

SmartSelect_20210929-175549_Samsung Notes.jpg

3. Is there a physical interpretation/explanation for ##F=\pi B##? The way I would think of it is that ##\pi## represents the patch of the sphere where the point resides (it is 1/4 of the whole sphere) and that this whole patch contributes to the flux at that point.
SmartSelect_20210929-175558_Samsung Notes.jpg
 
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yucheng said:
r is not the hypothenuse of the triangle
Looks like the hypotenuse to me.
You must have the wrong triangle.
The R is from the sphere's centre to where the tangent from P touches the sphere. It makes a right angle to that tangent, not to r.
 
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haruspex said:
Looks like the hypotenuse to me.
You must have the wrong triangle.
The R is from the sphere's centre to where the tangent from P touches the sphere. It makes a right angle to that tangent, not to r.
Oops, wrong triangle indeed. So when ##r \to R##? So it does become like figure 3 (In the second thumbnail), albeit a different orientation. Ah I see it. Thanks! But the interpretation of ##F = \pi B##?
 
yucheng said:
But the interpretation of ##F = \pi B##?
I'm not sure why it doesn't turn out to be ##F = 2\pi B##. On reaching the sphere, the sphere occupies one half of what can be seen from P, so that should be a solid angle of ##2\pi##.
Need to think about it some more.
 
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haruspex said:
I'm not sure why it doesn't turn out to be ##F = 2\pi B##. On reaching the sphere, the sphere occupies one half of what can be seen from P, so that should be a solid angle of ##2\pi##.
Need to think about it some more.
Let ##B_v## be the intensity (##\text{flux} \; \text{rad}^{-1} Hz^{-1}##)

However, the amount of radiation emitted is not isotropic. It depends on the angle from the normal of the surface (or projected surface).

$$F_v = \int B_v \cos{\theta} \, d\Omega =\int^{2\pi}_{0} \int^{ \pi}_{0} B_v \cos {\theta} \sin{\theta} \, d\theta \, d\phi = \pi B_v $$

I guess this makes sense, that F is not ##4\pi B##, nor is it ##2\pi B##
 

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