Inconsistent Radiation Questions

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Discussion Overview

The discussion revolves around the derivation of a temperature formula for a sphere radiating to an environment that is not at zero temperature. Participants explore the implications of introducing a second, larger concentric sphere and the assumptions involved in the derivation process, including the treatment of emissivity and radiosity equations.

Discussion Character

  • Exploratory
  • Technical explanation
  • Debate/contested

Main Points Raised

  • One participant presents a formula for the temperature of a sphere with internal heat generation and discusses its derivation from radiosity equations.
  • Another participant suggests that the result follows from detailed balance for a gray body, raising the possibility of complications if the body is not gray.
  • Some participants question the assumptions made, particularly regarding the outer sphere's properties and the implications of those assumptions on the derived equations.
  • There is a suggestion that the assumptions may require the view that the view factor between the two spheres approaches zero for consistency.
  • A later reply indicates that dropping the assumption of the outer sphere being adiabatic resolves the discrepancies between the equations.

Areas of Agreement / Disagreement

Participants express differing views on the assumptions and implications of the model, particularly regarding the treatment of the outer sphere and the conditions under which the derived equations hold. The discussion remains unresolved regarding the best approach to reconcile the differing results.

Contextual Notes

Participants note limitations in their assumptions, particularly concerning the emissivity of the spheres and the nature of the outer sphere, which is described as a surface rather than a solid. The discussion highlights the need for clarity in the setup and assumptions used in the derivation.

davidwinth
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I have a formula for a sphere radiating to the environment where the environment is not at zero temperature. The sphere has a constant heat generated within itself. The formula for the temperature of the sphere under these conditions is:

##T_s = \left( \frac{Q_{gen}}{A_s \sigma \epsilon} + {T_{amb}^4} \right)^{\frac{1}{4}}##

Where ##Q_{gen}## is in Watts and the subscript s refers to the sphere while the subscript amb refers to ambient. Fine and good, but I wanted to see if I could derive this equation from a circumstance where there are two concentric spheres, the inside sphere is identical to the above sphere and the outside sphere is super large, adiabatic, and at the temperature of the ambient.

My starting point are the 4 radiosity equation in 4 unknowns given by Nellis & Klein, i.e.,

##Q_{gen1} = \frac{\epsilon_1 A_1(E_{b1} - J_1)}{1-\epsilon_1}##
##Q_{gen2} = \frac{\epsilon_2 A_2(E_{b2} - J_2)}{1-\epsilon_2}##

and

##Q_{gen1} = A_1 F_{12}(J_1- J_2)##
##Q_{gen2} = A_2 F_{21}(J_2- J_1)##

Solving the first set of equations for the radiosity gives:

##J_1 = E_{b1} - \frac{Q_{gen1} (1 - \epsilon_1)}{\epsilon_1 A_1}##
##J_2 = E_{b2} - \frac{Q_{gen2} (1 - \epsilon_2)}{\epsilon_2 A_2}##

Now plugging these into the second set of equations gives (after some algebra):

##Q_{gen1} = A_1 F_{12} \left( E_{b1} - \frac{Q_{gen1} (1 - \epsilon_1)}{\epsilon_1 A_1} - E_{b2} + \frac{Q_{gen2} (1 - \epsilon_2)}{\epsilon_2 A_2}\right)##
##Q_{gen2} = A_2 F_{21} \left( E_{b2} - \frac{Q_{gen2} (1 - \epsilon_2)}{\epsilon_2 A_2} - E_{b1} + \frac{Q_{gen1} (1 - \epsilon_1)}{\epsilon_1 A_1}\right)##

So these are general, but now I introduce the assumptions above, namely

##Q_{gen2} = 0##
##F_{12} = 1##
##F_{21} {A_2} = A_1##
##A_2 \rightarrow \infty##

The first equation results in:

##Q_{gen1}\left( \frac{1}{\epsilon_1}\right) = A_1(E_{b1} - E_{b2})##

Which is identical to my formula above. Great, that is what I was hoping would happen! But the second equation gives:

##Q_{gen1} \left( \frac{1}{\epsilon_1} -1 \right)= A_1(E_{b1} - E_{b2})##

This is not the same result. My question, what happened? Shouldn't both equations give the same values?
 
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davidwinth said:
I have a formula for a sphere radiating to the environment where the environment is not at zero temperature. The sphere has a constant heat generated within itself. The formula for the temperature of the sphere under these conditions is:

##T_s = \left( \frac{Q_{gen}}{A_s \sigma \epsilon} + {T_{amb}^4} \right)^{\frac{1}{4}}##

Where ##Q_{gen}## is in Watts and the subscript s refers to the sphere while the subscript amb refers to ambient. Fine and good, but I wanted to see if I could derive this equation from a circumstance where there are two concentric spheres, the inside sphere is identical to the above sphere and the outside sphere is super large, adiabatic, and at the temperature of the ambient.

My starting point are the 4 radiosity equation in 4 unknowns given by Nellis & Klein, i.e.,

##Q_{gen1} = \frac{\epsilon_1 A_1(E_{b1} - J_1)}{1-\epsilon_1}##
##Q_{gen2} = \frac{\epsilon_2 A_2(E_{b2} - J_2)}{1-\epsilon_2}##

and

##Q_{gen1} = A_1 F_{12}(J_1- J_2)##
##Q_{gen2} = A_2 F_{21}(J_2- J_1)##

Solving the first set of equations for the radiosity gives:

##J_1 = E_{b1} - \frac{Q_{gen1} (1 - \epsilon_1)}{\epsilon_1 A_1}##
##J_2 = E_{b2} - \frac{Q_{gen2} (1 - \epsilon_2)}{\epsilon_2 A_2}##

Now plugging these into the second set of equations gives (after some algebra):

##Q_{gen1} = A_1 F_{12} \left( E_{b1} - \frac{Q_{gen1} (1 - \epsilon_1)}{\epsilon_1 A_1} - E_{b2} + \frac{Q_{gen2} (1 - \epsilon_2)}{\epsilon_2 A_2}\right)##
##Q_{gen2} = A_2 F_{21} \left( E_{b2} - \frac{Q_{gen2} (1 - \epsilon_2)}{\epsilon_2 A_2} - E_{b1} + \frac{Q_{gen1} (1 - \epsilon_1)}{\epsilon_1 A_1}\right)##

So these are general, but now I introduce the assumptions above, namely

##Q_{gen2} = 0##
##F_{12} = 1##
##F_{21} {A_2} = A_1##
##A_2 \rightarrow \infty##

The first equation results in:

##Q_{gen1}\left( \frac{1}{\epsilon_1}\right) = A_1(E_{b1} - E_{b2})##

Which is identical to my formula above. Great, that is what I was hoping would happen! But the second equation gives:

##Q_{gen1} \left( \frac{1}{\epsilon_1} -1 \right)= A_1(E_{b1} - E_{b2})##

This is not the same result. My question, what happened? Shouldn't both equations give the same values?
I have no idea idea about the source you quote.
For a gray body with emissivity ##\epsilon## your result follows immediately from detailed balance$$ \epsilon\sigma{T_s}^4-\epsilon\sigma{T_{amb}}^4=\frac Q A_s$$
A more likely complication is that the body will not be gray in which case this would be true only for a given frequency and one would need to integrate over the spectrum at the two temperatures giving an effective value for each ##\epsilon## at Temp.
 
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hutchphd said:
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I have no idea idea about the source you quote.
For a gray body with emissivity ##\epsilon## your result follows immediately from detailed balance$$ \epsilon\sigma{T_s}^4-\epsilon\sigma{T_{amb}}^4=\frac Q A_s$$
A more likely complication is that the body will not be gray in which case this would be true only for a given frequency and one would need to integrate over the spectrum at the two temperatures giving an effective value for each ##\epsilon## at Temp.

Right, I know how to get my result for the case without an external sphere. I am wondering how to get the same result if I come at it by assuming the ambient is a sphere. I am quoting the textbook Heat Transfer by Nellis and Klein, which is a widely used textbook.
 
If the first sphere is encased in an identical larger sphere, then you just have a bigger sphere. If that is not the setup, a drawing is necessary. ( sorry I don't have Nellis at al )
 
N.B. It appears to me that your assumptions require ##F_{21}=0## for consistency. That will eliminate the pesky equation I think. Otherwise I'm shooting in the dark here!
 
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hutchphd said:
If the first sphere is encased in an identical larger sphere, then you just have a bigger sphere. If that is not the setup, a drawing is necessary. ( sorry I don't have Nellis at al )
That is a problem with my description. The outer sphere is just a surface, not a solid. There is vacuum between the outer surface of the inner sphere and the larger shell.
 
Last edited:
hutchphd said:
N.B. It appears to me that your assumptions require ##F_{21}=0## for consistency. That will eliminate the pesky equation I think. Otherwise I'm shooting in the dark here!
I would think that would be the asymptote for the outer sphere approaching infinite distance, so it does make sense to me.
 
I discovered the problem. It was the assumption of the larger sphere being adiabatic. When that assumption is dropped, both equations agree.
 
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