Heat Transfer (Solar Radiation)

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SUMMARY

This discussion focuses on the calculation of absorbance (alpha) in the context of solar radiation and heat transfer, particularly in relation to a homework problem involving convective heat transfer. The user has successfully calculated the convective heat transfer (Qconv) as 420 W using the formula Qconv=h*A*(T-Tambient) with parameters including an area (A) of 2 m² and ambient temperature (Tambient) of 303 K. The user seeks clarification on how to determine the absorbance of the surface, given the relationship between emissivity and absorbance as stated by Kirchhoff's law of thermal radiation, specifically under equilibrium conditions. The discussion highlights the confusion regarding the application of these principles when considering solar radiation.

PREREQUISITES
  • Understanding of Kirchhoff's law of thermal radiation
  • Familiarity with convective heat transfer equations
  • Knowledge of the Stefan-Boltzmann constant
  • Basic principles of solar radiation and heat balance
NEXT STEPS
  • Research the calculation of solar absorbance using the Stefan-Boltzmann law
  • Explore the relationship between emissivity and absorbance in non-equilibrium conditions
  • Study the effects of surface temperature on heat transfer in solar applications
  • Learn about the convection heat transfer coefficient (h) and its determination
USEFUL FOR

Students studying thermodynamics, engineers working with solar energy systems, and anyone involved in heat transfer analysis in thermal systems.

Chibus
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Homework Statement



This questions relates to solar radiation and heat balance. I'm having trouble with part (b) of the question, having solved (a) already.

The question is found in the following image:

xogvvb.jpg


Homework Equations





The Attempt at a Solution



Qconv=h*A*(T-Tambient)=420 W

Qconv=420 W
A=2m^2
Tambient=303 K

Given T=(The equation found in the link)^(1/4)

Emissivity=0.9
Ne=0.15
Gsn=1000 W/m^2
Aplate=2m^2
Stefan-Boltzmann Constant=5.7E-8

The only thing I need is the abosrbance (alpha) of the surface.

I'm really unsure of how to calculate it, given I don't have the temperature of the sun.

Can anyone shed some light?



On a related note, regarding Kirchoffs law of thermal radiation:

Emissivity=Absorbance, given equilibrium temperature.

I'm having some trouble understanding where I can use this relationship. For example, in the given problem, I know that in the instant of time being looked at, the system is in equilibrium. Thus, I can say that the emissivity of the surface is equal to the absorbivity, however, this relationship doesn't apply when I am considering radiation coming in from the sun?

The following is taken from a section of my lecture notes describing the radiation function and the solar absorbance:

i.e. I evalulate the absorbance of the surface at the temperature of the sun, but I evaluate the emissivity at the equilibrium temperature of the surface. I don't understand why this is so -

rlw8dd.png


Sorry fellas, just getting pretty confused here. Any help would be eternally appreciated.
 
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If I remember my thermodynamics properly, for a grey body \alpha = \epsilon. Which applies to any radiating surface I believe.
 
The convective heat flux (q)=h*A*(Ts-Tinf) where Ts is the surface temp(a above), Tinf is the ambient air temp. h is the convection heat transfer coefficient. A is the area. You know q, A and both T's, looks like plug-and- chug to me.
 

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