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Question: The surface temperature of the Sun is \({T_0}\) , and it is at an average distance ‘d’ from a planet...

The surface temperature of the Sun is T0{T_0} , and it is at an average distance ‘d’ from a planet. The radius of the Sun is R. What is the temperature at which the planet radiates the energy?

Explanation

Solution

In this question, we need to determine the temperature at which the planet radiates the energy such that the surface temperature of the Sun is T0{T_0} and it is ‘d’ distance away from the planet. For this, we will use the relation between the power radiated by the energy source, the temperature at which the power is radiated and surface area of the body.

Complete step by step answer:
Let, the radius of the planet be ‘r’ and the temperature at which the planet radiates energy be T1{T_1}.
The radius of the Sun is R, and the surface temperature of the Sun is T0{T_0}
Energy received by the planet is the product of the flux and the area of the surface through which the energy is radiated. Mathematically, Ereceived=ϕA{E_{received}} = \phi A where ϕ\phi is the flux and ‘A’ is the area.
Here, the flux is given as ϕ=σT14\phi = \sigma {T_1}^4 and the area is given as A=4πd2A = 4\pi {d^2} as the average distance of the planet from the Sun is ‘d’.
So, the energy received by the planet is given as:
Ereceived=ϕA Ereceived=(σT14)(4πd2)(i)  {E_{received}} = \phi A \\\ \Rightarrow{E_{received}} = \left( {\sigma {T_1}^4} \right)\left( {4\pi {d^2}} \right) - - - - (i) \\\
Similarly, the energy radiated by the planet has been given as
Eradiated=ϕA Eradiated=(σT04)(4πR2)(ii)  {E_{radiated}} = \phi A \\\ \Rightarrow{E_{radiated}} = \left( {\sigma {T_0}^4} \right)\left( {4\pi {R^2}} \right) - - - - (ii) \\\
According to the question, at Thermal Equilibrium:
Absorbed power = Radiated Power. So, Ereceived=Eradiated{E_{received}} = {E_{radiated}}
Substituting the values from the equation (i) and (ii) in the equation Ereceived=Eradiated{E_{received}} = {E_{radiated}} to determine the temperature at which the planet radiates the energy.
Ereceived=Eradiated (σT14)(4πd2)=(σT04)(4πR2) T14d2=T04R2 T14=T04R2d2 T1=T04R2d24  {E_{received}} = {E_{radiated}} \\\ \Rightarrow\left( {\sigma {T_1}^4} \right)\left( {4\pi {d^2}} \right) = \left( {\sigma {T_0}^4} \right)\left( {4\pi {R^2}} \right) \\\ \Rightarrow{T_1}^4{d^2} = {T_0}^4{R^2} \\\ \Rightarrow{T_1}^4 = \dfrac{{{T_0}^4{R^2}}}{{{d^2}}} \\\ \therefore{T_1} = \sqrt[4]{{\dfrac{{{T_0}^4{R^2}}}{{{d^2}}}}} \\\
Hence, the temperature at which the planet radiates the energy such that the surface temperature of the Sun is T0{T_0} and it is ‘d’ distance away from the planet is T04R2d24\sqrt[4]{{\dfrac{{{T_0}^4{R^2}}}{{{d^2}}}}}.

Note: It is interesting to note here that, at thermal equilibrium the energy (or the power) received by a body equals to the energy (or the power) radiated by the body.