Chapter 4: Problem 25
The solar constant is the incident energy per unit of time on a unit area of a surface placed at right angles to a sunbeam just outside the earth's atmosphere. The value of the solar constant is \(1.37 \mathrm{~kW} / \mathrm{m}^{2}\). The area of a sphere with radius \(93,000,000\) miles is \(2.79 \times 10^{23} \mathrm{~m}^{2}\), and the surface area of the sun is \(6.09 \times 10^{18} \mathrm{~m}^{2}\). Assuming that the sun is a blackbody, calculate its surface temperature,
Short Answer
Step by step solution
Understand the Problem
Use the Inverse Square Law
Calculate the Total Power Output of the Sun
Use the Stefan-Boltzmann Law
Rearrange to Solve for the Temperature
Calculate the Temperature
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Key Concepts
These are the key concepts you need to understand to accurately answer the question.
Stefan-Boltzmann Law
\[ P = \text{A} \times \text{σ} \times T^4 \]
where:
- P = Total power emitted (W)
- A = Surface area of the blackbody (m^2)
- σ = Stefan-Boltzmann constant = 5.67 × 10^{-8} \frac{\text{W}}{\text{m}^2 \text{K}^4}
- T = Absolute temperature (K)
Blackbody Radiation
- A blackbody in thermal equilibrium emits radiation with a spectrum that only depends on its temperature.
- The peak wavelength of the emitted radiation shifts to shorter wavelengths as the temperature increases, a principle known as Wien's Displacement Law.
- The total energy emitted per unit area increases with the fourth power of the blackbody's temperature, as described by the Stefan-Boltzmann Law.
Inverse Square Law
\[ \text{Intensity} \backsim \frac{1}{\text{distance}^2} \]
In the context of solar radiation, it means that the intensity of solar energy reaching a unit area decreases with the square of the distance from the Sun. To find the solar constant, we can apply this law:
- The solar constant is the amount of solar energy received per unit area at a specific distance from the Sun (Earth's distance).
- The total power output from the Sun (P) can be calculated by multiplying the solar constant with the surface area of a sphere at Earth's distance from the Sun: \[ \text{P} = \text{SC} \times \text{A}_\text{EARTH} \]
Surface Temperature Calculation
- First, use the Inverse Square Law to find the total power output of the Sun (P): \[ \text{P} = \text{SC} \times \text{A}_\text{EARTH} \]
- Next, use the Stefan-Boltzmann Law to relate this power to the surface temperature (T): \[ \text{P} = \text{A}_\text{SUN} \times \text{σ} \times T^4 \]
- Rearrange the formula to solve for T: \[ T = \bigg(\frac{\text{P}}{\text{A}_\text{SUN} \times \text{σ}}\bigg)^{\frac{1}{4}} \]
- Substitute the known values to find the surface temperature: \[ T = \bigg(\frac{3.82 \times 10^{26}}{6.09 \times 10^{18} \times 5.67 \times 10^{-8}}\bigg)^{\frac{1}{4}} \]
- This simplifies further to: \[ T \to 5,777 \text{K} \]
Substitute the known values:
\[ \text{P} = 1.37 \times 10^3 \frac{\text{kW}}{\text{m}^2} \times 2.79 \times 10^{23} \text{ m}^2 = 3.82 \times 10^{26} \text{ W} \]