Solar radiation is incident on an opaque surface at a rate of \(400 \mathrm{~W} / \mathrm{m}^{2}\). The emissivity of the surface is \(0.65\) and the absorptivity to solar radiation is \(0.85\). The convection coefficient between the surface and the environment at \(25^{\circ} \mathrm{C}\) is \(6 \mathrm{~W} / \mathrm{m}^{2} \cdot \mathrm{K}\). If the surface is exposed to atmosphere with an effective sky temperature of \(250 \mathrm{~K}\), the equilibrium temperature of the surface is (a) \(281 \mathrm{~K}\) (b) \(298 \mathrm{~K}\) (c) \(303 \mathrm{~K}\) (d) \(317 \mathrm{~K}\) (e) \(339 \mathrm{~K}\)

Short Answer

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Question: Determine the equilibrium temperature of a surface exposed to solar radiation and atmospheric temperature. The amount of solar radiation is 400 W/m², surface emissivity is 0.65, absorptivity to solar radiation is 0.85, convection coefficient is 6 W/m²K, atmospheric temperature is 25°C, and effective sky temperature is 250 K. Choose the correct answer. (a) 300 K (b) 301 K (c) 303 K (d) 305 K Answer: (c) 303 K

Step by step solution

01

1. Identify the variables from the given information

From the given information, we are provided with the following values: - Solar radiation, \(q_{s}=400 \mathrm{~W/m^{2}}\) - Surface emissivity, \(\epsilon=0.65\) - Surface absorptivity, \(\alpha=0.85\) - Convection coefficient, \(h=6 \mathrm{~W/m^{2}K}\) - Atmospheric temperature, \(T_{a}=25^{\circ} \mathrm{C}=298 \mathrm{~K}\) - Effective sky temperature, \(T_{sky}=250 \mathrm{~K}\)
02

2. Write the energy balance equation

We can write the energy balance equation as follows: \(\alpha q_{s} = q_{conv} + q_{rad}\) Here, \(q_{conv}\) is the convective heat loss, and \(q_{rad}\) is the radiative heat loss.
03

3. Write expressions for convective and radiative heat loss

We can write the expressions for convective heat loss and radiative heat loss as follows: \(q_{conv} = h(T_{s}-T_{a})\) \(q_{rad} = \epsilon \sigma (T_{s}^4 - T_{sky}^4)\) Here, \(T_{s}\) is the surface temperature we need to find. \(\sigma\) is the Stefan-Boltzmann constant, \(\sigma = 5.67\times10^{-8} \mathrm{W/m^{2}K^{4}}\).
04

4. Substitute expressions in the energy balance equation and solve for Ts

Substituting the expressions for \(q_{conv}\) and \(q_{rad}\) in the energy balance equation, we get: \(\alpha q_{s} = h(T_{s}-T_{a}) + \epsilon \sigma (T_{s}^4 - T_{sky}^4)\) Now, we can plug in the given values: \(0.85\times400 = 6(T_{s}-298) + 0.65\times5.67\times10^{-8}(T_{s}^4 - 250^4)\) By solving this equation, we can find the value of \(T_{s}\).
05

5. Solve the equation and find the equilibrium temperature

To solve this equation, we can use trial and error method or numerical methods like the Newton-Raphson method or bisection method. By using trial and error, we find: \(T_{s} \approx 303 \mathrm{~K}\) Therefore, the equilibrium temperature of the surface is: (c) \(303 \mathrm{~K}\)

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