Question 12.8: The spectral, hemispherical absorptivity of an opaque surfac...
The spectral, hemispherical absorptivity of an opaque surface and the spectral irradiation at the surface are as shown.
How does the spectral, hemispherical reflectivity vary with wavelength? What is the total, hemispherical absorptivity of the surface? If the surface is initially at 500 K and has a total, hemispherical emissivity of 0.8, how will its temperature change upon exposure to the irradiation?

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Known: Spectral, hemispherical absorptivity and irradiation of a surface. Surface temperature (500 K) and total, hemispherical emissivity (0.8).
Find:
1. Spectral distribution of reflectivity.
2. Total, hemispherical absorptivity.
3. Nature of surface temperature change.
Schematic:
Assumptions:
1. Surface is opaque.
2. Surface convection effects are negligible.
3. Back surface is insulated.
Analysis:
1. From Equation 12.63, ρ_{λ} = 1 – α_{λ}. Hence from knowledge of α_{λ}(λ), the spectral distribution of ρ_{λ} is as shown.
α_{λ} + ρ_{λ} = 1 (12.63)
2. From Equations 12.51 and 12.52,
α \equiv \frac{G_{abs}}{G} (12.51)
α = \frac{\int_{0}^{∞}{α_{λ}(λ)G_{λ}(λ)} dλ}{\int_{0}^{∞}{G_{λ}(λ)} dλ} (12.52)
α = \frac{G_{abs}}{G} = \frac{\int_{0}^{∞}{α_{λ}G_{λ}} dλ}{\int_{0}^{∞}{G_{λ}} dλ}
or, subdividing the integral into parts,
α = \frac{0.2\int_{2}^{6}{G_{λ}} dλ + 500 \int_{6}^{8}{α_{λ}} dλ + 1.0 \int_{8}^{16}{G_{λ}} dλ}{\int_{2}^{6}{G_{λ}} dλ + \int_{6}^{12}{G_{λ}} dλ + \int_{12}^{16}{G_{λ}} dλ}
α = \left\{0.2(\frac{1}{2})500 W/m^{2} · μm (6 – 2) μm + 500 W/m^{2} · μm [0.2(8 – 6) μm + (1 – 0.2)(\frac{1}{2})(8 – 6) μm] + [1 × 500 W/m^{2} · μm (12 – 8) μm + 1(\frac{1}{2})500 W/m^{2} · μm (16 – 12) μm]\right\} ÷ [(\frac{1}{2})500 W/m^{2} · μm (6 – 2) μm + 500 W/m^{2} · μm (12 – 6) μm + (\frac{1}{2})500 W/m^{2} · μm (16 – 12) μm]
Hence
α = \frac{G_{abs}}{G} = \frac{(200 + 600 + 3000) W/m^{2}}{(1000 + 3000 + 1000) W/m^{2}} = \frac{3800 W/m^{2}}{5000 W/m^{2}} = 0.76
3. Neglecting convection effects, the net heat flux to the surface is
q''_{net} = αG – E = αG – εσT^{4}
Hence
q''_{net} = 0.76(5000 W/m^{2}) – 0.8 × 5.67 × 10^{-8} W/m^{2} · K^{4} (500 K)^{4}\\ q''_{net} = 3800 – 2835 = 965 W/m^{2}
Since q''_{net} > 0, the surface temperature will increase with time.

