44 RADIATIVE HEAT TRANSFER
3.17 On one of those famous clear days in Central Pennsylvania (home of PennState), a solar collector is irradiated
by direct sunshine and by a diffuse atmospheric radiative flux. The magnitude of the solar flux is qsun =1000
W/m2(incident at θsun =45◦), and the effective blackbody temperature for the sky is Tsky =244 K. The
absorber plate is isothermal at 320 K and is covered with a nongray, nondiffuse material whose spectral,
directional emittance may be approximated by
ǫ′
λ(λ, θ)=ǫnλcos θ, ǫnλ=0.9, λ < 2.2µm,
0.1, λ > 2.2µm,
where ǫnλis the normal, spectral emittance. Determine the net radiative flux on the collector.
σT4
3“Z2.2µm
0
2.2µm
=2
30.9f(2.2T)+0.1(1 −f(2.2T))
ǫ(Tcoll)=1
8f(2.2×320µmK)
+1
=1