Although we have focused on radiation emitted by a
surface, the foregoing concepts may be extended to incident radiation (Figure
12.9). Such radiation may originate from emission and reflection occurring at
other surfaces and will have spectral and directional distributions determined
by the spectral intensity Iλ,i (λ, θ, ϕ). This quant ity is defined
as the rate at which radiant energy of wavelength λ is incident from the (θ, ϕ)
direction, per unit area of the intercepting surface normal to this direction,
per unit solid angle about this direction, and per unit wavelength interval dλ
about λ.
The intensity of the incident radiation may be
related to an important radiative flux, termed the irradiation, which
encompasses radiation incident from all directions. The spectral irradiation Gλ
(W/m2.μm) is defined as the rate at which radiation of wavelength λ
is incident on a surface, per unit area of the surface and per unit wavelength
interval dλ about λ. Accordingly,
where sin θ dθ dϕ is the unit solid angle. The cos θ
factor originates because Gλ is a flux based on the actual surface area, where as
Iλ,i is defined in terms of the projected area. If the total
irradiation G (W/m2) represents the rate at which radiation is
incident per unit area from all directions and at all wavelengths, it follows
that
Or from equation 12.13
If the incident radiation is diffuse, Iλ,I is independent of
θ and ϕ and it follow that
And
Comments :generally, radiation sources do not
provide such a regular spectral distribution for the irradiation. However, the
procedure of computing the total irradiation from knowledge of the spectral
distribution remains the same, although evaluation of the integral is likely to
involve more detail.
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