International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Vol XXXV, Part Bl. Istanbul 2004
measured, since real measurements involve finite extension
intervals (resolution) of the concerned geometrical parameters.
Figure 2. Diagram of the measurement geometry for BRDF.
The origin of the coordinate system is the point at which the
central ray of the collimated irradiance E strikes the sample
surface at angle (9;,9;) with o; «n . The z axis is normal to
the sample surface, and the y axis lies in the plane defined by z
and £. The viewing direction is given by (9,,9,) and dO, is
the solid angle subtended by the receiver.
A common simplification of the BRDF is to assume the
concerned reflector as a Lambertian (perfectly diffuser) surface,
i.c. an infinite ideal surface for which the reflected radiance is
isotropic with the same value for all directions (9,,6,)
regardless of how it is irradiated. Therefore, Lambertian
surfaces constitute a restricted ensemble of reflectors, which are
included in the more general class of natural surfaces.
However, it is possible to define another class of reflectors
whose bi-directional reflectance distribution function
P sape (.9;,0;,9,,0,) is assumed to be a separable function
P sapi: 0,9;,0;,9,,0,) & po ()^(9;,0;,9,,0,). If we impose
according to the definition of reflected irradiance that:
| 1,.4,.9,.0, )cos9 dO, ox
(3)
21,
then, we obtain an additional definition of albedo p, (A):
[Paror 0.9,.9,.9, 4.20059, d0,
27%, (4)
5 pol) =
A relevant trouble to execute BRDF measurements is the
necessity to perform a reference measurement over a white
standard, for instance a sample of Barium Sulphate or a
Spectralon tile, for any used illumination and viewing geometry.
The standard experimental procedure would produce a wrong
or (2.8, ‚6, )= AySOA)LO Op Lor (1.8.6 $, b,)cosS,AQ, (5)
334
result since the angular behavior of the investigated sample
should be normalized to that of the employed reference, which
has its own angular dependence.
In order to avoid mixing of angular properties of reference and
target, the reference measurement has always been executed
with the same geometry, namely 9, =0° (indicated as 9, ) for
the illumination angle and 9, = 45° (indicated as S, ) for the
viewing angle, in the hypothesis to get the spectral
measurements in the principal plane, ie. $69 —6,-180'.
Utilising a collimated radiation source emitting the directional
radiance L,(A), it is easy to demonstrate that the flux
'^(1.9.,0,) reflected by the reference plate into the
direction (9,,0,) is:
with AQ, - [os9,40, . For a measurement executed with a
Q,
generic target we obtain a similar expression for the reflected
flux. The target-to-reference ratio fluxes. p,,, (1,99,0,9,.0,)
obeys the following expression:
PI (X) M (9, .00:9,,0,) cos9, 49,
Pa, 0,99.049,.0,) 7 DENT (6)
pA (X) ^" ($,,0,,9,,0,) cos9, AQ,
During our measurements the white reference plate always was
observed at a fixed geometry, and its outcome was employed to
normalize any target measurement as stated in Eq.6. We point
out that as an effect of ratio the instrument's sensitivity S(A) is
cancelled from the retrieved signal p,,,(1,9,,0,9,,0,) from
which we can deduce the complete target BRDF as explained in
the following. Under the discussed experimental set-up the
goniometric head allows a relative measurement of the bi-
directional reflectance function. The measured reflectance
Spectrum Pac (4.,95,09,9,,0,) can be expressed as the product
of a constant «& , which takes into account the directional
properties of the reference standard, and the target
Parpr (4,90.00,9,,H,) bi-directional reflectance distribution
function.
P4: 0599,0,9,.0,) 2 ap," (07 (84,9¢.9,,0,)cos8, (7)
In order to determine the unknown coefficient @ we have
executed a target measurement of directional-hemispherical
reflectance 077, (4,9,,0,,21,) with a Perkin Elmer Lambda
hem
19 double-monochromator, which operates from ultraviolet
(UV) to short-wave infrared (SWIR), using a deuterium lamp
(UV range) and a tungsten-halogen lamp (VIS-NIR and SWIR
ranges) as radiation sources. Then, integrating numerically Eq.7
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