Rochester Institute of Technology
RIT Scholar Works
Theses
Thesis/Dissertation Collections
12-1-1990
Comparison of methods for generation of absolute
reflectance factor measurements for BRDF studies
Xiaofan Feng
Follow this and additional works at:
http://scholarworks.rit.edu/theses
This Thesis is brought to you for free and open access by the Thesis/Dissertation Collections at RIT Scholar Works. It has been accepted for inclusion
in Theses by an authorized administrator of RIT Scholar Works. For more information, please contact
ritscholarworks@rit.edu.
Recommended Citation
COMPARISON OF METHODS FOR GENERATION OF
ABSOLUTE REFLECTANCE FACTOR
MEASUREMENTS FOR BRDF STUDIES
by
Xiaofan Feng
A thesis submitted
in
partial fulfillment of the
requirements for the degree of Master of Science
in the Center for Imaging Science in the
College of Graphic Arts and Photography at the
Rochester Institute of Technology
December 1990
Signature of the Author
_
Accepted by
N_am_e_Il_l_e....:::g_ib_l_e
_
Center for Imaging Science
College of Graphic Arts and Photography
Rochester Institute of Technology
Rochester, New York
CERTIFICATE OF APPROVAL
M.S. DEGREE THESIS
The M.S. degree thesis of Xiaofan Feng
has been examined and approved by the thesis
committee as satisfactory for the thesis requirement
for the Master of Science degree
Dr.
John
R.
Schott, Thesis Advisor
Dr. Mark D. Fairchild
Dr.
Mehdi Vaez-Iravani
Title of Thesis:
Center for Imaging Science
College of Graphic Arts and Photography
Rochester Institute of Technology
Rochester, New York
THESIS RELEASE PERMISSION FORM
Comparison of Methods for Generation of Absolute
Reflectance Factor Measurement for BRDF Studies
I,
Xiaofan Feng grant permission to the Wallace Memorial Library of the
Rochester Institute of Technology to reproduce this thesis
in whole or in part provided any reproduction will not
be of commercial use or for profit.
Xiaofan Feng
COMPARISON OF METHODS
FOR
GENERATION
OF
ABSOLUTE
REFLECTANCE FACTOR
MEASUREMENTS FOR
BRDF
STUDIES
by
Xiaofan
Feng
Submitted
to theCenter for
Imaging
Science
in
partial
fulfillment
oftherequirementsfor
theMaster
ofScience
degree
attheRochester Institute
ofTechnology
Abstract
For
remotesensing
applications,
thereis
a needfor knowledge concerning
thereflectanceproperties of natural and man-made materials as a
function
of measurementgeometry
andwavelength.
This information
is
used todetermine
theso-calledbidirectional
reflectancedistribution function (BRDF).
This
study
is
intended
to generate an absolutebidirectional
reflectance
factor for
BRDF
studies.This
is
accomplishedby
development
of a goniospectroradiometer which can simulateany
source-sensor-target geometry.The
spectralrange
is
from
visible tonear-infrared (2500
nm)
with a spectralresolution of10
nm.The
study
involves
both
theoreticalandexperimental workfor
calibration ofBRDF by:
(1)
thedirectional hemispherical
reflectanceand(2)
aNIST
calibrated standard reflectancetile.A
PTFE
sampleis
calibratedusing both
methods,
and a comparison testwas conducted toverify
the accuracy.This PTFE
sample canbe
used as a reference standard material totransfer reflectance
factor
scale to all source-target-sensor geometriesin
the visible andACKNOWLEDGEMENTS
This
workcould nothave been
completed withoutthesupport ofmany
people.I
wouldfirst like
tothankallthepeoplein
theDigital
Imaging
andRemote
Sensing Laboratory
(DIRS)
for
their assistancein
thevarious stages ofthisproject.I
wouldalsolike
to thankmy
committee membersfor
theirassistance:to
Dr. John
Schott,
for
theoverallguidance, patience,
andtranslating
this thesisinto
English;
to
Dr. Mark
Fairchild,
for his
timeandfor providing
mewiththevaluableinformation
aboutthe
Musell Color Science
Laboratory
gonio-spectrophotometer,
andto
Dr. Mehdi
Vaez-Iravani,
for his
encouragement.DEDICATION
This
workis
dedicated
tomy
family.
To my
parentsanduncleXingHua,
for
instilling
my desire
tolearn;
To my
mother-in-law,for her
babysitting;
and
especially
to
Table
of
Contents
List
of
Figures
List
of
Tables
1
Introduction
1
1.1
Background Review
2
1
.2BRDF Definition
1 1
1
.3Problem Related
to
BRDF Measurement
13
1.3.1 The Amount
of
Data Generated
13
1
.3.2Unavalability
of
Standard
13
1
.3.3Low
Signal Level
15
1.4
Situation
Involving
BRDF Measurement
15
1.5
Radiometry
of
the
Measurement
17
1.5.1
Measurement
Geometry
18
1.5.2
Radiant Flux Transfer
from
Source
to the
Sample
19
1.5.3
Radiant Flux Transfer from
Sample
to the
Collecting
Optics
20
1
.6Polarization
21
2
Measurement
2.1 Instrumentation
24
2.1.1
The Source Unit
24
2.1
.2Goniometer
25
2.1.3
The
Detection
System
26
2.1
.4The Computer System
30
2.1
.5Alignment
31
2.1.6
Characterization
32
2.2 BRDF Calibration
Using
Integration
Method
38
2.2.1
Directional
properties of
Reflection
40
2.2.2 Calibration
42
2.2.3 Measurement
of
BRDF
at
Illumination
angles
2.2.4 Error
Analysis
49
2.3 Calibration
of
BRDF
Instrument
Using
NIST Standard
2.3.1 Derivation
54
2.3.2
Measurement
of
the
BRDF
of
the
Standard
at
Angles
not
Provided
by
NIST
61
2.3.3
Generation
of
Absolute BRDF
Using
NIST
Standard
62
2.3.4
Error
Analysis
65
2.4
Verification
of
Accuracy
by
Independent
Determinations
of
BRDF
Using
Two Methods
67
3
Bidirectional
Reflectance
Properties
of
Materials
3.1
Measurement Equation
70
3.2
Error Analysis
71
3.3
Measurement Results
and
Discussion
3.3.1
The BRDF
of
Spectralon
75
3.3.2
The BRDF
of
Silicon Wafer
86
3.3.3
The BRDF
of
Sandpaper
96
3.3.4
The BRDF
of
Roofing
Material
103
4
Conclusions
and
Recommendation
4.1
Conclusions
105
4.2
Recommendations
4.2.1
Instrumentation
106
4.2.2 Calibration
106
4.2.3 Further Studies
107
6
Reference
108
Appendix I
Computer Program for BRDF
Measurement
and
Calibration
List
of
Figures
Figu
Figu
Figu
Figu
Figu
Figu
Figu
Figu
Figu
Figu
Figu
Figu
Figu
Figu
Figu
Figu
Figu
Figu
Figu
Figu
Figu
Figu
Figu
Figu
Figu
Figu
Figu
Figu
Figu
Figu
Figu
Figu
e
1
Beam
andSample
Geometry
1
2
e
2
Schematic
ofMeasurement
Geometry
1
9
e
3
BRDF
Instrument Schematic
26
e
4
Photo
ofBRDF
Instrument
2
7
e
5
Optical
Components
in
the
Sensor
System
2
8
e
6
Computer
Control
Diagram
3 0
e
7
Power
Supply Stability
Check
3
2
e
8
System
Stability
Check
3 3
e
9
Schematic
for
source
Polarization
Sensitivity
Measurement
3 3
e
10
Schematic
Setup
for B
Measurement
3 6
e
11
Illumination
Beam
Uniformity
37
e
12
Transformation
ofAngular
Coordinates
4 3
e
13
BRDF
ofSpectralon
(s-Polarization)
4
6
e14
BRDF
ofSpectralon
(p-Polarization)
47
e
15
BRDF Error
as a
Function
ofIncidence Angle
53
e
16
The 0/45 Reflectance Factor
asa
Function
ofWavelength
6 8
e
17
The Reflectance Factor
Differences
Between
the
Two Methods
6
9
e
18
Error Due
to
0.2
nmWavelength Offset
7 2
e
19
Error Due
to the
Position Error in
Viewing
74
e
20
Error Due
to
the
Position
Error in
Illumination
74
e
22
8/Hemispherical
Reflectance
Factor
7
6
e22
BRDF
ofSpectralon
at
0
Degree Illumination Angle
7 7
e
23
Comparison Between
the
Spectralon
and
Halon
7 7
e24
BRDF
ofHalon
withDifference Preparations
7
9
e25
Pressed PTFE Powder Reflectance
as aFunction
ofPowder
Density
7 9
e
26
Third Order Polynomial Fit
ofthe
Reflectance
ofSpectralon
80
Figure 33
Figure 34
Figure 35
Figure 36
Figure
37
Figure 38
Figure 39
Figure 40
Figure 41
Figure
42
Figure 43
The
Microscopic
Photo
ofthe
Silicon
Wafer
8 6
Spectral
BRDF
ofSilicon Wafer
at
Different
Illumination
Angles
88
Spectral
BRDF
ofSilicon Wafer
at
Different View Angles 8 8
Spectral
BRDF
ofSilicon Wafer
at
Different
Sample
Orientations
88
Measurement
Geometry
8 9
Measure
Geometry
for
Different Sample Orientations
8 9
BRDF
ofSilicon Wafer
at
Illumination Angle=0
91
BRDF
ofSilicon Wafer
at
Illumination Angle=30
91
BRDF
ofSilicon Wafer
at
Illumination Angle=45
9
2
BRDF
ofSilicon Wafer
atIllumination Angle=60
9
2
BRDF
ofSilicon Wafer
at
Illumination Angle=0
(1020
nm and1050 nm)
9 3
Figure
44
3-D
Plots
ofBRDF
ofSilicon
Wafer
atDifferent
Wavelengths
94
Figure 45
The Microscopic Photos
ofSandpapers
9 5
Figure 46
BRDF
ofSandpaper
atIllumination Angle
of0
degree
9 6
Figure 47
BRDF
ofSandpaper
atIllumination Angle
of30
degrees
9 6
Figure 48
BRDF
ofSandpaper
atIllumination
Angle
of45
degrees
9 7
Figure 49
BRDF
ofSandpaper
atIllumination Angle
of60 degrees
9
7
Figure 50
The Cross Section
ofthe
Sandpaper
9 8
Figure
51
BRDF
ofSphere Particles
9 9
Figure
52
3-D
Plots
ofBRDF
ofSandpaper
101
Figure 53
BRDF
ofRoofing
Material
atIllumination
Angle
of0 degree
103
Figure 54
BRDF
ofRoofing
Material
atIllumination
Angle
of30 degrees
1
03
Figure 55
BRDF
ofRoofing
Material
atIllumination
Angle
of60 degrees
103
List
ofTables
Table
1
Source
Polarization
Sensitivity
Measurements
34
I.
Introduction
During
the
last decade
orso,
remote
sensing
ofland
surfaceshas
been
widely
usedfor
collecting
information
about
agriculture,
hydrology,
geology,
military
intelligence,
etc,
and
its
importance
is
likely
to
increase
in
the
future
as
more
powerfulremote
sensing
instruments
andbetter
analysis
tools
become
available.In
remotesensing,
the
electromagneticenergy from
the
Sun is
reflectedby
the
earth andmeasured
by
the
sensor system onboardthe
satellite
or aircraft.The
reflective properties of materialcarry
the
signature ofthe
materialsto
be
sensed andthus
are essentialfor
the
understanding
of remote sensing.The
directional
reflectance of natural and man made surfaces changesdramatically
as afunction
of source-sensor geometry.Common
backgrounds
like
soil and vegetation canvary
in
their
reflectancefactor
by
100
to
400% for
view anglesranging from
nadirto
75
degrees
off nadir(Deering,
19881
13]).
These
data
clearly
demonstrate
the
needfor
consideration of
directional
reflectanceproperties,
evenin
materialsnormally
thought
of ashaving
relatively
wellbehaved
directional
reflectance properties.Measurements
by
Deeringt13]
1988,
Kriebel
1978[22],
and others[2i][5]have clearly
pointed outthe
needto
characterizethe
directional
reflectance of scene objects.Directional
reflectance
data
will
be
necessary
for
material(target)
identification
studies,
scene
classification,
target-to-background
prediction andbecome
increasingly
criticalin
higher
level
analysis ofremotely
senseddata
to
assessthe
metal,
condition
of vegetation).The directional
reflectance
properties arealso essential
for
someradiometric
calibration
techniques
like
the
multiple view angle method^] where
reflectance
data
are usedto
back
out
the
radiantenergy
ontothe
scene.In
orderto
build
adata
base
ofdirectional
data
as atool
in
image
analysis
andto
model phenomenaassociated with
directional
imaging,
laboratory
instrumentation
andcalibration are needed
to
reduce
the
field
collection requirements andto
provide more accurate
data
setsthan
wouldtypically
be
availablefrom
field
data.
This study is intended
to
generate an absolute reflectancefactor for BRDF
studies.
This
is
accomplishedby
development
of agoniospectro-radiometer which can simulate
any
source-sensor-target geometry.The
study
involves
both
theoretical
and experimental workfor
calibration ofBRDF
by:
(1)
the
directional
hemispherical
reflectance and(2)
a standardtile
calibratedby
the
National
Institute
ofStandards
andTechnology
(NIST).
The
primary
goal ofthis
study is
to
develop
anddemonstrate
a
device
and a method capable ofdefining
aworking
standardfor
BRDF
measurement.
The secondary
goalis
to
measureBRDF
characteristics ofsome materials.
1.1
Background
Review
The
bidirectional
reflectancedistribution
function
(BRDF)
is
the
family
ofcurves or
the
data
set associated with measurement ofthe
directional
throughout
the
hemisphere
above
the
sample.
The
spectralBRDF implies
that the
BRDF data
areavailable
as
afunction
of wavelength.The
early
drive
for
reflectance
standards
came
from
industries
wherephotometric or
colorimetric
procedures
were part ofmanufacturing
orinspection
processesDo].A
reference
standard
wasnecessary in
orderto
provide
consistency
ofmeasurement
among
different
companies,
or evendifferent
countries.The
benefit
wastighter
tolerances
on products andbetter
control of quality.Later,
withimproved
instrument
arising
from
the
use ofphotoelectric
methods
displacing
visualmethods,
more accurateand
reproducible
standards
were
needed.
In
1931,
majorrecommendations
by
CIE1[9]
introduced
the
adoption offreshly
smoked magnesium oxide asthe
primary
standardfor
reflectionmeasurements.
Conditions
of measurement were specifiedby
using
three
preferred
geometries!9]:0Q/450,
oo/total
and0/diffuse,
and
the
reflectance
factor
in
any
instrument
wastaken
asunity
for
smoked
magnesium oxide
in
orderto
permit
instruments
to
have
a
calibrated
scale of reflection.Also
during
that
time,
McNicholas[23]
atthe
National Bureau
of
Standards(NBS)
developed
the
first
goniospectrophotometer.Smoked
magnesium oxide servedfor
about40
years asthe
primary
standard of reflection.
Meanwhile,
Clark
et al[8]
(1953)
described
whatthey
called a goniometric spectrophotometer which shared some physicalsimilarities
withMcNicholas
design.
The
illumination
wasmonochromatic
and
provision
was madefor
rotation
ofthe
sample
and
detector
in
the
horizontal
and vertical.The
spectralrange
was
extended
from 400
nmto
2600
nm.Increasingly
asinstrumental
measurements
became
more
precise andreproducible,
it
was realizedthat
individual
smoking
varied and wereimpermanent
evenif
carefully
handledMo].
|n
particular at shortwavelengths,
a range of variation of4%
could occur.It
was also noticedthat
short wavelengthreflectance
deteriorated
significantly
during
the
first
day
of use.Because
ofthese
difficulties,
in
1959
the
CIE
Colorimetry
Committee
proposedthe
eventual adoption of perfectreflecting
diffuser(PRD)
whichhas
three
properties:(1)
allincident
radiation
is
reflectedback
into
the
hemisphere,
(2)
the
reflected radiantintensity
distribution
obey
the
Lambert's
Cosine
Law,
and(3)
the
PRD
depolarizes
the
incident
radiation completely.Although
a perfectreflecting
diffuser
does
notexist,
it
gives a quantitative means ofdefining
directional
reflectance.Afterwards,
many
white materialslike
MgO
and
BaS04
were measured againstthe
perfect
reflecting
diffuser for
reference standards or so called
transfer
standards.In
some applications wherethe
geometriesdo
notcomply
withthe
CIE
recommended
geometries,
laboratory
instruments
mustbe
used.Branderberg
andNeu[6]
(1965)
described
a
instrument
to
measure
absolute
bidirectional
reflectance of someengineering
materialsfor
refinedheat
transfer
calculation.The instrument
was capable ofmeasuring
BRDF
overthe
visible spectrum.Narrow
band
filters
were usedto
determine
the
continuously
overthe
polarangle
from
10
to
870,
the
azimuth angle ofthe
source
couldbe
variedby
turning
the
sample
aroundits
normal.The
detector
positioncould
be
variedcontinuously
over azimuthal angle andpolar angle.
The
sample
is
smallerthan
the
cross
section ofboth
the
incident flux
and
the
field
of view ofthe
detector.
In
orderto
getthe
absolute
reflectance
factor,
the
directional/hemispherical
reflectancewas
measured
to
calibrate
the
BRDF.
The
overallaccuracy
is 6%
atthe
normal view condition.
As
the
angle ofillumination
increases,
the
erroris
expected
to
increase.
Clarke
et alMO](1983)
described
the
NPL
goniophotometer which usedstandard 0/45
reflectance
to
calibratethe
reflectance at nonstandardgeometries.
In
particularthis
instrument
usedtwo
polarizersto
correctthe
polarizationeffect
ofthe
sample.The
angulardistribution
ofthe
luminance
factor
wasdetermined
for
all planes of polarization statesfor
nine
types
of whitematerials,
andit
is
surprising
to
find
that
strongly
diffusing
matt surfacesfail
significantly
to
fully
depolarize
the
incident
light.
All
the
instruments
described
aboveemploy
a singledetector,
thus
in
order
to
make spectralmeasurements,
either monochromaticlight
orbandpass
filters
mustbe
used.The
Munsell
Color
Science
Laboratory
(MCSL)
(Daoust
1987M2],
Fairchild
andDaoust
1988(15])
goniospectrophotometer used a
256
channeldiode array
radiometer.This
modification converted
the
instrument
from
ascanning
spectrophotometer
which requires
5
minutes/trialto
anarray device
whichcould
provide
the
This
reduction
in
measurement
time
wasnecessary
to
facilitate
a
complete
characterization ofa
material.
Four
polarization combinationswere measured at each
angular
combination,
and aNIST
tile
was usedto
calibrate
the
instrument.
Pressed
polytetrafluoroethylene(PTFE)
powder2,
pressedBaS04
andRussian Opal
glass were evaluated as possiblereflection
standards
for
goniospectrophotometry.
The
data
was sufficientto
define
the
in-plane
bidirectional
reflectance
factors
for
useas
atransfer
standard
for
nonstandard
instrumental
geometries.Before
the
1970's,
most
BRDF
measurements
werefor
photometric orcolorimetric purposes.
The
applications ofBRDF
in
remotesensing
arerelatively
new.1978
K.
T.
Kriebel[22]
measured spectralbidirectional
reflection properties of
four
vegetated surfaces at seven wavelengthsbetween
430
nm and2200
nm.The
measurements ofthe
reflectedradiation were
taken
by
means of an airborne eight-channelscanning
radiometer.
The
reflectance values weredetermined
from
measuredvalues of reflected radiance and
from
the
actualirradiance
derived
from
measured values of
the
opticaldepth
ofthe
atmosphere.The
results showthat
reflectance of vegetated surfacesis
notisotropic.
For
allsurfaces,
the
anisotropy
(ratio
ofthe
highest
to
the
lowest
reflectancevalue)
increases
withincreasing
zenith angle ofthe
incident
flux
from
about afactor
of3
to
abouta
factor
of10
or more.Kimes
andKirchner[2i]
(1982)
presented atechnique
for
determining
the
2
The
pressedPTFE
is
frequently
referredto
ashalon
orSpectralon.
In
this
thesis,
halon
is
usedfor
pressedPTFE
andSpectralon is
usedfor
error
in
diurnal
irradiance
measurements
that
resulted
from
the
non-Lambertian
behavior
ofa
reference
panel
under variousirradiance
conditions.
The
relative
biconical
reflectance
factors
of aspray
paintedbarium
sulfate panelwere
measured
using
a goniophotometerin
two
wavelength
bands
(0.63-0.60
^m and0.76-0.90
|im).It
wasfound
that
atnadir view
condition,
the
relative
reflectance
valuechanges
from
1
atthe
zenith angle of 15
to
0.7
at
the
zenithangle
of75.
These
data,
along
with simulated
sky
radiancedata
for
clear andhazy
skies at six solarzenith
angles,
were usedto
calculate
the
estimated
panelirradiances
and
true
irradiances for
anadir-looking
sensor.The inherent
errorsdue
to
the
Lambertian
assumption ofthe
panelin
total
spectralirradiance
at0.68
|imfor
a clearsky
were0.6, 6.0,
13.0
and27.0% for
solar zenith angles of0,
45,
600,
and750.
Francois
Becker
et
al[3]
(1985)
described
a
method
ofmeasuring
angularvariation of
the
bidirectional
reflectance(BDR)
ofbare
soilsin
the
thermal
infrared band
(TIR).
The
goniometerhas
an angular resolution of0.5
degree,
andboth
illumination
and observation can reachany direction
in
the
whole upwardhemisphere.
Modulated
source andsynchronous
detection
were employedto
provide a signalfree
from
thermal
emissionof
the
sample and environment.The
absolute calibration ofBDR
is very
difficult
in
TIR
because
there
is
no
good standarddiffuse
reflector.
The
calibration was avoided
by
normalizing
the
data for
each spectraldomain
with respectto
the
particular values ofthe
BDR
ofthe
sand specimenat
0o
viewing
condition.Once
againthe
experiment reveals greatvariability
Jackson
et al[20]
described
a
procedure
by
which a reference panel canbe
calibrated withthe
Sun
as
the
irradiance
source.The
directional
hemispherical
reflectance
factor
ofpressed
PTFE
was usedto
calibratethe
absolutebidirectional
reflectance
factor.
The accuracy
ofthis
method was estimated onthe
order of1%.
The
reflectance
factor
values ofPTFE
andBaS04
panels
weremeasured
at
nadir view condition withthe
Sun
at 15-750 zenith angles.The
data
indicate
that
reflectancefactors
for
panels constructedby
the
same person atthe
sametime
may
differ,
andthe
reflectancecharacteristics
of a panel will change with use.The
results presentedin
that
reportdemonstrate
the
needfor
careful panel calibration.However,
the
field
method requires clear skies and constant atmospheric conditionsduring
the
measurementperiod,
andthe
illumination
and measurementgeometry
can notbe
held
to
very
high
accuracies.Due
to
these
difficulties,
a
methodfor
laboratory
calibration offield
reflectancepanels
was presentedby
the
sameauthors
(Biggar
et al[5],
1988).
A
halogen
lamp
was usedinstead
ofthe
Sun
asthe
source.The
calibration procedure wasthe
same asthat
ofthe
field
method.The
PTFE
andBaS04
panels were measured atthe
wavelengthbetween
0.45
and0.85
|im.These
reflectance
factor
values were comparedto
those
measuredby
the
field
method,
andthe
results agreeto
within0.013
in
reflectance atincidence
angles
between
15
and75
degrees.
using
the
PARABOLA
directional
field
radiometer
in
the
visible and nearinfrared
wavelength.The
radiometer
was
mounted
on a collapsibleboom
apparatus.
Different viewing
angles
weresimulated
by
helical
spiral scanmotion of
the
radiometer.
A
direct
beam
solar radiometer was usedto
obtain
direct beam
data
whichis
requiredfor
computations
ofdirect
andtotal
irradiant
flux
ontothe
ground.Radiometric
calibration wasperformed
for
both
instruments
so
that
absolute
BRDF
couldbe
determined.
The
result revealsthat
BRDF
ofland
covertypes
notonly have
great angular
variation,
but
also wavelengthdependency.
There
is
anothercategory
ofBRDF
measurementsusing
lasers
aslight
source.
The
advantages ofthe
laser line based
system are:(1)
high
outputpower,
(2)
high
spectralpurity,
and(3)
smalldivergence
angle ofthe
illumination
beam,
thus
making
this
technique
very
attractivefor
BRDF
studies.
Arnold
et alI1]
(1989)
reported aninstrument
usedfor
characterization of calibration standards and material properties.
Three
lasers
(0.351,
1.06
and10.6
u.m)
were employed asthe
source.Several
materials were evaluated as possible
secondary
standards.The laser line based
systemhave been extensively
usedin
measuring
the
particle size
distribution
of surfaces^].The
TMA
Technologies,
Inc
is
marketing
its
CASIScatterometeriso].
up
to
sevenlasers
canbe
employed and multiple
detectors
canbe
mounted onthe
detection
subsystem
to
speedup
the
data
correction process.The
disadvantages
of
the
laser
line
based
systemis
that
it
canonly
used
to
define
the
spectral
BRDF,
which
may
result
in
erroneouspredictions.
Despite
all oftheir
activities,
the
task
ofquantitatively
characterizing
the
BRDF
is
along
way from finished.
In
the
Council for Optical
Radiation
Measurements
(CORM)
fifth
report,
SRM
(spectral
reflectancemeasurements)
for
visibleand
near-infrared
BRDF
is
listed
asthe
priority
2
task.
The
need
for
these
kinds
ofmeasurements
is
because
"The uncertainty
ofthese
measurements
is excessively high due
to the
infancy
ofthis
type
ofmetrology
anddifficulties
in
calibrating
the
photometric
and
geometric
scale
onthe
absolute
basis,
A
need existsfor
a standard reference material
to
transfer
the
scale of reflectancefactor
at specific geometric conditions of
incidence
and collectionin
the
visibleand
infrared
regions(380
nmto
3000
nm)
ofthe
electromagneticspectrum
to
aidto
the
calibration ofthese
instruments."!11]
It
is
nodoubt
that the
work of each authorlisted has greatly
advancedthe
technique
for
BRDF
measurements,
but
there
are still somelimitations,
e.g. some of
the
instruments
employedfilter
radiometersthus
limited
the
spectral resolution and spectral
range!4!!19]!11];
somehad
limitations
ongeometry
(e.g.
in-plane
measurement!1o]
orfixed
view angle!1tit19]),
andsome
did
not
have
absolute calibration!19][2].
The
present workis
intended
to
extendthe
scope ofBRDF
measurementso
that
it
is
possible
to
characterize
the
BRDF
of material completely.The
instrument
developed
for
this
study
features:
|im with a spectral resolution of
10
nm;
2.
the
capability
to
simulateany
source-sensor-target
geometry;
3.
the
capability
to
measurematerials
withvery
low
reflectancevalues;
4.
the
capability
ofcalibrating
the
reflectance
factor
in
the
absolutescale.
The
calibration usedin
this
study
is
similarto
Branderberg
andNeu's
approach^],
but
the
measurement
geometry is different.
In
their approach,
the
sampleis
smallerthan
the
cross section ofthe
illumination
andthe
field
of view ofthe
detection
system,
thus
the
sample controlsthe
field
of view.While
in
this
instrument,
the
field
of view ofthe
detection
systemis
smallerthan
both
the
sample
andthe
illumination
beam.
This
modificationhas
two
advantages:(1)
improved
the
signallevel,
whenthe
view angleis
large,
the
increase
in
view area compensatesfor
the
Lambert
cosinefalloff
in
radiantintensity,
and(2)
improved
calibrationaccuracy.
In
their approach,
the
sample was smallerthan
the
field
of view ofthe
detection
system,
thus
the
background
radiation also contributedto
the
measuredsignal,
the
larger
the
viewangle,
the
bigger
the
background
radiation,
andthe
bigger
the
calibration error.These four features
madethis
a uniqueinstrument
capable ofdefining
the
spectral
BRDF
completely.1.2
BRDF
Definition
compared
to
the
radiant
flux
reflected
into
that
solid
angleby
a
perfectLambertian
diffuser
irradiated
in
the
same
manner whenilluminated
through
a smallsolid
angle.In
this
study,
the
bidirectional
reflectance
factor
(BRDF)
is
representedby
the
symbolB,
whichis
afunction
of6j,
ft,
9r
and<t>r.These
angles are shownin
figure
1.
All
quantities
associated
withthe
incident
flux
have
asubscript
i,
and allquantities
associated withthe
reflectedenergy
have
asubscript
r.Fig.
1
Beam
and samplegeometry
Or
Lrdcorcos6rdA
Lr
P(G.,9i; er,cpr)
=^
=Lodc0rCOs9rdA
=7^
{1
^
where
<Drand
<D0
are
the
radiant
flux
reflected
by
the
sample anda
perfectly
reflecting
diffuser,
Lr
and
L0
arethe
corresponding
radiance,
dcor
is
the
solid angle ofthe
collecting
optics,
dA is
the
sample area.1.3
Problems
Related
to
BRDF
Measurement
The
greatvariability
ofBRDF
with angulardistribution
andits
dependency
on wavelength makeit absolutely necessary
to
characterizeBRDF
notonly
at varioussource-sensor-target
geometries,
but
also atdifferent
wavelengths.Three
problemsarising
therefrom
aredescribed
below:
1.3.1
The
Amount
ofData
Generated
Ideally,
the
properties ofa
material shouldbe
understoodin
terms
ofspectral reflectance properties under all geometric
conditions
ofillumination
and viewing.For
example,
for
eachsample,
there
mightbe 5
different
illumination
angles (0to
75in
150increment),
15
viewing
angles (-750
to
750in
100increment),
9
azimuthal angles (00to
900in
100increment),
210
wavelengths centers(400
nmto
2500
nm at10
nminterval)
andtwo
polarizationstates,
sothe
total
number ofdata
points
would
be
This
huge
amount ofdata
creates
two
difficulties,
oneis
it
willtake
along
time
to
collect.A
fully
computer
controlled
instrument is
essential,
and
the
instrument
must
be
capable
ofmeasuring
over severaldays
without
any drift in
signal.
Another
difficulty
is
that
it is hard
to
presentand
to
process
the
huge
amount
ofdata
collected,
so
3-D
ploting
andmathematical
models
areneeded.
1.3.2
Lack
ofStandard
There
is
actually
noNIST
BRDF
standardpresently
existing.Most
likely
this
is because only four
geometries
arerecommended
by
CIE
(fjo/d, d/Oo,
00/450 and
450/00,
whered
standfor
diffuse)
which means calibrationstandards
areonly
providedto
matchthese
four
geometries.And
the
situation
become
worse atthe
infrared
wavelength whereonly
0/d
reflectance
data
are available.To
circumventthis
situation,
three
approacheshave
been
used.One
assumes some materials
like
BaSCU
and pressedPTFE
to
be
Lambertian,
and
the
00/45 reflectanceholds
for
all geometries.At
eachangle
combination,
the
instrument
is
standardizedto
these
materials.This
approach was proved
to
be
incorrect
in
several studies(Daoust
1987H2],
Young
1980P4]).
The
second approachis using
the
reflectance value at a standardgeometry
like
00/450to
calibratethe
BRDF
atany
othergeometry
by
carefully
characterizing
the
geometricbehavior
ofthe
instrument
whenthe
accurate
and
more
difficult.
It
requires
avery
welldesigned
and
characterized
instrument.
One
limitation
ofthis
technique
is
that
it
couldnot
apply
to
the
infrared
region
where
no
00/450
reflectance
standardis
available.
The
third
approach
is
using
the
directional/hemispherical
reflectanceto
calibrate
the
bidirectional
reflectance[2op].
a
precise
knowledge
ofthe
angular
behavior
ofthe
reflected
flux is
needed
to
performthe
integration.
The instrument
mustbe
capable
ofmeasuring
the
reflected
radiant
flux
atall possible
viewing
angles
above
the
sample.The
last
two
methods areused
in
this
study.1.3.3
Low
signal
level
The incident
radiationis diffused
by
the
sample
to
the
wholehemisphere.
In
orderto
keep
the
measurement
accuracy,
the
solid angle ofthe
receiving
opticsis
small,
thus
only
a small portion ofthe
radiant
flux
reflected reaches
the
radiometer entrance slit andthe
signalis
againattenuated
by
the
monochromatorin
orderto
measure spectralBRDF.
So
the
total
throughput
is
very
low
by
the
nature ofthis
kind
ofmeasurement.
The
situationbecome
worse whenmeasuring
low
reflectance material
like
asphalt whichhas only
about2%
reflectance.
So
a well
designed
illumination
system and a sensitivedetection
system
are
absolutely
required.In
the
field
ofradiometry,
the
bidirectional
reflectancedistribution
factor
is
a
fundamental
term,
many
other radiometricterms
canbe
derived from
it.
A
selection
ofthese
are
represented
here
to
stressthe
importance
ofBRDF
measurement
in
the
world
of radiometry.(1)
Directional/hemispherical
reflectance
Suppose
the
incident
radiation
is
wellcollimated
within a small elementof solid angle
dcoj
from
direction
(9|,
$,),
the
directional/hemispherical
reflectance
pid(0j, <fo)
is
givenby
Pid(Qi>
<h)=JJ3(9j,
<t>i;er> <M
cos9r
dcor/7t
dimensionless
(1-2)
Where
B(9j,
<J>j;9r,
<|>r)
is
the
bidirectional
reflectance.If
a point onthe
surface of an opaque solidis
uniformly
irradiated
from
all external
directions
(i.e.
approximately
the
case of skylightirradiation),
the
hemispherical/directional
reflectancepdr(9r,
r)
is
givenby
pdr(9r,
<t>r)
=11B(0j,
<J>i;6r,
<\>r)
COS9j
dcOj/K
(1-3)
where
the
integration
is
overthe
hemisphere.
A
ccording
to
the
reciprocity
relationB(9j,
<t>i;er,
<t>r)
=3(9r,
<j>r:ei,
M
thus
giving
Thus
the
directional/hemispherical
reflectance
is
equalto
the
hemispherical/directional
reflectance,
actually
it
turns
outto
be
anotherreciprocal relation.
(2)
Absolute
Emissivity
orAbsorbtivity
Measurement
A
direct
determination
ofthe
emissivity
orabsorbtivity
is
very
difficult.
However,
the
Kirchhoff Law
provides alink between
passive measurementand active measurement.
According
to
Grum
I16],
Kirchhoff's
Law
is
statedas:
At
a point onthe
surface of athermal
radiator at eachtemperature
andfor
eachwavelength,
the
spectral(directional)
emissivity in
any
givendirection
is
equalto
the
spectral(directional)
absorbtancefor
radiantenergy
incident
from
the
samedirection.
This
hold
for
any
polarizedcomponent and
hence,
for
unpolarized radiantenergy
as well.That is
,for
a given
material,
the
following
equationholds.
e(k,
9,
([>)
=a(k,
9,
<J))
(1-5)
Where
e(k,
9, $)
is
the
emissivity
at(9,
$)
direction,
anda(X,
9,
<|>)
is
the
absorbtivity
of materialto
the
incident
radiantenergy
in
(9,
<j>)
direction.
According
to
energy
conservationlaw,
For
opaque mediaxx
=0
thus
Where
B(91><|)1;92,
<t>2)
is
the
absolute
bidirectional
reflectance ofthe
material,
px
is
the
directional/hemispherical
reflectance.
If
the
absolutedirectional/hemispherical
reflectance
orthe
BRDF
ofthe
material
is
known,
the
emissivity
ofmaterial
can
also
be
determined
by
the
above
equation.(3)
Helmholtz
Reciprocity
Law
Helmholtz
reciprocity
law
is
: "The
loss
in
flux
density
which aninfinitely
narrowbundle
ofrays
ofdefinite
wavelength and state ofpolarization undergoes on
its
paththrough
any
mediumby
reflection,
refraction,
absorption,
andscattering
is
exactly
equalto
the
loss
in
flux
density
sufferedby
a
bundle
ofthe
same wavelength and polarizationpursuing
anexactly
oppositepath."
This is
animportant
theorem
whichmany
authorshave
referredto
or madeuse of
in
various ways withoutgiving
aproof,
including
Helmholtz
himself[31L
Several
authorshave
questionedthe
validity
ofthe
law,
but
many
authors offer supportfor
the
law.
The
goniospectroradiometeris
1.5
Radiometry
of
the
Measurement
1.5.1
Measurement
Geometry
There
aretwo
major approachesin BRDF
measurement.
One is
keeping
the
cross section of
both
the
incident flux
andfield
of view ofthe
detector
larger
than
the
sample^].Another
approachis
keeping
the
irradiated
areaand sample
larger
than
the
area
ofthe
field
of view ofthe
detector.
The
second approach
is
chosenfor
this
study
because
it
can collect moreradiant
flux
atlarger viewing
anglesthan
the
first
approach,
the
increase
in
viewing
area compensatesfor
the
Lambert
cosinefalloff
in
radiantintensity
whenthe
viewing
angleincreases.
Figure
2
showsthe
measurement geometry.
Source
Slit
Collecting
lens-dA
er
1.5.2
Radiant
Flux
Transfer
from
Source
to
the
Sample
The
radiant
intensity
from
a
point
source
is
given
by
I
=dO/dcoi(W SM
)
(1-8)
Where do
is
the
radiant
flux into
the
solid
angle
dcoj. The irradiance
onthe
sample
is
givenby
E(9j)=l do)i/dAei=l
dcoj
cos9i/dA0=E0 cos9j
(W cm-2)
(1-9)
Where
E(9j)
is
the
irradiance
ontothe
sample
whenirradiated
at9j
from
normal,
E0
is
the
irradiance
whenirradiated
atthe normal,
dAeji is
the
areacontained
in
solid angleda>i.
This
relationship
meansthat
increasing
the
illumination
angledecreases
the
irradiance
ontothe
sample.1.5.3
Radiant
Flux
Transfer
from
Sample
to
the
Collecting
Optics
Assuming
the
irradiance
ontothe
sampleis
uniform andthe
sample
is
aperfect
reflecting
diffuser
(PRD),
the
reflected radianceis
givenby
U=E(9i)/7u=E0
cos9i/7r.(Wcm-2Sr-1)
(1-10)
According
to
Lambert's
cosinelaw,
the
reflected radiantintensity
is:
I0(9ii9r)=l0cos9r
(1-11)
Where
l0
is
the
radiantintensity
in
the
normaldirection.
According
to
the
dO0=L0
cos(O)
dcor dAer=l0 dcor
(1-12)
l0=L0
cos(O)
dAer=L0
dAer
(1-13)
Where dAer
=dA0/cos9r
is
the
areacontained
in
the
solid angle ofthe
receiving
optics when viewedin
9r
from
the
normal,
dA0
is
the
area whenviewed
in
the
normaldirection.
l0(9ii9r)=L0
cos9rdAo/cos9r=L0dA0=E0
dA0cos9i/:r
(W
Sr-1) (1-14)
Thus
the
radiantintensity
is
independent
ofviewing
angle,
the
Lambert
cosine
falloff
is
compensated
by
the
increase
in
the
viewing
area.The
radiant
flux
collectedby
the
receiving
opticsis
expressed asO0=l
dcor=E0 dA0
cos9j
dcor/7i
(W)
(1-15)
Where
dcor
is
the
solid angle subtendedby
the
collection optics.For
animperfect
sampleL(9i,<t>i;9r,^r)
=B(9i,<|>i;9r,(|)r)
L0
(116)
0(9i,<t>i;9r,(|)r)=L(9i,<|)i;9r,<j)r)
dcor
dA0
=L0B(9i,<|)i;9r,<j)r)dcor
dA0
=
E0
cos9j
B(9i,<t>i;9r,<t>r)clcordAo/TC
(W)
(1-17)
Where
E0,
dA0,
anddcor
are constants.Thus,
the
radiantflux
collectedby
the
opticsis
directly
proportionalto the
BRDF
modifiedonly
by
the
cosine
1.6
Polarization
Clarke
no] has
pointed
out
that
most
matt
finish
materials which aregenerally
treated
as anideal
diffuser
fail
greatly
to
depolarize
the
incident
radiation,
thus
unacceptable
errormay
be
introduced
into
BRDF
measurement
if
eitherthe
source
orthe
sensoris
polarization sensitive.Many
optical elements arecapable
ofinfluencing
the
state of polarizationin
instruments.
For
the
instrument
usedfor
this
study,
the
polarizationsensitivities
ofthe
elements
arediscussed below:
(A).
Source:
atungsten
filament
lamp
is
usually
slightly
polarizeddepend
on
the
configuration ofthe
filament.
For
the
frosted
halogen
lamp
usedin
this
instrument,
no significant polarization effecthave
been
observed.(B).
Lamp
with parabolic reflector: no polarization effectis
observed atthe
central region ofthe
illumination
pattern whichis
what we areinterested
in,
but
beyond
the
central regionthere
did
exist somepolarization effect
due
to
the
parabolic reflector.(C).
Mirrors:
polarizationfrom
surface reflection.(D).
Double
grating
monochromator:Major
source of polarization.The
polarization
sensitivity
is
wavelengthdependent.
(E).
Detectors:
When
radiationfalls
ontothe
detector
at normalincidence,
no polarization
is
observedfor
silicondetector
orPbS
detectors.
In
orderto
correctthe
polarization effectin
reflectancemeasurement,
two
polarizers shouldbe
usedto
measuredthe
polarized reflectance.The
two
subscripts.The
first
subscript
indicates
the
state ofthe
polarizationof
the
incident
radiation(p=polarized
parallelto
the
plane ofincidence,
s=polarized perpendicular
to
the
plane
ofincidence,
u=unpolarized).The
second
subscript
indicates
the
polarization
sensitivity
ofthe
detection
system
(p=sensitive
only
to
the
radiation parallelto
the
plane ofmeasurement,
s=sensitiveonly
to
radiation perpendicularto
the
plane ofmeasurement,
u=equally
sensitiveto
all polarizations).Buu
is
the
reflectancefactor for
unpolarized or random polarizedincident
radiation and unpolarized
detection,
whichis
always referred asthe
correct reflectance
factor.
It
canbe easily
proventhat
Buu=(l3ss+Bsp+3ps+BpP)/4
(1-18)
For
the
instrument
usedfor
this
study,
the
sourceis
unpolarized,
thus
only
the
polarization effect ofthe
sensor needbe
corrected.A
polarizeris
usedin
the
detection
beam
whichis
set either parallel or perpendicularto
the
measurement plane of
the
radiometer.The
equation above shouldbe
modified as
Buu=(Bus+Bup)/2
O-I9)
2.
Measurement
2.1
Instrumentation
The BRDF
instrument
usedfor
this
study is
composed
offour
units: abroad
band,
high
output,
very
stable
source,
a
goniometer
which can simulateany
source-sensor-target
geometry,
a
spectrometer
to
measure
the
spectralreflectance
factor,
and acomputer
systemto
controlthe
instrument
operation,
data
collection
and
data
processing.
2.1.1
The
Source
Unit
The
source
consists of a500 W frosted
tungsten
halogen
lamp
operated at120
V.
In
orderto
have
extremely
long
operating
life,
the
operating
voltage
is
about
90%
ofthe
ratedvoltage,
further
reduction ofthe
voltagemay
causethe
halogen
cycleto
ceaseto
operate andconsequently
decrease
the
life.
The frosted
lamp
envelop
waschosen,
because
(1)
it
could
improve
the
uniformity
ofillumination
whenthe
parabolic
reflectorwas
used,
(2)
it helps
to
depolarize
the
output radiation.The
lamp
is
poweredby
a precision powersupply
withless
than
0.008%
rms
voltage variation observed over a48
hour
period.The
systemmonitors
source currentand
voltageat
the
lamp
andthe
data
is
automatically
logged
by
the
computerto
verify
stability.increase
the
irradiance
atthe
sample
by
a
factor
of60
as comparedto the
bare
lamp.
This
is
essential
when
measuring
the
low
reflectancematerials,
but
in
the
procedure
to
calibrate
the
standard,
where uniformirradiation
is
moreimportant,
the
parabolic
reflector
is
removedfrom
the
sourceresulting
in
avery
good
approximation
of point sourceillumination.
While
this
modificationeffectively
generates
a uniformirradiance
field,
it
alsoreduces
the
overall signalreaching
the
sensor.However,
this
is
not a
problem sincethe
standard
has
a
very high
reflectance value.2.1.2
Goniometer
A
goniometeris
usedto
simulateany
source-sensor-target geometry.The
degrees
of motion requiredto
generate aBRDF
data
set are configured asfollows (cf. Figure 3
andfigure
4
):
1.
the
sensoris fixed because
ofthe
large
size,
2.
the
source rotates 5to
1350 relativeto
the
sensor,
wherethe
50limitation
is due
to
the
physical size ofthe source,
the
1350limitation
is
imposed
by
the
rotationstage,
3.
the
sample rotates -900to
900 aboutits primary
axis,
the
source andsample rotate
horizontally
together
whichis
equivalentto
the
sensorrotation,
4.
the
sampletilts
Oo
to
750 aboutits secondary
axisas
shownin Fig. 3.
Motion
is
achievedby
computer control of precision stepper motors.The
angular
step
canbe
controlledto
0.00250 per step.Typical
collections areTilt Axis
Data and
Spectrometer
Control
Axis ofRotation
figure 3
BRDF Instrument Schematic
The
sample stageis
an 8" platen whichis
adjustedin
andout,
depending
on
the
samplethickness,
to
ensurethat the
face
ofthe
sample
is
located
on
the
primary
axis ofthe
rotation.It is
important
to
notethat the
area
of
the
sample viewedby
the
sensorincreases
for
off axisacquisition
to
Dimlilr Cr;itin^ ,Mdnm'
llI<i mili' i
PC ( lunc
ilh 12-liil A'D Im <l:il:i
(Oil IT inn
:iltd I ml nil
DiuiCil Voltintier
2.1.3
The
detection
systemThe
sensor systemis illustrated in Figure 5.
The lens images
the
sampleonto
the
entrance
aperture
ofthe
Optronics
Spectrometer,
andthus
collects
the
reflected radiantflux.
The
signalis
then
sampledby
aSi
orPbS detector
at
the
exit
aperture
ofthe
Spectrometer.
Source
Sample
Si
orPbS
Detector
The
1"diameter,
4"focal
length
lens
is
made
of calciumfluoride
whichhas
a
broad
transmission
range
of0.13
u.mto
8.0
u,m.The
f#
of4
is
chosen
to
matchthe
f#
ofthe
Spectrometer.
The
polarizeris
a calciteGlan-Thompson
polarizing
prism(wavelength
rangefrom
350
nmto
2.3
|im,
extinctionratio
<1x10-5,
clearaperture
10x10
mm).The Model 7351 R-D Double
Grating
Monochromator
andthe
Model 736
Lock-In
amplifiercombined,
form
the
Model
746-D
Infrared
Spectrometer
system.
The basic features include:
(1).
A
monochromator withbuilt-in
chopper and mechanical wavelengthreadout of
0 to
2500
nm.(2).
A
Lock-In
Amplifier
with autoranging
preamp.(3).
Two diffraction
gratingsblazed
at0.6
firm and1.6
u.m.These
gratings,
combined with
two
detectors
(Si
andPbS),
coverthe
wavelength rangefrom 400
nmto
2500
nm,
and(4).
A
set of5
blocking
filters from 400
nmto
2500
nm are employedto
sort
the
order ofthe
diffraction
gratings.The
Spectrometer
signal outputis
modifiedto
passthrough
a12
bit A
to
D
converter
for
data
logging.
The
entrance aperture ofthe
spectrometer
defines:
(1)
the
spectralbandwidth,
and(2)
the
area ofthe target
sampled
and
the
solid angle accepted.For
the
measurement
reported
here,
the
aperture
diameter
is
3
mm,
corresponding
to
a spectralbandwidth
of10
nm,
an acceptance angle of 0.90from