(a) (h)
FIG. 4-18. AbsorptioninDebye-Scherrer specimens:(a)general case, (b)highly absorbing specimen.
4-10
Absorption factor. Still another factor affecting the intensities of the diffracted raysmust
be considered,and
that is the absorptionwhich
takes place in thespecimen
itself.The specimen
in theDebye-Scherrer method
has theform
ofa verythin cylinder ofpowder
placedon
thecamera
axis,
and
Fig. 4-1 8(a)shows
the cross section of such a specimen.For
the low-angle reflectionshown,
absorption of a particular ray in the inci-dentbeam
occurs along apath
such asAB]
at5
a small fraction of the incident energy is diffractedby
apowder
particle,and
absorption of this diffractedbeam
occurs along thepath BC.
Similarly, for a high-angle reflection, absorption ofboth
the incidentand
diffractedbeams
occurs along apath
such as(DE + EF). The
net result is that the diffractedbeam
is of lower intensitythan one would
expect for aspecimen
ofno
absorption.
A
calculation ofthis effectshows
that the relative absorption increases as 6 decreases, forany
given cylindrical specimen.That
thismust
be so canbe
seenfrom
Fig. 4-1 8(b)which
applies to aspecimen
(for example, tungsten) of very high absorption.The
incidentbeam
isvery
rapidly absorbed,and most
of the diffractedbeams
originate in the thin surface layeron
the left side of thespecimen
,-fbackward-reflectedbeams then undergo very
little absorption, but forward-reflectedbeams have
to passthrough
thewhole specimen and
are greatly absorbed.^ Actually, the forward-reflectedbeams
in this casecome
almostentirelyfrom
the topand bottom
edges of the specimen.* This difference in absorptionbetween
*
The
powder patterns reproduced in Fig. 3-13show
this effect.The
lowest-anglelineineach pattern issplitin two, because thebeam
diffracted through the center of the specimen is sohighly absorbed. It is importantto keep the possi-bility of thisphenomenon
inmind when
examining Debye-Scherrer photographs, orsplitlow-anglelinesmay
beincorrectly interpreted asseparatediffraction linesfrom twodifferent setsof planes.
130
DIFFRACTION
IIITHE
INTENSITIESOF DIFFRACTED BEAMS
[CHAP. 4 high-0and
low-0 reflections decreases as the linear absorption coefficient of thespecimen
decreases,but
the absorption isalways
greater for the low-0 reflections. (Theseremarks apply
only to the cylindricalspecimen used
intheDebye-Scherrer method. The
absorptionfactorhas an
entirelydifferent
form
for the flat-platespecimen used
ina
diffractometer, as willbe shown
in Sec. 7-4.)Exact
calculation of the absorption factor for a cylindricalspecimen
is oftendifficult, so it is fortunate thatthiseffect can usuallybe
neglected in the calculation of diffracted intensities,when
theDebye-Scherrer method
isused. Justification of thisomissionwill be
found
in the next section.4-11 Temperature
factor.So
farwe have
considered a crystal asa
collection ofatoms
located at fixed points in the lattice. Actually, theatoms undergo
thermal vibrationabout
theirmean
positionseven
at the absolute zerooftemperature,and
theamplitude
ofthisvibration increases as thetemperature
increases. Inaluminum
atroom
temperature, the average displacement ofan atom from
itsmean
position isabout
0.17A,which
isby no means
negligible, beingabout
6 percent of the distance of closestapproach
of themean atom
positions in this crystal.^Thermal
agitation decreases the intensity of a diffractedbeam
becauseit has theeffect of
smearing
out the lattice planes;*atoms
canbe
regarded as lyingno
longeron mathematical
planes but rather in platelike regions of ill-definedthickness.Thus
the reinforcement ofwaves
scattered attheBragg
angleby
variousparallel planes, the reinforcementwhich
iscalled a diffractedbeam,
is not as perfect as it is fora
crystal with fixed atoms.This reinforcement requires that the
path
difference,which
is a function of the plane spacingd,between waves
scatteredby
adjacent planes bean
integralnumber
of wavelengths.Now
the thickness of the platelike"planes'
' in
which
the vibratingatoms
lie is,on
the average, 2?/,where u
isthe average displacement ofan atom from
itsmean
position.Under
these conditions reinforcement is
no
longer perfect,and
itbecomes more
imperfect as the ratiou/d
increases, i.e., as thetemperature
increases, since that increases u, or as increases, since high-0 reflections involve planes oflow d
value.TThus
the intensity ofa
diffractedbeam
decreases as the temperature is raised, and, for a constant temperature, thermal vibration causesa greater decrease inthereflected intensity athigh anglesthan
atlow
angles./The
temperature effectand
the previously discussed absorption effect in cylindrical specimens thereforedepend on
angle in oppositeways
and, to a first approximation, cancel each other. Inback
reflection, forexam-ple, theintensity ofadiffracted
beam
isdecreased verylittleby
absorptionbut very
greatlyby
thermal agitation, while in theforward
direction the reverse is true.The two
effectsdo
not exactly cancelone
other at all4-11]
angles; however, if the
comparison
of line intensities is restricted to lines notdifferingtoogreatly in 6values, the absorptionand temperature
effects can be safely ignored. This is.a fortunate circumstance, sinceboth
of theseeffects are ratherdifficultto calculate exactly.It should be
noted
here that thermal vibration oftheatoms
of a crystal does not causeany
broadening of the diffraction lines; theyremain
sharp rightup
to the melting point, but theirmaximum
intensity gradually de-creases. Itisalsoworth
noting that themean amplitude
ofatomic
vibra-tion is not a function of thetemperature
alone butdepends
alsoon
the elastic constantsofthe crystal.At any
given temperature, the less "stiff"the crystal, the greater the vibration
amplitude
u.This means
thatu
is
much
greater atany
one temperature forasoft, low-melting-point metal like leadthan
it is for, say, tungsten. Substances withlow
melting pointshave
quite large values of ueven
atroom temperature and
therefore yield rather poorback-reflection photographs.The
thermal vibration ofatoms
has another effecton
diffraction pat-terns. Besides decreasing the intensity of diffraction lines, it causessome
general coherent scattering in all directions. This is called temperature-diffuse scattering; it contributes only to the general
background
of the patternand
its intensity gradually increaseswith
26. Contrastbetween
lines
and background
naturally suffers, so this effect is a very undesirable one, leading inextreme
cases to diffraction lines in the back-reflection region scarcely distinguishablefrom
the background.In the
phenomenon
of temperature-diffuse scatteringwe have
another example,beyond
those alluded to in Sec. 3-7, of scattering atnon-Bragg
angles.Here
again it is not surprising that such scattering should occur, since the displacement ofatoms from
theirmean
positions constitutes a kind of crystal imperfectionand
leads to a partialbreakdown
of the con-ditions necessary for perfect destructive interferencebetween
rays scat-tered atnon-Bragg
angles.The
effect of thermal vibration also illustrateswhat
hasbeen
called"the
approximate law
of conservation of diffracted energy."
This
law
states that the total energy diffractedby
a particularspecimen under
par-ticular experimental conditions is roughly constant. Therefore,anything done
toalterthephysicalconditionofthespecimen
does notalterthetotalamount
of diffractedenergybut
onlyitsdistribution in space.This "law"
isnotatall rigorous,
but
it doesprove
helpful inconsideringmany
diffrac-tion
phenomena. For
example, atlow
temperatures there is very littlebackground
scatteringdue
to thermal agitationand
the diffraction lines are relatively intense; ifthespecimen
isnow
heatedtoa high temperature, the lines willbecome
quiteweak and
the energywhich
is lostfrom
the lines willappear
ina
spread-outform
as temperature-diffuse scat-tering.132
DIFFRACTION
II:THE
INTENSITIESOF DIFFRACTED BEAMS
[CHAP. 44-12
Intensities ofpowder
pattern lines.We
arenow
in a position to gather together thefactors discussedinprecedingsections intoan
equation fortherelative intensity ofpowder
pattern lines:Y
1+
C0s22g>)
, (4-12)
\sin26cos6/
where
I=
relative integrated intensity (arbitrary units),F =
structure factor,p =
multiplicity factor,and
6= Bragg
angle. In arriving at this equation,we have
omitted factorswhich
are constant for all lines of the pattern.For
example, all that is retained oftheThomson
equation (Eq.4-2) is the polarization factor (1
+
cos226), with constant factors, such asthe intensityof theincidentbeam and
the chargeand mass
ofthe elec-tron, omitted.The
intensity of a diffraction line is also directly propor-tional tothe irradiatedvolume
ofthespecimen and
inversely proportional tothecamera
radius,but
these factorsare again constantforall diffraction linesand may be
neglected.Omission
of the temperatureand
absorptionfactors
means
that Eq. (4-12) isvalid only fortheDebye-Scherrer method and
then only for lines fairly close togetheron
the pattern; this latter restriction is not as serious as itmay
sound.Equation
(4-12) is also re-stricted to theDebye-Scherrer method
because of the particularway
inwhich
the Lorentz factorwas
determined; othermethods,
such as those involving focusing cameras, will require a modification of the Lorentz factor given here. In addition, the individual crystalsmaking up
thepowder specimen must have
completelyrandom
orientationsifEq.
(4-12)isto apply. Finally, itshould be
remembered
that thisequation givesthe relative integrated intensity, i.e., the relative areaunder
the curve of in-tensityvs. 20.It should
be noted
that "integrated intensity" is not really intensity, since intensity is-expressed interms
of energy crossing unit area per unit oftime.A beam
diffractedby
apowder specimen
carriesa
certainamount
of energy per unit time
and one
could quite properly refer to the total powerofthe diffractedbeam.
Ifthisbeam
isthenincidenton
ameasuring
device, such as photographic film, for a certain length oftime and
if a curve of diffracted intensity vs. 26 is constructedfrom
themeasurements,
then the areaunder
thiscurvegivesthetotal energyinthediffractedbeam.
This is the quantity
commonly
referred to as integrated intensity.A
more
descriptiveterm would be
"total diffracted energy,"but
theterm
"integrated intensity" has
been
too long entrenched in thevocabulary
of x-raydiffraction tobe changed now.
4-13 Examples
of intensity calculations.The
use ofEq.
(4-12) will be illustratedby
the calculation ofthe positionand
relative intensities of4-13] 133
the diffraction lines
on
apowder
pattern of copper,made
withCu
Ka.radiation.
The
calculations aremost
readily carried out in tabular form, as inTable
4-2.TABLE
4-2Remarks:
Column
2:Since copper is face-centered cubic,F
isequal to 4/Cu for linesof un-mixedindicesand zero for lines of mixed indices.The
reflecting planeindices,allunmixed, are written
down
in this column in order of increasing values of (h2 -f-fc2
+
Z2), from Appendix 6.Column
4: Foracubic crystal, valuesof sin26 aregiven by Eq. (3-10):sm"0 =
j-gC/r -h /r -h r;.
In this case, X
=
1.542A (CuKa)
and a=
3.615A (latticeparameter of copper).Therefore, multiplication of the integersincolumn 3 by X2/4a2
=
0.0455givesthe values of sin2 listed in column 4. In this and similar calculations, slide-rule accuracyisample.
Column
6:Needed
to determine the Lorentz-polarizationfactorand (sin0)/X.Column
7: Obtained from Appendix7.Needed
todetermine /Cu-Column
8:Read
fromthe curveofFig. 4-6.Column
9:Obtained fromthe relationF
2=
16/Cu2-Column
10:Obtained from Appendix9.134
DIFFRACTION
II:THE
INTENSITIESOF DIFFRACTED BEAMS
[CHAP. 4Column
11: Obtained from Appendix10.Column
12:Thesevaluesarethe productofthe valuesin columns9, 10, and 11.Column
13:Valuesfrom column12recalculated to givethefirstlineanarbitrary intensity of 10.Column
14: Theseentries give the observed intensities, visually estimated ac-cording to the following simple scale, from the patternshown
in Fig. 3-13(a) (vs=
verystrong,s=
strong,m =
medium,w =
weak).The agreement
obtained herebetween
observedand
calculatedintensities is satisfactory.For
example, lines 1and
2 are observed to be of strongand medium
intensity, their respective calculated intensities being 10and
4.0. Similar
agreement
can befound by comparing
the intensities ofany
pair of neighboring lines in the pattern. Note, however, that the com-parisonmust
bemade between
lineswhich
arenot toofarapart: forexam-ple, the calculated intensityof line 2 isgreater
than
that ofline 4,whereas
line 4 is observedto be stronger thanline 2. Similarly, the strongest lines
on
the pattern are lines 7and
8, while calculationsshow
line 1 to bestrongest. Errorsof this kind arisefrom
the omissionofthe absorptionand temperature
factorsfrom
the calculation.A more
complicated structuremay now
be considered,namely
that of the zinc-blendeform
of ZnS,shown
in Fig. 2-19(b). Thisform
ofZnS
iscubic
and
hasa latticeparameter
of5.41A.We
will calculate the relativeintensities ofthe first six lines
on a
patternmade
withCu Ka
radiation.As
always, the first step is towork
out the structure factor.ZnS
has four zincand
four sulfuratoms
perunit cell, located in the following posi-tions:'Zn:
\
\ \+
face-centering translations, S:+
face-centering translations.Since the structure is face-centered,
we know
that the structure factor will be zeroforplanes ofmixed
indices.We
alsoknow, from example
(e)of Sec. 4-6, that the
terms
in the structure-factor equation corresponding to the face-centering translationscan be
factored outand
theequationforunmixed
indiceswritten do\vn at once:|F|
2
is obtained
by
multiplication of theabove by
itscomplex
conjugate:This equation reduces to thefollowingform:
|F|
2
=
16I/!,
2
+
/Zn2+
2/s/Zncos*-(h+
k+
J
4-13] 135 Furthersimplification is possible forvarious special cases:
\F\
2
=
16(/s2+ /
Zn2)when
(h+
k+
I) isodd; (4-13)\F\
2
=
16(/s
-
/Zn)
2
when
(h+
k+
1} isan odd
multiple of2; (4-14)|^|
2
=
16(/s+
/zn)2
when
(h+
k+
I) isan even
multiple of2. (4-15)The
intensity calculations are carriedoutinTable
4-3, withsome columns
omitted for thesake of brevity.TABLE
4-3Remarks:
Columns 5 and 6: These values are read from scattering-factor curves plotted from the data of Appendix 8.
Column 7: \F\~is obtainedby theuseofEq. (4-13), (4-14), or (4-15), depending on theparticular values of hklinvolved. Thus,Eq. (4-13) is used forthe 111 re-flection and Eq. (4-15) forthe 220reflection.
Columns 10 and 11:
The
agreement obtained here between calculated and ob-served intensities is again satisfactory. In this case, the agreement is goodwhen
any pair oflinesis compared,becauseof thelimited rangeof6valuesinvolved.One
furtherremark on
intensity calculationsisnecessary. In thepowder
method, two
sets of planes with different Miller indices can reflect to thesame
pointon
the film: for example, the planes (411)and
(330) in the cubic system, since theyhave
thesame
value of (h2+
k2+
I2)and hence
thesame
spacing, or the planes (501)and
(431) of the tetragonal system,JLJO
DIFFRACTION
II:THE
INTENSITIESOF DIFFRACTED BEAMS
[CHAP. 4 since theyhave
thesame
values of (h?+
fc2)and
I2.In such
a case, theintensity of each reflection
must
be calculated separately, since in general thetwo
willhave
different multiplicityand
structure factors,and
thenadded
to find thetotal intensity ofthe line.4-14 Measurement
ofx-rayintensity.In
theexamples
just given, the observed intensitywas
estimated simplyby
visualcomparison
ofone
line with another.Although
this simple procedure is satisfactory in a sur-prisingly largenumber
ofcases, there areproblems
inwhich
amore
precisemeasurement
of diffracted intensity is necessary.Two methods
are in general usetoday
formaking
suchmeasurements,
onedependent on
the photographiceffectof x-raysand
the otheron
theabilityofx-raysto ionize gasesand
cause fluorescence of light in crystals.These methods have
alreadybeen mentioned
briefly inSec. 1-8and
will be describedmore
fully inChaps.
6and
7, respectively.PROBLEMS
4-1.
By
adding Eqs. (4-5) and (4-6) and simplifying the sum, show thatE
3,the resultantofthesetwosinewaves, is alsoasine wave,ofamplitude
A
3=
[Ai2+ A
24-2. Obtainthe same result
by
solving the vectordiagram ofFig. 4-11 for the right-angle triangle ofwhichA
3is the hypotenuse.4^3. Derive simplified expressions for
F
2 for diamond, including the rules gov-erning observedreflections. Thiscrystaliscubicand contains 8 carbonatomsper unitcell, located inthefollowing positions:000 HO $0i OH
Hi Hi Hi Hi
4-4.
A
certain tetragonal crystal has fouratoms of thesame
kind per unitcell, located atH.
i i, \ f,H-(a) Derivesimplified expressions for
F
2.(b)
What
isthe Bravaislatticeof this crystal?(c)
What
are the valuesofF
2forthe 100, 002, 111,and Oil reflections?4-6. Derive simplified expressions for
F
2 for the wurtzite formof ZnS, includ-ing the rules governing observed reflections. Thiscrystal ishexagonaland
con-tains2ZnS
perunit cell, located inthe following positions:Zn:000, Hi
S:OOf,Hi
Note that these positions involve a
common
translation, whichmay
be factoredoutofthestructure-factor equation.
4-6. In Sec. 4-9, inthe part devotedto scattering
when
the incidentand scat-teredbeams make
unequal angles witli the reflecting planes, it is stated that"raysscattered
by
allother planesare inphase with the corresponding rays scat-teredby
thefirstplane." Provethis.4-7. Calculate theposition (intermsof6) and the integrated intensity(in rela-tive units) of the firstfive lines on the
Debye
patternof silvermade
withCu Ka
radiation. Ignore the temperatureand absorptionfactors.
4-^8.
A
Debye-Scherrer pattern of tungsten(BCC)
ismade
withCu Ka
radia-tion.The
firstfour lines on this pattern were observed to have the following 8 values:Line 6
1 20.3
2 29.2
3 36.7
4 43.6
Index these lines (i.e., determine the Miller indices of each reflection
by
the useofEq. (3-10) and Appendix 6) and calculate their relative integrated intensities.
4-9.
A
Debye-Scherrer pattern ismade
of gray tin, which has thesame
struc-tureasdiamond,withCu Ka
radiation.What
aretheindicesofthefirsttwolinesonthepattern, and
what
istheratio oftheintegrated intensity ofthefirstto that ofthesecond?4-10.
A
Debye-Scherrer pattern ismade
of the intermediate phase InSb withCu Ka
radiation. This phase has thezinc-blende structureandalatticeparameter of 6.46A.What
are theindices of the first twolines on the pattern, and whatistheratio ofthe integrated intensityofthefirst tothesecond?
4-11. Calculate the relative integrated intensities of the first six lines of the Debye-Scherrer patternof zinc,
made
withCu Ka
radiation.The
indicesand ob-served6valuesof theselinesare:Line hkl 6
(Line 5 is
made up
of two unresolved lines from planes of very nearly thesame
spacing.)