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IN-PLANE TEXTURING IN
SPUTTERED FILMS
J.F.
WHITACRE*,
S.M.YALISOVE
andJ.C.
BILELLOUniversity
of
Michigan,Departmentof
MaterialsScienceand Engineering,2300 Hayward Street, AnnArbor, MI48109, USA(Received8October1999)
Filmsconsisting ofMo, Cr,andTahaveall been foundtodisplaywell-defined biaxial textureswhen grown undercertain conditions.Awell-definedout-of-planetextureevolves
withinthefirst 100nmof the film, followed by theevolutionofapreferred crystal-lographicorientation inthe plane of thefilm.Theseeffect werestudiedusingX-ray pole-figure analysis, scanning electron microscopy(SEM),transmissionelectron microscopy
(TEM),transmissionelectrondiffraction(TED),and highresolutiongrazingincidence
X-rayscattering(GIXS).Ithas been found that in-planetextureevolvesonly when there is,onaverage, oblique adatom fluxincident ontothe substrate.Further, the type of
out-of-planetexturecan be controlled by altering the deposition conditions. Parameters
including cathode-to-substrate distance, deposition rate, average angle of adatom
inci-dence, and sputter gas pressure, have been shownto determinethetypeout-of-plane texture, as well as therateofin-planetextureevolution.Thestudiesconducted have shown thatit ispossibleto createand control biaxially textured films and multilayers made of a variety ofmaterials.Arecentmodelwhichdescribes thisphenomenais discussed.
Keywords: Sputtered films;Texture;Multilayers;X-ray; TEM;SEM
INTRODUCTION
Thin metallic films are frequently used in applications such as
inte-grated circuit interconnects
(Muraka, 1993),
protective coatings(Windischmann, 1992;Adamsetal.,
1993),
magnetic recording media(Katoaka
etal., 1993; Kiefand EgelhoffJr.,
1993; Kimetal.,1993),
and superconducting multilayers
(Mattson,
1997; Bauer etal.,1997).
* Corresponding author.
Thetexturingin these filmsis acritical property,andtheabilityto
con-trol the development ofboth out-of-plane and in-planetexture is of
interest. Relevantstudieshave focused on theeffects of energeticion
beams (Bradley et al.,
1986),
sputter gas pressure(Je
et al.,1997),
deposition geometry (Hagemeyer etal., 1993; Karpenkoet al., 1994;
Bilelloetal., 1995;
Harper
etal., 1997; Rodriguez-Navarroetal.,1998),
surface energetics(Knuytetal., 1995; ThompsonandCarel,
1995),
andimpurity concentration
(van
de Waterbeemd and van Oosterhout,1967)
haveontexturing. Thedevelopmentofin-planetexturehas beenattributedtoanumber ofmechanisms.Theexistenceof oblique adatom
flux has been found to benecessary in somecases (Karpenko et al.,
1994;
Harper
etal.,1997;Bauer
etal.,1997).
Othersusedanoff-axis ion beamtopreferentiallysputter films duringgrowth, thereby encouragingthe formation of in-plane texture(Bradley etal.,
1986).
Still anotherinvestigation hasshown that filmsgrownwithoutanyaverageoblique influencedonotdevelop any in-plane texturing
(Malhotra
etal.,1996).
Deposition geometryplays a critical role in in-plane texturing, while
the role of deposition kinetics and energetics are not currently well
understood.
Belowisareviewof work donetoincreaseunderstandingoftexture
evolution in thin sputteredfilms.
A
particularsetofdeposition condi-tions whichleadtothe formationofastrongbiaxialtextureinsputteredfilms of
Mo, Cr, CrN,
andTa
will be described. Once the basicphe-nomena of in-plane texturing was well documented, further
experi-mentsweredonetoprovidebetter understanding of the role ofadatom
kineticsduringgrowth. This wasaccomplishedby altering the sputter
gas pressure, chamber geometry, deposition rate, and growth
tem-perature during film growth. Experimental results will be presented
and discussed in light ofa model which describes in-plane texturing
andisbased on twosimplephysicalmechanisms.
DESCRIPTIONOF EXPERIMENTS
Deposition Chamber
All filmswere deposited in a DentonTM cryo-pumped
DC
magnetronsputter chamber (Whitacre et al.,
1998). A
base pressure ofat mostvaried from 2 to 20mTorr. The substrates, as received test-grade Si
(100)
wafers, were mounted on a platen which rotated beneath the sputter targetat a rateof20rpm. This setupallowed formultiple filmstobegrownatonce.Thesubstrateswereexposedto afull 180 rangeof
flux in the plane parallel to their direction ofrotation.
In
the planenormaltorotationdirection,however, theangular flux rangeismuch
less.Thisconfiguration providesabreak in the symmetry of the
depo-sition: thereis, on average,more oblique fluxin one plane over any
other. Figure showsaschematicof thedeposition chamber.
Analysis Techniques
Microstructureand film texturingwerestudiedusing scanning electron
microscopy
(SEM),
transmission electron microscopy(TEM),
trans-missionelectrondiffraction
(TED), X-ray
pole figure analysis, and highresolution
X-ray
diffraction (using the symmetricGIXS
geometry).An
Hitachi S-800 field emission SEM was used with its acceleratingpotential at 7kV and its sample distance set to 5 mm, allowing for resolved imagestobe recorded atmagnifications of20,000-40,000x.
Further analyses used a JEOL 2000
TEM
(accelerating voltage=200
kV).
Plan-viewsampleswerecreatedusinganHFetching technique(Whitacre
etal.,1998),
whilecross sectionsamplesweremadeby tripod polishing. TEDwas performed usingthe JEOL 2000to qualitativelyanalyze texturing. Alldiffraction patterns were recorded from a defined
areaof equalsize ineachofthe samples usingaselectedareaaperture.
Pole figu.re analysis wasdone using both a Rigaku reflection pole
figure apparatus which used the Schultz geometry, and an inelTM
(It) ca
e
pl
sutrate/./7/,
U
rotation direction (b)]
cathode averageou v //
rotationectionFIGURE Schematic showing deposition chamber geometry: (a) overview, and
(b) representation showing how the average flux vector changes angle ofincidence
position sensitive detector attached to a Huber four-circle
diffracto-meter(Karpenkoetal., 1994;Malhotraetal.,
1998).
scanscollectedin thesymmetric grazingincidence
X-ray
scattering(GIXS)
geometry allowed for thedegreeof in-plane texturing offilmstobe studied preciselyatvaryingdepths (Karpenko,
1996).
RESULTS AND DISCUSSION Texture Evolution in
Mo
FilmsTheevolutionof both in-plane andout-of-planetextureswasobserved
in Mo films grown at a rate of
34nm/min
under the conditionsdescribed above (Karpenko etal., 1994; Bilello et al.,
1995).
Textureevolution may be seen in the
(110)
pole figures and correspondingTEM/TED
analysisshown in Fig. 2.By
thetimethe film reachesathicknessof 200 nrn,awell-definedout-of-planetexture,
(110)
in thiscase, is observed.As
thefilms becomethicker, both the out-of-planeand in-plane texturesbecome stronger.
The 2ttmthick filmdisplaysa "timesrandom" value of 16: this film is 16
times more organized crystallographically than a randomly oriented
sample(Karpenkoetal.,
1994).
TheTEM/TED
analysis supports thepole figure data: as the film becomes thicker,the electron diffraction
(a)
FIGURE2 (a)Pole figures showing theevolutionoftextureinMofilmsfor thick-nessesofa:200run,b:500run,c: 1000runand d:2000run.Thenumber inthe upper righthand comer of eachpole figureisthe "times random value.(b) TEM/TED
ana-lysis for thesamefilms.The directionof grain elongation in the thickerfilms is
patterns showan increase in localized diffraction consistent with the
existenceof in-planetexture.There is alsoanincrease ingrainsize inthe
planeof the film; the grains becomeelongatedin the directionnormalto
substratemotion.
By
comparingthe electron diffraction patternstothebrightfield
TEM
images,itcanbededucedthatthe grainsareelongatedin their
(100)
direction and arenarrowestin the(110)
direction. Thesurfacemorphologyof the 2tmthick film isshown in the
SEM, AFM,
and cross section
TEM
imagesofFig.3. Thegrainsarefacetedandhavesomevoid formation betweenthem,asattested tobythe
TEM
image.X-ray
analysis, scans in the symmetricGIXS
geometry, ofMofilmsof different thicknesses show theevolution of in-plane texturing
(Karpenko,
1996).
Figure 4 has this data. The full-width at halfomaximum of the recorded peaks isinversely related to the degree of in-plane texturing; thediffractedintensityatany
b
isproportional tothe number of grainswiththat particular in-planeorientation. Thistype
of analysis allows for precise comparison of the degree of in-plane texturing in various films.
Chromium
Crfilms grownunder nominally the sameconditionsasthe Mo films
describedabove alsodisplayedin-planetexturing. Figure 5 shows the
FIGURE 3 Comparative images showing the surface morphology ofa2pro thick
MoFilm:(a)plan-viewSEM, (b) AFM (theprofileplotis a cross sectiontaken from the area indicated by thewhiteline), and(c) cross sectionbright-fieldTEM (figure adapted fromWhitacreetal.,1998).
104
1000
0 60 20 B0 240 300 360
Phi(’)
FIGURE4 Plot showing the detecteddiffractedintensityinforatexturedMofilm
oriented inthe(110) Braggconditionusingbscansinthe symmetricGIXSgeometry.
Foreach film, theX-raypenetration depthwas100 nm.Thethickerthe film, the higher
thedegree oftextureobservedinthetop 100 run(figureadapted from Karpenko,1996).
90 90 90 f/-
-
counts 135/./’- "",>.4,5 135:... 135./....,
.45/.
-.
::,,(....,,
700,.---_
--..,..
,.>
/
:S
(a) 270 (b) 270 (el 2705mTorr 7 mTorr I0mTorr
FIGURE 5 Plan-viewSEMimages and corresponding(110) polefigures for 1.5pm
thickCrfilms grownwithArsputter gas pressures of(a) 5mTorr, (b)7mTorr, and
(c) 10mTorr. The 5mTorr film has a strong(111) out-of-plane texture anda
well-defined in-plane texture. The in-plane texture is lessdefined in the 7 and 10mTorr
surface morphology and
(110)
pole figures from aCr
film grown at roomtemperaturewithacathode height of 9.5cm,a rateof 20rim/
minandthree different
Ar
pressures: 5, 7 and 10mTorr. Thepolefig-ures show thatin-planetextureoccursin varying degreesin Crfilms.
Texturingdependenceonsputter gaspressurewillbediscussed in alater
section.Though the grain shape andsymmetryof the
Cr
films arenotidentical tothose observedin Mo,the sameeffects and evident: grain
elongationin theplaneofgrowthnormaltothe direction of substrate
motionduringgrowth,and faceted surface morphology.
Tantalum
Figure 6 shows the surfacemorphology andcorresponding
(002)
and(202)
pole figures ofa3Im thick (tetragonalphase) Ta film grownunder theconditionsdescribed in the experimental section. The
micro-structure differs dramatically from that observed in the
Mo
and Crfilms; the surface is not faceted, but instead consists of elongated
rounded features.
As
inthe other cases,however,thedirectionoffea-tureelongation isnormalto the direction ofsubstratemotion during
deposition. The pole figures show that thefilmhasastrong
(002)
out-of-planetexture.The
(202)
polefigure shows that there isasignificant in-planetexture,thoughitis not asstrongasthatobserved in films suchasMoor
Or.
Chromium Nitride
In-planetexturing has been observed inCrN (Zhao,
1998).
Thedepo-sitionconditions leadingtotheseeffectsareidenticaltothosedescribed
FIGURE6 Plan-view SEM images and corresponding pole figures for 3pin thick
Ta film. The pole figuresindicate a strong (002) out-of-plane texture and some
in-planetexture. Thedirection ofsurface feature elongationisnormaltothedirection of
above,except thatnowthereactivesputteringisused.
A
dependenceofnitrogencontent ontexturingwasobserved.
Texture Control
The type ofout-of-planetexture has been foundto depend upon the
cathode height during deposition, the growth rate (Karpenko etal.,
1994; Bilello et al.,
1995),
and sputter gas pressure (Windischmann,1992).
Figure 7 shows SEM and corresponding(110)
pole figuresfor 2.5tm Mofilmsgrownwithacathodeheightof 9.5 and 12cm. If thecathode height is 9.5 cm, there is a strong 111 out-of-plane texture
component, while the film grown with the cathode height at 12cm
showsonly
(110)
typeout-of-planetexture.These filmsweregrownat,nominally, thesamerate.If theratesarechanged, however,wealsosee adifference inthetextureorientation
(Karpenko
etal.,1994).
Thereisa difference between 2tmthick Mo films grown at different growth
rates: films grown at 68
nm/min
displays a strong(111)
typeout-of-plane orientation, while similar films grown at 34
nm/min
shows astrong
(110)
out-of-planetexture.Figure 5 showspolefigures fromCrfilmsgrownatthree different
Ar
pressures: 5, 7,and 10mTorr.The type ofout-of-planetexturedepends
upon thesputtergaspressure. The filmgrownat 5mTorrhas a
(111)
out-of-planetexture, while the filmgrownat10
mTorr
displaysa(112)
out-of-plane texture. The 7mTorr film has a mix of the two types ofout-of-planetexturing. The filmdepositedusing 5mTorrof
Ar
dis-playsahigherdegree of in-planetexturethanthefilmsgrown under 7
and 10mTorrofAr.
FIGURE 7 Plan-view SEM images and corresponding (110) pole figures for 2tm
thick Mo films grown with cathode-to-platen distances of(a) 11ern and (b) 7cm.
The smallercathodeto substratedistance provided a mixed(111)/(110) out-of-plane
FIGURE8 Plan-viewSEMimages and corresponding(110)pole figures for 1.5ttm
thick Crfilms grownat 290Cwith Arpressures of(a) 10mTorr, and (b)3mTorr.
Thereisless in-plane organization for the film grownat10mTorr. Bothfdms display
astrong(111)out-of-planetexture.
Temperature
EffectsChromium filmsweredepositedatatemperatureof-,290C usingtwo
different sputteringgas
(Ar)
pressures. The cathode height was 9.5mand a shieldedfilamentheater affixed totheceilingof the deposition
chamber was used. Figure 8 shows plan-view SEM and
(110)
polefiguresoftwo2Ixmfilmsgrownusing 10 and 3
mTorr
ofAr.
Several differences frompreviousgrowthsareevident.The grainsize
issignificantlysmallerthanfilmsgrownunder the same conditionsat
room temperature. The grains are still faceted, though they are no
longerelongatedintheplane of growth.Thepolefigures show that each film hasa
(111)
out-of-planetexture, butonlythe filmgrownusing thelower
Ar
pressure of3mTorr
displaysanyin-plane texturing.Growthonto RoughSurfaces
Mo films
400tm
thick were deposited onto well-defined roughenedsurfaces
(Whitacre
et al.,1998).
This study found that if the roughfeatures were largeenough to limitthe angular rangeof adatom flux
duringgrowth thereis a measurable decreasein the rate of in-plane texturing
(Whitacre
etal.,1998). By
slightlymanipulatingthe geometry of thedeposition, substrateroughnesslimitsthefilmstexturing.Discussion
It is evident that in-plane texture develops in thin sputtered films if thereis:
(1)
onaverage, oblique adatomflux,and(2)
sufficientadatomIf the substrate restsdirectlybeneath thecathode during growth,no
in-plane texture develops, though a strong out-of-plane texture and
faceted surface
morphology
exists(Malhotra
etal.,1996).
If, however,the substrateiskepteitheratastationary off-axis location
(Malhotra
etal.,
1996)
or isrotated beneaththecathode,biaxial texture iscreatedinthe film.
It
has been shownthat if thesubstrate surfaceisroughenedsuch that the averageangleof oblique adatom fluxislimited, therateof in-plane texturing decreases(Whitacreetal.,
1998).
Inall of thesecases,an out-of-plane texture develops first, followed by the evolution of in-planetexture asgrainscompeteduringgrowth.
A
model has been proposed which describes in-plane texturing(Karpenkoetal.,
1997). It
isassumed that in-plane texturingis aresultofthe combination oftwophysical mechanisms:
(1)
anisotropicsurfacetransport, and
(2)
atomistic shadowing effects whichoccurwith obliqueadatomincidence.Anisotropic surfacetransport causesgrainstogrow
faster along a particular crystallographic direction in the plane of
growth. Forexample, Mo grainsgrowmostrapidly along their
(100)
axisand slowest in the
(110)
direction. Thisresults ingrainswhichareelongated
(to
increasingdegreesasthe filmsthicken) alongtheir(100)
direction.
If there is minimal surface diffusion, atomic shadowing occurs.
Adatomspileuponexisting grains creating significantvoidformation
between those grains
(Dirks
andLearns, 1977).
Ifthe adatoms areobliquely incident onto the substrate, this shadowing effectwill also
causethe adatom pileuptobemoreefficient in one in-plane direction overany other.
In
particular, adatomswill contributemostefficientlytoin-plane formationinthedirectionnormaltothe projection of the flux
vector ontotheplaneof the substrate.Thisisthein-planedirectionof
highestadatomcaptureefficiency.Minimumcapture efficiencyis inthe
directionparalleltothe projection of the incoming fluxvector.When
both shadowing and anisotropic surface transport conditions exist
concurrently with oblique adatom flux, those grains whose crystal-lographic fast in-plane growth direction corresponds to the highest
adatom capture efficiency direction will compete favorably during
deposition. Eventually, onlythosegrainsthatnucleatedwith theirfast crystallographic growthdirectionalignedwiththe directionof highest
expressed mathematically and compared with
X-ray
data collectedfrom filmswasin-planetexturing(Karpenko,
1996).
Ifthismodelis correct, an increase in eithersurfacetemperatureor
adatom kinetic energy should affect the in-plane texturing rate by
altering anisotropic surfacediffusionandthe effectivenessof the shad-owingmechanism.If thefilmsurfaceisheated, surfacediffusionshould
dominatetheshadowingeffect and in-planetextureshould evolvemore
slowly.This isobservedin theCrfilmsstudied,where the filmgrownat
290Cin 10mTorrof
Ar
has almostnoin-plane texturingcomparedtoasimilar filmgrownat roomtemperature.
An
increase inadatomkineticenergy should promotesurfacediffu-sionand workagainsttheshadowingeffect.
By
lowering theAr
pres-sure,the averageadatom kinetic energy increases(Meyeretal.,
1981).
Experimentally,different
(or
mixed) out-of-planetexturingisobserved.However,
there isnotasignificantdifference inthedegree of texturingbetween
Cr
filmsusing differentAr
pressures. This effectiscurrently underconsideration andwillbe addressedinalaterpublication.CONCLUSIONS
For
sputteredthinfilmstodevelopabiaxial texture,theremustbe,onaverage,someoff-axisoroblique geometrical influenceonthegrowing
film to allow for grain competition during growth. This paper has
addressed how thepresence ofoblique adatom fluxduring DC
mag-netronsputteringleadstothedevelopment of in-planetexture.
Once
thegeneral phenomena was characterized in a variety of films, further
studies weredonetoexplore therole ofsurfaceenergeticsandadatom
kineticsduringgrowth. Ithasbeenshown thatin-plane grain
compe-tition is sensitive to surface diffusion; films develop in-plane texture
moreslowly atelevated temperatures. Ithas also been shown the an
increase in adatomkinetic energy, while beingenoughto control the
type ofout-of-planetexture, isnotenoughtodramatically affettherate
of in-plane texturing. The relevance of these results to a model
which describes the evolution of in-plane texturingwasdiscussed.
By
addressingquestions raised, a newlevel ofunderstandingofin-plane
Acknowledgments
This work wassupported under
ARO
Army
contractnumbersDAAH
04-95-1-0120 and
DAAG
55-98-1-0382. Diffraction data collected atSSRL beamline7-2, fundedbytheUS
DoE.
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