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Ar+ beam sputtering on solid surfaces and nematic liquid crystal orientation
Z. Sun, J. Engels, I. Dozov, Geoffroy Durand
To cite this version:
Z. Sun, J. Engels, I. Dozov, Geoffroy Durand. Ar+ beam sputtering on solid surfaces and ne- matic liquid crystal orientation. Journal de Physique II, EDP Sciences, 1994, 4 (1), pp.59-73.
�10.1051/jp2:1994115�. �jpa-00247950�
J.
Phys.
II France 4 (1994) 59-73 JANUARY 1994, PAGE 59Classification Physics Abstracts
61.30 68.10
Ar+ beam sputtering
onsolid surfaces and nematic liquid crystal orientation
Z. M. Sun
(*),
J. M.Engels,
I. Dozov(**)
and G. DurandLaboratoire de Physique des Solides. Bit. 510, Umversitd de Paris-Sud, 91405 Orsay Cedex, France
(Received 8 July J993, received in final form 20 September J993, accepted 27 September J993)
Rdsumd. Nous avons dtudid
expdrimentalement
l'orientation moldculaire du ndmatique SCB sur des substrats solides bombardds obliquement par un faisceau d'ions Ar+. Le bombardement d'un substrat isotrope donne une orientation planaire le long de la projection de la direction de bombardement sur la surface. Un bombardement sur un substrat qui donne ddjh une orientation planaire (selon un autre m6canisme)produit
une orientation intermddiaire saris inclinaison. Darts lecas d'un bombardement sur un substrat donnant une orientation planaire par dvaporation sur une
sous couche d'ITO, nous trouvons en
plus
de la torsion une inclinaison additionnelle. Nos exp6riences montrent que la variation de l'orientation en surface crdde par le bombardement est reticle h la profondeur drodde.Abstract.- The molecular orientation of nematic SCB on various solid substrates eroded obliquely by an Ar+ ion-beam has been studied
experimentally.
The sputtering on an isotropicsubstrate
(normally evaporated
SiO) results in a nematic planar orientation along theprojection
of the localvelocity
of the ion direction on the surface. When using an anisotropic substrate(obliquely evaporated SiO which gives planar orientation in absence of sputtering) we find a continuous twist of the
resulting
alignment, from the initial planar orientation towards the beam track projection. Although the geometry allows it, we do not observe any surface orientation bistability.1. Introduction.
Molecular orientation of nematic
liquid crystals
on solid substrates isimportant
because of its fundamental interest and forpractical application
inliquid crystal display
devices. In the last years,anchoring properties
ofliquid crystals
on surfaces have beenextensively investigated
(*) Present address Laboratory of Solid State Microstructures, Nanjing University, Nanjing, 21008, P-R- of China.
(**) Present address Institut of Solid State Physics. Bvd Lenin, Sofia, Bulgaria.
[1-3].
Inthermotropic nematics,
surfaceanchoring
isusually
described in terms of theRapini- Papoular expression [4].
The « order electric »polarization
associated with thegradient
oforder parameter also
plays
animportant
role in surfaceanchoring
onrough
surfaces[5].
Recently
Monkade et al. described an « orderelectrically
» controlled continuous transition from aplanar
to anoblique
nematic orientation on SiOobliquely evaporated glass plates [6].
In the transition zone, a twofolddegenerate oblique
surface orientation was observedexperimen- tally.
Thisdiscovery
allowed the realization of surface transitions between these bistableanchorings,
drivenby
electric fields ofopposite polarities [7, 8].
It seems to bepossible
todevelop
with these bistableplates
a new type ofdisplay
devicecomparable
to thatusing
ferroelectric
liquid crystals
inswitching speed.
On the other hand, the transition zone ofevaporation
parameters where surfaceanchoring bistability
is observed is very narrow andrequires
a delicate control of the process.Therefore,
it isimportant
to seek for a methodinducing
a twofolddegenerate
surface orientation moreeasily.
In this paper, we
study
the influence ofsputtering
with an Ar+ ion-beam on solidplates,
upon the nematic orientation induced
by
these surfaces. First we shall start with asimple
caseI-e-,
sputtering
of anisotropic
substrate, to see the pure effect of thesputtering
on the surfaceorientation. Then, we
study anisotropic
surfaces : we describe the variation of surfaceorientation induced
by oblique
ionsputtering perpendicular
to theplanar
orientationproduced by oblique
SiOevaporation.
We observe a symmetrybreaking
of the surface orientation.Finally, considering
the need toapply
an electric field inswitching
surface orientations, weinvestigate
the sameproblem
when the surface is aplanar
ITO-coatedplate, looking
for abetter
approach
to create a twofolddegenerate
surface orientation.2.
Experimental.
The
liquid crystal
used in ourexperiment
is the nematic SCB(pentyl cyanobiphenyl).
Theoptical
observation of the surface orientation isperformed
in a «hybrid
» cellconsisting
of a SiOevaporated plate la
standardglass plate
or an ITO-coated Baltraconplate)
and a silane-coated
homeotropic aligned glass plate.
The SiOplates gives «planar» orientation,
I.e.nematic molecules in the
plane
of theplate,
andperpendicular
to theplane
ofevaporation.
The silaneplane gives
«homeotropic
» orientation, I.e. molecules normal to theplates.
Theseorientations result in a bent «
hybrid
» nematic texture. Thehybrid
geometry is chosen because theresulting
orientation of the nematic texturedepends only
on theplanar
treated substrateplate.
Theevaporation
set-up has beenlong
ago described[9].
Theevaporation
zenithalangle
with the normal (seeFig. I)
a is 0° and60°,
and theevaporated
SiO nominal thickness 3 is 300Ji
and 700h,
measurednormally
to theplate
from thefrequency
shift on anoscillating
quartz.Before
preparing
thehybrid
cell, SiOevaporated plates
aresputtered by
an 8 kev ion-beamwith a beam diameter of l mm. In the case of
oblique sputtering,
we want tostudy
theinfluence of the
sputtered
thickness on the surface nematicorienting
power. To do so, we vary thesputtered depth
with thespatial position along
thesputtered
track. This can be doneby
astep-scan
technique, I.e.,
thespatial juxtaposition
andsuperposition
ofsputtered
areas with differentdepths.
Several methods can beindependently
used to fulfil thisgoal,
e.g. mechanical small rotation of targets, variation of sweep beamvoltage,
a.s.o. In ourexperiment,
the ion beam iselectrically
scanned to create a line in one direction. The scan in theperpendicular
direction is achieved
by
afive-step
scan. Each step takes between 10 to 60 s.Generally, sputtered
tracks are about 7 to 12 mmlong,
6 to 8 mm wide. The maximumsputtered depth
can reach 000
h.
For the normal incidence, the substrate issputtered
for 4 to 40 s without steps scan.N' NEMATIC ORIENTATION ON SPUTTERED GLASS 61
When
sputtering
an insulator substrate such as, forexample,
SiOevaporated glass plates,
aspace
charging phenomenon happens
so thatsputtering
cannot beeffectively performed.
Toovercome this
difficulty,
we use agrounded
metal cover[10]
with arectangular
window incontact with the surface of the
plate,
to surround the chosen zone to besputtered.
Whensputtering
atgrazing
incidence, a breach is cutalong
the side of the windowfacing
the ion-beam so that no obstacle shades the ion-beam. When
sputtering
SiOevaporated glass plates
with
ITO-coating,
nogrounded
metal cover needs to be used, theconducting
ITOlayer being
in fact
grounded by
the metallic holder itself.The variation of the eroded
depth
d withspatial position
inside the track can be assessedfrom the measurement of surface
profiles.
This measurement is made on a surfaceprofiler
Dektak 3030 with a vertical resolution of 20
h
anda
profile
scanlength
of 10-12 mm. On the non-treated side of theplate,
we draw a series ofpoints
at intervals of 2 mmalong
two directionsperpendicular
to each other in order to locate referencepositions.
On the surfaceprofiler,
we let the diamondstylus
scanalong
differentstraight
lines locatedby
the markedpoints.
We thus obtain a series of surfaceprofiles. By comparing
two surfaceprofiles along
achosen line before and after
sputtering,
we can determine thespatial
variation of erodeddepth along
this line. Thepractical
accuracy of the measurement is more related to thedifficulty
offinding
back the same track on theglass
than to the resolution. Inpractice,
we loose almost an order ofmagnitude
in accuracy. We can achieve anuncertainty
on d of ± 50h, depending
on
the
glass
surfaceroughness.
The thickness of the nematic
hybrid
cell used to determine the nematic orientation is definedby mylar
spacers 8 ~Lm thick. Theexperiment requires
a uniform thickness of the cell, which can be controlled as follows : let the empty cell be illuminatedby
a beam ofHg
monochromatic greenlight.
Interierencefringes
can be observed in the cell.By suitably adjusting
threefixing
screws on the cell holder, we can eliminate all
fringes.
In this way, we obtain an empty cellwith uniform thickness. This uniform thickness. This uniform thickness is not
exactly
that of the spacers. The real thickness of the nematiclayer
can be determinedby
anoptical
method that we will describe later. The cell is filledby capillarity
with nematic SCB(pentylcyanobi- phenyl)
in theisotropic
state at 40-50 °C.Anisotropic
nematic textures are observed at roomtemperature
(22
°C j under a Leitzpolarizing microscope
with crossedpolarizers.
Thesample
is illuminated with
linearly polarized light
which ispropagating
normal to theglass plates.
The wavelength
oflight
is A=
5
461h.
To
analyze
the effect of the erodedsurface,
we must determine the orientation of the nematic director n on thesputtered
surface with the geometry defined infigure
I. Undermicroscope
z
b
a e
n fi
/
~
/
x
Fig.
I. Orientation geometry on thesputtered plate.
e, b arerespectively
the directions of SiO evaporation and Ar~ ~puttering.with crossed
polarizers,
black zones characterizeregions
where the horizontalprojection
ofn
is
along
one of thepolarizer
oranalyzer
axes. n can be further determined with anoptical
compensator. The azimuthalangle
~b of n can beeasily
measured for each surfacepoint by rotating
themicroscope
stage andtaking
thestarting planar
directionimposed by
the SiOcoating
in absence ofsputtering
as ~b=
0°. The tilt
angle
o of n with the z-axis normal to the cellplates
can, inprinciple,
be obtainedby using
the twin domain method[I II
for which we need not know the cell thickness. In the case of absence of twin domains, we have to use therelationship
between the tiltangle
and someoptical
and elastic parametersreported
inreference
[12]
to calculate theangle
if other parameters are known. However,just
asmentioned
above,
we do not know the real thickness of the cell. Therefore we must firstdetermine this parameter. In the non-eroded
region
of SiOobliquely evaporated
substrate, wehave checked that the molecular orientation is
strictly planar,
I.e., o=
90° in terms of the twin
domain method
[I I] (note
that in the non-erodedregion
twin domainsalways appear).
Wemeasure the
optical path
difference between theordinary
andextraordinary
waves with acompensator in the non-eroded
region.
We can then derive the cell real thicknessby
means of a standardoptical
calculation(Eq. (7)
in Ref.[12]),
and the data of elastic constants and refractive indices of SCB[13, 14].
Since we have a uniform thickness cell, we can deduce theangle
o in thesputtering
track with this calibration.3. Nematic orientation induced
by
thesputtering.
3.I SPUTTERING ON ISOTROPIC SUBSTRATES.
3. I. I
Single sputtering.
First of all, we would like to know the pure effect ofsputtering
on anisotropic
substrate. It is known thatoblique
SiOevaporation
canproduce
nematic surfaceorientation
(planar
ortilted), depending
upon thepreparation. Conversely,
from the symmetry,a SiO normal
evaporation
must result in an «isotropic
» texture. Such a texture has beenobtained
by
an SiO normalevaporation
onglass plates la
=
0°,
3=
700
h).
Observation of the nematichybrid
cell does show a local orderedplanar
orientation but a random distribution of n. We are not sure whether n isexactly parallel
to the surface or not, because it isimpossible
to measure the tilt
angle
in such aspatially inhomogeneous
texture.As a first step, an
isotropic
SiO normalevaporated glass plate la
=
0° is
sputtered
withAr+ ions at
grazing
incidence(p
=
80°
).
The nematic cell(Fig. 2)
shows areasonably good
classicalplanar
texture. In thesputtered
track, limitedby
twostraight boundary
lines inducedby
thestraight
border of thegrounded
metal cover, the directors n orient themselveseverywhere along
theprojection
of thesputtering
direction on the surface withouttilting.
Forsimplicity,
thisprojection
direction is calledb~
direction(parallel
to they-axis
ofFig. Ii.
In thecase of nematic surface
anchoring,
the ionsputtering
atgrazing
incidenceplays
the same roleas a unidirectional
rubbing,
which also inducesplanar
texture. It has been revealedby
electronmicroscopy
that for standard SiO incidenceangle (a
=
60° the SiO
layer
appearsquite
smooth for small thicknesses 16 100
hi
and becomesfully
compact above 000h [15]. Up
to now no information is available for SiO normal
evaporation.
From texture observation, we suppose that ionicsputtering produces
tracks inside the smoother SiOlayer,
which forcesmolecules to
align along b~.
Note that, in the ionsputtering
atgrazing incidence,
we wereunfortunately obliged
to use thinmicroscope
coverglass plates
of lower surfacequality.
It is then difficult to measure thespatial
variation of erodeddepth
in this case. We are sure however that the erodeddepth
does increase,although
we did not measured itreliably. Experiments
show thatplanar
surface orientation inducedby
such asputtering
seems to beindependent
of the erodeddepth, although
itsstrength
may vary.Then, we
change
the zenithalangle
p of the Ar+sputtering
at constant azimuth(Fig.
I). Westudy
the influence of p on the nematic surface orientation. The same «isotropic
» substrate isN° I NEMATIC ORIENTATION ON SPUTTERED GLASS ~~
Fig. 2. - of an
sotropic SiO
sputtered obliquely
withp
=
40°.
Figure
3 shows the nematic texture afteroblique sputtering.
We find that the nematic director orients itself
along
theprojection
on the surface of the localvelocity
of ions, withouttilting.
In the central part, the directorsalign along
theprojection
of thesputtering
direction on the surface. Close to the two lateral boundaries, the nematicdirectors deviate of about ± 10°-30°. Such distributions of n is
probably
related to a surface electric field. SiO is an insulator. Whensputtering
on such a substrate with Ar+ ions, there must exist an electric field between the centre of the ion eroded SiO and thegrounded
metalFig.
3. Texture of anisotropic
SiO normalevaporated
(a = 0°, 3=
7001)
glassplate sputtered
obliquely (p 40° ), (x 10).cover. Therefore, ions could deviate outwards from the
original
track under the action of thisfield,
and create a small twist of ncompared
to the centre.Finally.
let us see the effect of normalsputtering (fl
=
0
).
We expect noplanar
orientation, whensputtering normally
on anisotropic plate.
However, as a result of a surface fieldaction,
ions should deviate
radially
from theiroriginal
track. We do observe(Fig. 4)
a « core » in thecentre of the eroded track and four black brushes outside the core. These black brushes remind
us of the texture of a nematic « disclination » with S
= + I. Measurements indicate that
directors
align
more or lessradically
withouttilting.
Thisexperimental
fact is ingood
agreement with the surface electric fieldhypothesis.
P A
l'
Fig.
4. Texture of an isotropic SiO normalevaporated
(n = 0°, 3 = 700h) glass
plate sputterednormally (p 0° ), (x 10).
In summary,
sputtering
of anisotropic
substrateby
Ar+ ions creates ingeneral
aplanar
nematic orientation without tilt,
along
theprojection
of the localvelocity
of ions on theglass plate.
Normalsputtering
creates a radial distribution of directors but this isprobably
due to a surface deviation of the ion from a radial surface field. Whenincreasing
the zenithalangle
p of Ar+sputtering,
the nematic director tends toalign unidirectionally along
the ion beamprojection
on theplate. Sputtering
atgrazing
incidence induces the best uniformplanar
orientation.
3.1.2 Double
sputterin~g.
We have beenknowing
so far thatsputtering
atoblique
incidenceon
isotropic
substrates can create aplanar
orientation without tilt. We would like now to check if doubleoblique sputtering along
differentdirections, performed
on the sameplate,
couldresult in two
planar
« bistable» orientations.
So,
we let an Ar+ ion-beam sputter anisotropic
substrate twice
along
two directionsb~j
andb~j. b~j
makes a 45°angle
with respect tob ~_ When the two associated
sputtering
times ti and t~ are the sameit,
= t~ 20 s), the
n~matic
texture inducedby
the treatedplate
is shown infigure
5. In theoverlap region
all directors orientalong
b~ direction. It seems that the second
sputtering destroys completely
the effect of the first one. ~~ie can still find some very small domains in which directorskeep
theoriginal
orientation bj. If the second
sputtering
time is shorter than the first one, e.g.N° I NEMATIC ORIENTATION ON SPUTTERED GLASS 65
, l'~ bpi
Fig. 5. - of
an isotropic SiO normal evaporated (n = 6 = 700hi glass plate
tj/t2
~ 5 and t~ = 4 s, the texture exhibitsdiffering
features, as shown infigure
6. We note that the secondsputtering
cannotdestroy completely
the first one in theoverlap region.
Across thesputtered
track, the_molecular
orientationchanges
fromb~,
to b~~. Meanwhile, we also observea few small double-leaf domains shown in
figure
7. These domains have defined leaf-likeshapes
and do notchange
theirshapes
whenforcing
the nematic to flowby squeezing
the cell.The
optical
pattem of the double-leaf domain shows that surface orientation in each leaf of domain is orientedalong
theprojection
direction of thecorresponding sputtering.
Fig.
6. - ofan isotropic SiO normal evaporated (a = 0°. 3 =
001) glass late at
r'
N° I NEMATIC ORIENTATION ON SPUTTERED GLASS 67
the
sputtered depth.
Based on these ideas,planar
SiOobliquely evaporated glass plates
areprepared (a
= 60°, 3
=
700
hi
andsputtered obliquely (p
=
40°
),
in theplane
of the direction e~ of the SiOevaporation,
and z(Fig. Ii, I.e., perpendicular
to theplanar
nematicorientation.
To
study
thedependence
of surface orientation on the erodeddepth,
we measure the surfaceprofiles.
Atypical
surfaceprofile
is shown infigure
8. Curves A and B representtypical
surface
profiles along
the chosen line inside thesputtered
track after and beforesputtering, respectively.
The vertical distance difference between these two curvesgives
thespatial
variation of the eroded
depth.
»
a)
'j
' ' I j
' ' ' ~ i
~f'~'j"~,~i ,'
~~-~~~~~~/,i'i'[i
ii~ ~'~ ~~ ~
"'l'ii~l~'l
~~~~~
~~ '~'"iii)(, 'j,i'i,1
~~~
~~~ "i_~'~~ ~~~~"'l~ ~l' ~',l
If'~
'°'S~~l
<'l'II, ~
~'~
II
(jj p
~~ ~~ ~~
~lj~ll
i)('I 1' ~-~~ "If ~
~-~ i l'l'/
' ' 'jy
Z ~) -~~~zj I
l'jj(( jjllli~~l'/,$ $j~i)i~'i~lj')'j~ j'~' e
~~)~~~~~~~$~j~~~~~ ~~'j~~
~
~
~lll ~l( i)/j'>i Ii Ii "'
x' Ii ' '~l j~j
Ill jl
'~ ' (j
b)
Fig. 9. a) Texture of a planar SiO oblique evaporated (n = 60°, 3
= 700
hi
glassplate sputtered
obliquely (p 40° ). when the optical
eigenaxis
makes theangle
~b=
0°, with the non-eroded
planar
orientation. b) Distribution of the director field
corresponding
to the texture shown in figure 9a.We now observe the
optical
texture of thecorresponding
nematicsample
shown infigure
9a.The
sample
isplaced
between crossedpolarizers,
and can be rotated. For eachposition,
the black appearance shows theregions
where the nematic molecules areparallel
orperpendicular
to the
polarizer
axes.Figure
9a shows for instance thesample
texture when these axes areparallel
to theedge
of thepicture.
Bothright
and left parts of thepicture
appear to be black.They
are howeverseparated by
a defect line(bright
on thepicture).
Theanalysis
withcompensator shows that on the
right
the moleculesalign vertically, although
on the leftthey
are horizontal.
Rotating
the stage, we can follow these orientationsby continuity.
Thecorresponding
distribution of the director field isplotted
infigure
9b. Theexperiment
shows that the director rotatesparallel
to the surface in two senses and do not tilt at all. This can beseen more
clearly
infigure
10. Thefigure plane
is theprojection
on the x-yplane
of the unitsphere
n~= I. The initial
planar
orientation isalong
x.Increasing
thedepth
of the erodedregion
makes the director n rotate towards b~along
y. Thepoint
P is a bifurcation of the orientation, similar to the one described in reference[17], although
there is no tilt of n in ourcase.
_,' ,~
.h' 0 8 t 'I,
"' /,"'
<~ -~-~ i~ f .,_'~.
,"~,_ ',, .., 0.6 i~ _.' ," _,~,,
~",
'- 1'', ~
,'
~
j. 'lo ~
,' '. '- ~i /,' _.' ',
". ~-'i', ~. / "
,"
l' "''~ ,'m' _." I 1'
/ j
'.
,'
~
x
-1
0-(
fi÷O.6.=,0 0 4~ D-E- Q~8"'[ '- / / ')"j"
,' ',',"" / j
.h I ,"' '-"'," -"'-" -", (~, ,'~
,' l -~'~ ,/ j
~' ~-~
'- '~_
~ ~
,' "' ~. ', -', P p
', '.
-' "-
,' )-
~' ' -~
'.,' -' " '" ,' '~
,', / ; ~
'/( ["
J "~ ,-j." ,.'"'
/ ,,~,"".
~i
Fig. 10. -Variation of surface orientation in two senses, starting from planar
(nflox)
for non sputtered SiO coating toward the ion direction b~ for the largedepth
eroded region.With reference to the
graph le.
g. shown inFig. 8)
and the observation of texture(e.g.
shown inFig. 9a),
we can determine thecorrespondence
between the surfaceprofile
and the differentzones of texture. In this way, the
dependence
of ~b on the erodeddepth
d is measured.Figure
I I shows the ~bid dependence
observed on sevensamples,
with the associated noise.~b increases
together
withd,
and saturates at 90° when d is over 200h.
Asa matter of fact, the
measurement of d cannot be
accurately
made(because
of various reasons, such as surfaceroughness,
diffusion of thefringe etc.).
The measurement error on d is about 20-50h.
According
to the symmetry, four domains should be observed in the nematicsample.
In thenon-sputtered planar region,
twin domains with same mean tiltangle
and different surface azimuthalangles
~b=
0° and ~b =180° may form in the
sample. They
areseparated by
N° I NEMATIC ORIENTATION ON SPUTTERED GLASS 69
1 (°)
o
«
«
. «
«
«
@ o
i,
/fi$$/(()~(i~~~~~')~i~'~~)'~'jl)~~
~fi~,,"",Qj'~'~<,"
ijj j<ijl
Q'~i"'~'),'i),'jlj'~~~[li,jlj('j'jl
/~,'~~~Q'~),/I
'j~ i~~,ji(,j<,jlj',i
/fii~~~/,'jil,'jj('j'l jljjijll,l~j
"-"~-~.m ~"~~~~~~~~)~~~~~)~)jj~l' ~~
~~~~~~~~ll 'jlj lij'l'j l~j
~~-
~-~~'-?~'~ ljj
~i~- ~~ -
till j'jl
ii jjjj-j~ -~$fllfil <',j jj ep
/- - i~/ jj
~f~l'~$"' l'ii ~l<'~l
~
~-~~/$Sf~~ jl,,"ij<ji X
'-~S~~/~)" j"lj'jl'jjj
~'/~~ll/ <'jj,I'
"Iill ill
$~$f~ lj'jljljljljl
b)
Fig.
12. al Nematic textureshowing
the disclination lines and points defects on the boundary between the non-erodedregion
and the sputtered track (x 40 ). b) Distribution of the director fieldcorresponding
to the texture shown in
figure12a.
After
sputtering,
the texture is observed and shown infigure
13a. Undermicroscope,
theeroded track can be located
only by
a series of marks made on the other side of theplate.
At theedge
of thesample,
the non-erodedregion
shows aplanar
texture (nalong
thex-axis). By rotating
themicroscope
stage, shadowfringes
move from theedge
of thesample
to the centre,where the black part shows a
homeotropic alignment corresponding
to the maximum erodeddepth.
This means that the surface orientationchanges progressively
whenincreasing
theeroded
depth. Although
ITOplates generally
favour aplanar
butdegenerate (undefined
WIN° I NEMATIC ORIENTATION ON SPUTTERED GLASS 71
~~i~/I)l~~)')')'i~')
j(jj~~~i~[~jl~ (~lj)'j
)~)l)j~)I))~j~j))) bP
$i~~/i~jj~ l~l~lj'i
jii[~~ jj j1 $
'
~ii(~~~l~~~(' I)' lj~'j
~
i)(l'~)lj/(l~l j~(j~'j
~
,,
°; ;.j/([,)/~ijjl(I j'jllj~'l
b)
Fig.
13. a) Texture of a planar SiOoblique
evaporated («= 60°. 3
=
300 h ) on ITO coated glass plate sputtered
obliquely
(p= 40° ). On the
right
side of the photograph the black region shows ahomeotropic
alignment (x 40). b) The distribution of the director field corresponding to the texture shown in figure13a.orientation
[6], they
tend toalign
moleculeshomeotropically
afterbeing
eroded. Around thehomeotropic
part, there is a narrow transition zone(about
100-500 ~Lm). It is worthnoting
that outside the transition zone ~bchanges
a little 20-30° ), but ohardly
varies(~
5°).
However,in the transition zone both ~b and o vary
sharply.
The distribution of the director fieldcorresponding
to the texture shown infigure
13a isplotted
infigure
13b. Since the width of the transition zone is muchlarger
than the thickness of the cell(~
8 ~Lm),
it isimpossible
for thecurvature elastic interaction from the
hybrid
texture to tilt molecules. Various measurements of surface orientation areplotted
on the unitsphere
n~=
I,
as shown infigure
14.Experimentally
we observe that the azimuthal
angle
~b canchange
in two senses, clockwise and coun-terclockwise. From symmetry, surface orientations associated with both rotations of the
director should be
equivalent.
Here weonly
take the absolute value of ~b infigure14
tocompare the results of measurements. From this
figure,
we can see that ~bapproaches
90° and o goes to 0°. The director n tends tochange
its orientation from the non-erodedplanar
texture(along x-axis)
to theplane
ofsputtering (y-z plane)
and normal to the surface. Themeasurements are
reproducible, especially
when both ~b and(90°-
H) are notlarge.
Forlarger
values of ~b and
(90°- o),
theexperiments
show some datascattering.
In fact suchscattering
is not difficult to understand. We note that the transition zone shown infigure
13a is narrow andinhomogeneous.
As a result it is not easy to measure ~b and o veryaccurately. Besides,
the surfacemorphology
in differentsamples
may also lead to a different variation of surfaceorientation. In
spite
ofthis,
we still have agood empirical
law of variation of nematic surface orientation. Since ~b can twist in two senses, we suppose that a bifurcation similar to thatreported
in reference[17]
mayprobably
be observed, whichdepends
upon thepreparation
ofsamples.
In case I and2,
no tilthappens
for thesputtering
on the SiOevaporated glass plates
without ITO
coating.
The tilt fromsputtered
ITOlayer
is not yet understood. More work has to be done toclarify
thesepoints.
o
-i
~ ~ -o.5
~
~ ~p
o $
~p
i i
X y
Fig. 14.
Spatial representation
of the surface director on the unit sphere, for the figure 13b nematic orientation.Conclusion.
We have shown that an
oblique sputtering
with Ar+ ion-beam on solid subsuates has a strong influence on the nematic surface orientation. For anisotropic
SiO substrate, thesputtering
induces a pure
planar
orientation without tiltalong
theprojection
of the localvelocity
of ions at the surface.Sputtering
atgrazing
incidence creates the best uniformplanar
texture. IonN° NEMATIC ORIENTATION ON SPUTTERED GLASS 73
sputtering perpendicular
to analready planar (SiO oblique evaporated) glass plate
results in a continuous twist in two senses withouttilting. Increasing
the erodeddepth
from 0 to 200h,
we
obtain
symmetrical planar anchoring
with local orientationgoing
from the initialplanar
SiO to the 90° twisted ionvelocity projection
on the surface. Forplanar
SiOplates,
coated aboveby
an ITO electrode, the
sputtering
induces both twist and tilt which also vary whenincreasing
the erodeddepth. Although
we do observe thesymmetrical
left- andright-handed
twists, we have not been able to demonstrate that these surface orientations were twofolddegenerate.
Acknowledgments.
The authors wish to thank M. Boix for
preparation
of the SiOevaporated plates,
Mr. Rousse forhelp
insputtering,
and Prof. Blaise and Prof.Martinot-Lagarde
for fruitful discussions.Z. M. Sun was
supported by
a contract n 179909 from the French C.N.R.S.References
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