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Origin of the incommensurate phase of quartz : II.
Interpretation of inelastic neutron scattering data
M. Vallade, B. Berge, G. Dolino
To cite this version:
M. Vallade, B. Berge, G. Dolino. Origin of the incommensurate phase of quartz : II. Interpretation of inelastic neutron scattering data. Journal de Physique I, EDP Sciences, 1992, 2 (7), pp.1481-1495.
�10.1051/jp1:1992223�. �jpa-00246634�
Classification
Physics
Abstracts63.20D 64.70R
Origin of the incommensurate phase of quartz
:II. Interpretation of inelastic neutron scattering data
M.
Vallade,
B.Berge
and G. DolinoUniversitd
Joseph
Fourier (Grenoble I), Laboratoire deSpectrom£trie Physique
(*), BP 87, 38402 Saint-Maxtin-d'Hdres Cedex, France(Received 25 November J99J, accepted in final form ii March J992)
Rksl~md. Los rdsultats de
l'investigation
par diffusionindlastique
des neutrons des modes de bassefrdquence
du quartz p, ddcrits dans l'articlepr6cddent
[Ii, sontinterpr6tds
h l'aide de deuxapproches
diff6rentes : I) un modkleph6nom6nologique,
directement issu d'unddveloppement
du type
Landau-Ginzburg
del'6nergie
libre ; cc modkle n'est valable que pour lapanic
du spectre relatif auxphonons
de grandelongueur
d'onde, mais il perrnet d'6tablir une connexion aisle avec les donndestherrnodynamiques
it) un modmemicroscopique
dedynamique
de r6seau, qui estune extension du modme de Grimm-Domer (modkle h t6trakdres
rigides)
on montre que lesprincipales caract6ristiques
du spectre desphonons
de basseft6quence,
et enparticulier
l'amollissement d'un mode3~
h un vecteur d'onde incommensurableprks
du centre de zone, peut Etrecompris
par uneanalyse
des mouvements de t6trakdresSi04
Presquerigides.
Abstract. The results of an inelastic neutron
scattering investigation
of thelow-frequency
modes of p quartz, described in the
preceding
paper [I], areinterpreted using
two differentapproaches:
I) aphenomenological
modeldirectly
derived from aLandau-Ginzburg
typeexpansion
of the free energy ; this model isonly
relevant for thelong-wavelength
part of thephonon
spectrum but it allows an easy connection withtherrnodynamical
data ; it) amicroscopic
lattice
dynamical
model, which is an extension of the Grimm-Domer model ; it is shown that the mainproperties
of thelow-frequency phonon
spectrum and, inparticular,
thesoftening
of a3~
mode at an incommensurate wave vector close to the zone,center, can be understoodby analysing
the motions ofnearly rigid
Si04 tetrahedra.I. Introduction.
The various
physical
mechanismsleading
to the occurrence of incommensurate(inc) phases
in dielectrics have been an active field of researchduring
the recent years[2].
From aphenomenological point
ofview,
incphase
transitions in dielectrics have been related to the presence of the so-called « Lifshitz invariant »j3] (which
canonly
be found when the order(*) Assoc16 au C-N-R-S-
parameter has several
components)
or to a «Lifshitz,type
invariant»[4] (when
the order parameter iscoupled
to anotherthermodynan~ic variable).
On the other hand the
microscopic
mechanismsleading
to the existence of an incphase
have been
clearly
elucitadedonly
in a restricted number of materials : forbiphenyl,
thecompetition
between intramolecular and intermolecular interactions has been invoked toexplain
the occurrence of a modulated structure[5].
InNaN02
the incphase
isthought
toresult from the
coupling
oflarge amplitude
reorientations ofN02
groups with thetranslational motion of Na
[6]. Microscopic
models have also beenproposed
for some other systems e,g.,K~Se04 17], propylammonium
tetrachlorometallates[8].
The relative
simplicity
of the quartz structure makes attractive thestudy
of the mechanismleading
to the incphase existing
near the a-p transition in this material[9]. According
to thephenomenological theory
ofAslanyan
et al.[10, iii
the occurrence of an incphase
in quartz typecrystals
would result from a «gradient coupling
» between the elastic strains and thegradient
of the order parameter 1~ of thea-p
structural transition. This kind ofcoupling corresponds,
in the soft-modepicture,
to an interaction between anoptical
mode and an acoustic mode close to the Brillouin zone-center as shown in reference[12].
Astriking
illustration of the
physical meaning
of this kind ofcoupling
inquartz-type crystals
isprovided by
the so-called «exaggerated gradient
method » of Heine and Mc-Connell[13].
The order parameter 1~ of thea-p phase
transitioncorresponds mainly
to altemate rotations ofSi04
tetrahedra around axes
lying
in the basalplane
of thehexagonal
lattice. Itcorresponds
to azone center
optical
mode. In the «phase
1~ can take twoopposite
values(according
to the twopossible signs
of rotation of eachtetrahedron), leading
toDauphind twinning.
A very thin domain wall between these twins(as represented
inFig, I) corresponds
to a strong(and probably quite exaggerated) gradient
of 1~ but one caneasily
see that deformations of the unit cell(-I.e. strains-)
are present in the wall.Furthermore,
thecomparison
betweenfigures
la and 16clearly
showsthat, according
to the direction of thegradient
of1~, the strains are either pure shear
(VI~ along
theOy
typedirections)
orpurely compressive
strains(VI~ along
the Ox typedirections).
Inspite
of theirqualitative
character thesepictures
are of somehelp
tounderstand the mechanism
leading
to the incommensuratephase
in quartz: the actualgradient
of1~ which is present in a
long-wavelength
incmodulation, although
much smaller than that described infigure I,
is associated with strains of differentkinds, according
to itsdirection. One is then
logically
lead to ascribe theorigin
of the incphase
to aninterplay
between two modes of atomic
displacements
:optical,like
and acoustic-like. A controverse tookplace
some years ago about the relativeweight
of the two modes[14].
In a recentpreliminary work,
Gouhara et al.[15] reported
on anX-ray
determination of the inc structureand
they
confirmed that the modulated atomicdisplacements correspond
to amixing
ofacoustic and
optical
components(with
alarge
contribution of the acousticone).
As the incphase
arises from thehigh
temperature pphase through
a 2nd ordertransition,
thedynamical
critical fluctuations above thep-inc
transitionpoint T,,
must also involve amixing
of acoustic and softoptical phonons.
Thispoint
wasalready
evidenced inpreliminary
inelastic neutronscattering experiments [16]
and a more detailedinvestigation,
described in thepreceding
paper
[Ii, brings
astronger support
to thispoint
of view. The purpose of this paper is an attempt togive
aquantitative interpretation
of the temperaturedependence
of thelow-energy phonon
branches in thep phase
and thus to propose a mechanismleading
to the incphase.
The
analysis
will be made at two different levels :.
First,
as the inc wave vector isonly
a small fraction of thereciprocal
lattice unit vector(qo>0.03a*),
a continuous-mediumapproximation
is relevant. We consider asimple
phenomenological theory
which follows theoriginal
model of reference[10] by considering
only
a softoptical
mode(SM)
and acousticphonon modes,
with small wave vectors. The mainx x
a)
b)Fig, I.
-Exaggerated
gradient
picture of
aDauphind
twin wall inThe
figure
thearrangement
of thecomersharing Si04 tetrahedra,rojected on the (0
0
) lane : a) wallerpendicular to the Oy axis.
The
radient of the orderparameter
(v,u~ )
is associated with aunit
cell. b)Domain wall erpendicular to
the
Ox axis. The gradient (v~u~) is associatedwith
acompressive strain
of
the unit cell. In figure la the two twins have beentranslated
along
order
deformed.)
interest of
thisapproach
isto
provide an easy connectionmacroscopic operties,
Sect. 2).
. In a second step, an ttempt
is
adeto
interpret theof the
modes over
the
wholeBrillouin zone, by considering
a
icroscopic model. As a
starting point
for this
study, we use theGrimm-Domer model
[17,
18] which assumes thatfrequency ptical modes are those hich leave the Si04 trahedra
The
methodused to find these modes is
described in
ection 3.A
impleBom,von rman
force
constants
and a uasi-harmonicapproximation)
is hen oposed insection
emarks.
2. henomenological radient
coupling model.
As usual
in the
soft-modetheory of
phase
transitions, the phonon requencieswithin the
pproximation,
using
an effective otential energywhichhas
thesame
form
as the andau-Ginzburg freeenergy.
Inthe
high emperaturep phase
ofhas already
been shown that the potentialenergy
correspondingto
the long velengthsoft
optical phonon
mode
andto
In this
expression ~(q)
is theamplitude
of theuncoupled soft-optical
mode with a wave vector q, andwj(q, T)
is thecorresponding frequency.
Close to the Brillouin zone center weassume that :
wj(q, T)
m A
(T To)
+gq~
+hq~
U~~~(q), UT~~(q)
andU~~(q)
are theamplitude
of the two transverse acoustic modes(polarized respectively
in the(0 01) plane
andperpendicular
to thisplane)
and thelongitudinal
acoustic mode. Theuncoupled
acoustic modefrequencies
are :W(Ai(~)
~j~ ~~ W(A2(~)
"
~ ~~, W/A(~)
~
)~ ~~
(p
=volumic mass,
C~~ = elastic
constants).
The bilinear
coupling
between1~
(q)
andU~A (q)
orUTA~(q),
inequation (I) corresponds
to theLifshitz-type
invariant introducedby Aslanyan
andLevanyuk j10].
This term exhibitsanisotropy (since
itdepends
on theangle
~b between q and the twofold Ox axis of thehexagonal p phase).
One can note that for4
= 0
(mod ar/3)),
~(q )
isonly coupled
with the LA mode, whereas for4
=
(ar/2) (mod (ar/3)),
1~(q)
isonly coupled
with theTAT
mode.This agrees with the «
exaggerated gradient picture
» offigure I,
since q isalong
thegradient of1~.
A bilinear
coupling
between1~(q)
andUT~~(q)
is also allowedby
symmetry but it isproportional
toq~ and,
for small q, it can beneglected.
A similardescription
of the interaction between a softoptical
mode and an acoustic mode hasalready
been usedby
Axe et al, toexplain
the anomalousdispersion
of acoustic branch inKTaO~ j19].
In order to describe the finite linewidth of the
phonon
groups, adamping
y has to be introduced for the softoptical
mode(the damping
of acousticphonons
isproportional
toq~
and it can beneglected
in the small wave vectorlimit).
Thecoupled
modecomplex frequencies
are then obtained from the secularequation
:ml
w y w ~) aq~ cos 3#
aq~ sin 3#
det
aq~cos
3# (w/~ w~
0= 0.
(2)
aq~
sin 3#
0(w(A w~)
For q
along
the 3 lines( ii
00)
directions of thereciprocal lattice)
cos(3 #)
= 0 andequation (2)
reduces to a 4th orderpolynomial equation
for w.Explicit
solutions canonly
beobtained in the limit y
= 0 :
ml (q)
=
iwl(q)
+WlAi(q)i
±
~/iwl(q) WlAi(q)i~
+ 4a~q~j (3)
The lower branch
w_(q)
exhibits a minimumequal
to 0 at thep,inc phase
transitiontemperature
T =T;
for an inc modulation wave-vector q = qo.Ti
and qo are relatedby
the relations :A
(T~ To )
= 1/2£
g
q(
=
hq( (4)
66
Since h is assumed to be ~
0,
an incphase
canonly
occur when g <(pa~/C~~).
When y is
non-vanishing, equation (2)
must be solvednumerically.
The solutions behaveessentially
in the same way as in the y= 0 case except that both
frequencies
w~ are nowcomplex,
the modecoupling producing
a transfer ofdamping
from the soft-mode to the acoustic mode, as observed in Brillouinscattering experiments [12].
Most of the
input parameters
of thismodel,
have been deducedby fitting
the inelasticneutron data of
[Ii
obtained at thehighest temperature (T= Ti +400K)
in the range[q[
< 0.I a*along
the 3 direction.(This
limited range of wave-vector was chosen ratherarbitrarily,
but it appears to be an upper limit ofvalidity
of the qexpansion
used for theuncoupled frequencies).
The coefficient h(proportional
to(Tj To) according
to(4))
wasmuch more
sensitively
deterJnined from the value of qo and from the spectrum at TT,.
The elastic constants Cii and
Cm
were taken from ultrasonic data[201.
The numericalvalues of the
parameters
are summarized in table1[211.
Thedispersion
curvesalong
3((f00))
directions and A directions((f to))
for thetemperature
range(T;
< T< T
; + 400
K)
were then calculated with this set of parameters. The fit wasimproved by allowing
a lineartemperature dependence
of thedamping
coefficient y(from
0.5 THz atTi,
to 0.7 THz atTi
+ 400K).
Ageneral picture
of thedispersion
curves is shown infigure
2.The main conclusions which can be drawn from a
comparison
of calculated andexperimental
curves are thefollowing
:I)
The overall agreement is correct. Inparticular
thestrong anisotropy
of the soft modes and of theTAj
and LA modes in the basalplane
isfairly
wellreproduced
with a minimum ofadjustable parameters. Neglecting
thecoupling
between the softoptical
mode with theTA~
mode isjustified
since thedispersion
curve of this mode is almostisotropic
and exhibitsno anomalous
dispersion.
ii)
The maindiscrepancy
concems the value of theparameter Ti To (calculated
to be0.7K whereas the
experimental
value is5±2K). Any attempt
toadjust Tj- To
to itsexperimental
value results in astrong
increase of the value of theparameter
h(according
toEq. (4))
which leads to a curvature of thedispersion
curve at T= T~
by
far too steep for qo < q < 0, I. Thisdiscrepancy
may arise from someinadequacy
of the mean fieldtheory
and(or)
of thequasi,harmonic-approximation.
Let us recall that an anomalous temperaturedependence
of some elastic constants and of the thermalexpansion
aboveTi [221
shows theimportant
roleplayed by
fluctuations combined with strong anharmoniccouplings.
Unfortu-nately, owing
to the limited resolution and to thedifficulty
of a reliable deconvolution of our neutronscattering data,
it seemsmeaningless
at the present time to introduce additionalfitting parameters
in the model(such
as non-classical criticalexponents).
On anotherhand,
it is noticeable and somewhatpuzzling that,
inequations (4),
the termspa~/Cm
and gnearly
Table I. Parameters
of
thephenomenological
modelof
section 2(with JFequencies
in THz and wave vectors in unitsof
thereciprocal lattice).
~~~
= 350
(C11
= 166.5 x
llfN/m~)
P
~~~
=
120
(Cm
=
57.075 x
llf N/m~)
P A
= 0.0025 g
= 140
a =131.2 h =1600
y =
0.5(T/To) To
= 850 K
T; To
= 0.74 K qo =
0.033 a *
/
~ 2
o
0
0.00 .02 .04 .06 ,08 .10
a) b)
Fig.
2.-Dispersion
curves of theinteracting phonon
branchesaccording
to thephenomenological
model of section 2. The lines are calculated with the set of parameters of table I and the
points
areexperimental
values(Ref. [I]).
al Wave-vectoralong (I
00)
direction(3
orOy).
b) Wave-vectoralong (I
2 I0)
direction (A or Ox). (~ D) T T~ = 0.75 K, (. . .) T T, = 12 K, (... 6)T T, = 50 K, (~ m) T T, = 100 K, (- o) T T~ = 400 K.
cancel each
other,
I.e. the constant g is close to the threshold value for which an incphase
canoccur.
(This
is related to the small range oftemperature (1.5 K)
over which the incphase
exists,
and to the small value of the inc wave vectorqo).
This closecancellation,
which appearsas a pure coincidence in the
phenomenological theory,
can be better understood in thelight
of themicroscopic
model described in the next section.3.
Rigid
tetrahedra modeanalysis.
In this section we present an
attempt
to derivesimple physical
arguments which can shedsome
light
on the existence of an incphase
inquartz, by considering
thepeculiar
structures of this material. Inprinciple
the occurrence of the incphase
should be foundby solving
the fulldynamical problem (27 phonon branches) using
anadequate
force constant model. Several models of this kind have beenproposed [23]
most of them are relative to a-quartz but someof them also concem
p-quartz [24, 25].
It is notsurprising
however that such models do notpredict
the incinstability,
because the characteristicdip
on the lowestphonon
branch isexpected
to be atiny
detail in the fullphonon spectrum,
and its existence is related to a subtlebalance between weak force constants. In
addition,
even if a model were able to exhibit thisdip,
it wouldprobably
obscure thephysics
underheavy
numerical calculations. Therefore itseems to be more advised to concentrate our attention on the lowest energy
phonon
modes.As
already
oftennoted, quartz
is built of ratherrigid Si04
units which share a common comer(see Fig. 3).
The covalent character of the SiObonding explains
thisrigidity
and therelatively
open structure of
p
quartz.Megaw [26] analysed
thea-p
transition inquartz
as the result of rotations ofrigid Si04
tetrahedra. This idea was thendeveloped by
Grimm et al.[17]
who tried to relate the thermalexpansion
near the transition to these rotations. The samej,
5 6
I.o
7
y3
Fig.
3.-Projection
of the unit cell ofp-quartz
on the basalplane.
(o) oxygen atoms, (o) silicon atoms.assumption
ofrigid
tetrahedra was later usedby Boysen
et al.[181
toanalyse
the lowfrequency part
of thephonon
spectrum of a andp quartz
thatthey
have measuredby
inelastic neutronscattering.
The mainassumption underlying
theiranalysis
is that intertetrahedron force constants are smaller than intratetrahedron ones. Therefore the lowest energyphonon
modes must
correspond
tonearly rigid
motions ofSi04 units,
if any motion of this kind is allowedby
the structure. As a matter offact,
theseparticular
modesmerely correspond
to the« extemal modes »
widely
used in the context of latticedynamics
of molecularcrystals.
In thecase of covalent framework
materials, however,
severetopological
constraints areimposed
onthe motion of
rigid
moleculesby
the fact thatthey
share a comer and the existence of« extemal modes » cannot be taken as
granted
in thegeneral
case. Theanalysis
ofBoysen
et al.
[18] only
concemed the existence ofrigid
tetrahedron modes(RTM)
at somehigh
symmetry
points
in the Brillouin-zone(r
andM).
In apreceding
paper[16]
we gave the results of a moregeneral analysis
valid for anypoint
inside the Brillouin zone. Since no detailwas
given
in that paperconceming
the method used to derive theseRTM,
and since this method isthought
to be of somegeneral
interest topredict
the existence of soft modes in frameworkcrystals,
wegive
in thefollowing
a morecomplete description
of theprocedure.
Let us consider a 3-dimensional framework of N identical comer
sharing
molecular units withp comers shared. The total number of
degrees
of freedom is 6N(3
translationsT~~ and 3 rotations
R~~ (per
unitI).
The threedisplacements
of each atom sharedby
two units(I
andj)
can beexpressed
as a function of both the(T~,
R~ and the(T~, Rj).
There are then 3 relationslinking
the motions of two connected units : thesecompatibility
relations will becalled «constraints». The total number of constraints in the system is
clearly ~~~
2
(neglecting
surfaceeffects)
since(Np/2)
atoms are shared. For small atomicdisplacements
these ~
)P
constraints lead to asystem
of ~~P
homogeneous
linearequations
with 6N 2unknown
(T~~
andR~j).
For tetrahedral units(as
inquartz)
p= 4 so that the number
of equations
is the same as the numberofunknown.
This case isparticularly interesting
since non-trivial solutions
only
exist underspecial
conditions.Using
a harmonicapproximation,
theequation
of motion can be writtenusing
Fourier componentsT~;(q)
andR~;(q)
where the index I denotes now the molecular unitsbelonging
to agiven
unit cell(I
= I to
n)
and q is avector of the lst Brillouin zone
(BZ).
For each q there are then ~ ~Pequations
with fin 2complex
unknownT,(q)
andR,(q).
Let us consider thep
quartz structure(with
theassumption
ofperfect Si04
tetrahedra for the sake ofsimplicity).
There are three(Si04)
units per unit cell(see Fig. 3).
The 18 constraintscorrespond
to thedisplacements
of 6 oxygenatoms O~ = 4 to
9) (see
tab.II). They correspond
to asystem
of 18homogeneous equations
in which the wave vector q appears
through
thephase
factorse;.
For q at ageneral position
inthe BZ there are no non-trivial
solutions,
but solutions exist when q lies in the(0
01) plane
or
along
the[0
0Ii
directions(and
alsoalong particular
lines on the BZedge).
Insolving
thesystem
ofequations,
it is convenient to usesymmetry adapted
combinations ofT,(q)
and R~(q)
which transformaccording
to irreduciblerepresentations
of the small group of the waveTable II. Atomic
displacement
components u~~(in
the(x,
y,z) reference JFame)
as ajknction of
the translation and rotation componentsof
theSi04
units,for rigid
tetrahedron modesofwave
vector q R(
e)
is the matrixcorresponding
to a rotationofangle
e around the z- axis.T~,
andR~;
are translations and rotations components in the local(x;,
y;,z,) reference frame (see Fig.
3).
The setof18 equations
relative to the oxygendisplacements
determine thepossible
RTM with wave vector q(coordinates
11~D.Si ui
~
=
Ti
j2arj~
~u2«"R~p ~
2pj4arj~
"3«"R«fl $
3fl~
U4a ~
(Tl
~~l
X Pa)a
"
°3 ~afl ~) (T3
~~3
X
Pd)fl
115 a " R
«fl
~)
1'~2 +~2
XPb )fl "
°3 ~afl ~) (~3
+~3
XPc)fl
"8
a "
~ap ~) (T3
~
~3
XPa)p
"°2 ~afl ~/
1'~2~
~2
XPd)p
"9
a
"
(Tl
~~l
XPb)a
"
°2 ~ap ~) (T2
~~2
X
Pc)fl
91 = exp(2 ar(7~
-
)) ; 9j
=
xp(2 ar(7~ <))°2
"exp(2 iar(- -
~+
<)); 93
" XP(217r(Ivector q, so that the system
splits
intoindependent sub,systems corresponding
to eachrepresentation.
The various solutions are summarized in table III. In this table is also indicated the character of the RTM when q goes to zero. Three different cases are found :I)
the RTM behaves as a pure translationaldisplacement
and is called acoustic(A), it)
it behaves as a pureoptical
mode(O) (center
of massinvariant), iii)
it is amixing
of acoustic andoptical components (A+O).
At the BZ centerl~
it is clear that the 3 uniforJn translations leave theSi04
units undeforJned so thatthey
are RTM(labelled Qx(r~), Q~(r~)
andQ~(r~)).
There exists an additional solutionQ(r~)
whichcorresponds
to theorder
parameter
1~ of thea-p transition,
since it involves altemate rotations of theSi04
around the
Ox-type
directions.Compatibility
relations can be foundby looking
at theq - 0 limit
along
various directions of thereciprocal
space. For qalong [0
0fl (A line),
onehas 3 RTM
belonging
to differentrepresentations
A~, A~, A~ and :Q(A4)
-
Qx(r6)
+joy(J~6)
Q (A6)
-
Qx(r6) ioy(J~6) Q (A2)
-
Q (r3)
The former two are associated with the TA modes
polarized
in the(0
01) plane
and the latter is the softoptical
mode.Table III.
Rigid
tetrahedron modes with wave vectorsalong
the3,
A and A directions.T,,
andR,;
are the(unnormalised)
translation and rotation components relative to the I-thSiO~
unit
(see Fig.
3).
Thecorresponding
atomicdisplacements
can be calculatedusing
table II. In the last line is indicated the characterof
each RTM when q goes to zero(O
=
optic,
TA=
transverse
acoustic).
«=
art
; y = "< y'
=
"
((
I)
;y"
=
"
(<
+1).
3 3 3
~l zg oo) A(oon
Txi '2 cos a a. cos a
Ty1 °
~~2m $11 4cosZy)slay T~~ I(d3+1)sin a
Rxi 2 cos a
4COS~Y'l~coSy
RyI 0 ~
xe2i" "(4C°S~tI)slay
R~j 2i sin a
~ sinix Tx2
as Q(62) Q(62)
~'~
~~~~ ~'~
~ y ~
Tz2 U
l(4
cosla-I) sinaRy2 xe""
x ~lu sina
x
e~"
Rz2
C°S" ~~~
xe-2iu
xe.2iu e~4iy
Ry3 -Ry2 xe-2>a x e-4.y
Rz3 0
q ~ o ~6) lox+ ;Qy) ~6)
When q is
along
ageneral
direction in the(001) plane, only
one RTM is found and it behaves as a pure TA modepolarized along [0
0Ii (the
mode labeledTA~
in Sect.2).
Noadditional RTM is found in the
particular
case when q liesalong ii I 0) (A directions),
butone extra RTM is
actually
found when q liesalong ii
00) (3 directions).
This lastmode,
notedQa(3~),
appears to be the mostinteresting
one. As a matter of fact it is theonly
RTM which exhibits a « mixed » character(A
+O)
:Qa(32)
- 0.6
Q (1~3)
0.8Qx(1~6) (The
modes have been normalizedusing
:£
m;[u~~(q)[~
=
l.)
i, a
This
singular
behaviour deserves some comments, since actualphonon
modes arealways
pure acoustic or
optical
modes when q goes to zero. This «hybrid
» mode is a consequence of the infinite force constants which areimplicitly
assumed in therigid Si04
tetrahedronhypothesis.
Modes which are not RTM have an infinitefrequency.
This is the case, inparticular,
for the acoustic modes(at
q #0)
which are notRTM,
such as the LA mode and theTAT
mode. Thecorresponding dispersion
branches have an infiniteslope
at q # 0 forperfectly rigid
tetrahedra. Thecrossing
of this acousticphonon
branch with anoptical
modeoccurs
right
at the rpoint,
andhybridization
of acoustic andoptical
modes takesplace
atvanishingly
small q.(With
a more realisticassumption
of finite intra tetrahedron force constants, thecrossing
would occur at finite wave vectors and thesingular
behaviour would be removed see below Sect. 4-).
It isinteresting
to note that thistype
of behaviour isquite
reminiscent of the TOphonon-photon
mode interaction in thepolariton region
:assuming
aninfinite
light velocity
results in a « mixedphoton-phonon
» excitation at q =0 which leads to the LO-To
splitting.
Thissingular
behaviourdisappears
when a finitelight velocity
is takeninto account.
An additional
interesting
feature of theQ~(3~)
mode is found when one considers the meanchange
Ad of the(Si-Si)
distance for this mode. As shown infigure
4 Ad vanishes at r and at the BZedge point
M and it isquite
smallalong
the whole 3 line for thisparticular
mode.Since the Si-O-Si force constant is known to be the
strongest
among the intertetrahedron force constants[2, 5]
one can expect theQ~(3~)
mode to be flat and softalong
the whole 3 line.Let us summarize what kind of
qualitative
conclusionsconceming
thephonon dispersion
curves of
p quartz
can be inferred from ourassumption
ofrigid
tetrahedra :I)
the existence of threelow-lying
branches(two
TA and oneoptical)
for qalong [0
0fl (A line)
it)
for qalong if
00) (3 lines),
a very soft and flatbranch, corresponding
to a stronghybridization
of anoptical
and an acoustic(TAj)
components nearl~
and amoderately
lowfrequency (TA~)
branch ;iii)
for other directions of q in the(0
01) plane,
amoderately
soft(TA~)
branchroughly isotropic
aslong
as q lies in thisplane.
A
comparison
withexperimental
data[Ii
shows that thesepredictions
areessentially
correct.
FurtherJnore,
inelastic neutronscattering
structure factors can be calculated for the variousRTM. The results
conceming
the zone-center soft-modeQ(r~)
and the soft-branchQ~(3~)
are shown infigure
5. It isstriking
that thelargest
calculated structure factors are foundalong
the « fourthhexagon
», inagreement
with thelarge
scattered intensities observedalong
these directions[27].
The RTM
analysis provides
us with aqualitative explanation
of the mechanismleading
to an incphase
; theQ~(3~)
mode possesses the twokey
features which arerequired
for theAd
z ' /
2c '
' / /
~ //
A
r zFig.
4.- Mean relative change Ad of the Si-Si distance for the variousrigid
tetrahedra modes considered in the model of section 3. Ad is definedby
Ad=
i<J) jj
[(1~~ -1~~),r~~]~)~'~ where 1~~ is the (norrnalised)displacement
of the I-th silicon in the mode andr~~ the unit vector
along
theequilibrium
Si- Si direction. (Ad for the shear modeQc(3~)
is alsorepresented
using a dashed line.)) ) £ L
IQ, ~ .-.--"l«<i<11]ibjjjjjl«>"-"..-zJ.-
~ JL
Q Q S J L
L Q Q 7
$ 4
Z
L /
IQ'
L
IO.
ii, oi 12,o) 13, oi 14, o) 15,o)
Fig.
5. Inelastic structure factors calculated with the atomicdisplacements
of theQ~(3~)
mode (Tab. III). The size of the bars isproportional
to the squared modulus of the structure factors. The circles are relative to the zone-center optic-mode Q(r~).
Maximumscattering intensity
is found along the «4thhexagon»
in agreement withexperimental
observations. (Thefigure corresponds
to the f= 0 strate of the
reciprocal space.)
occurrence of a modulated
phase, according
to ourphenomenological approach
: a flat softdispersion
branchalong
3(g small)
and alarge SM-TAT hybridization
at small q(gradient coupling
coefficient alarge).
The ratio r of theoptical
modecomponent
to the TA modecomponent
is r= 0.75 in our model and it can becompared
with the ratio of thecorresponding
staticdisplacements
in the incphase recently
determinedby
Gouhara et al.[15]
(r
<0,15).
It is noticeable that all the above conclusions have been deduced frompurely geometrical considerations,
without anyadjustable parameters.
In order to be a bit morequantitative
one has to choose aspecific
force constant model.4. Lattice
dynamical
model of fl quartz within thenearly rigid
tetrahedraapproximation.
To follow on the lines of the
analysis
of thepreceding section,
we shallattempt
a calculation of thedispersion
curves ofp
quartzby assuming
almost undeformableSi04
units. As we aremainly
interested in the lowestfrequency phonon branches,
we do nottry
todiagonalize
the full 27 x 27dynamical
matrix but we assume that it can be truncated to a 4 x 4 sub-matrixcorresponding
to the lowest energy modes(acoustic
and softmodes).
Such anapproximation
is better near the Brillouin zone center
(where
these modes havefrequencies
much lower than othermodes)
than near the zoneedge
wherethey
arerelatively
close to the hard modes. Ouraim is to
keep
a maximumphysical transparency by introducing
the minimum number offitting parameters.
The set of modes chosen to write the 4 x 4dynamical
sub-matrix includes the RTMcomplemented by
non-RTMpurely
acousticcomponents.
For qalong
A the 3acoustic modes and the soft mode
belong
to different irreduciblerepresentations.
The two TA modes and theoptical
mode are then the RTM of table III ;only
one LAcomponent
should have to beadded,
but since itbelongs
to the irreduciblerepresentation Ai
it does notcouple
with the
previous
modes and it is of no interest for our purpose. For qalong 3,
one LA component(with
symmetry3j)
and oneTAT component (with symmetry 3~)
should be added to the two RTMQ~(3~)
andQ~(3~).
One must note that there is alarge
arbitrariness in the choice of the non-RTM modes sinceonly
their behaviour close to q = 0 is well defined. A reasonableguide
inbuilding
these modes is to select those whichkeep
the Si-O bondlength invariant,
since thecorresponding
force constant isby
far the strongest one[25].
Unfortu-nately
thisprescription
is not sufficient touniquely
define them. One hasfound, however,
that theshape
of thedispersion
curves does notdepend
very much on aparticular choice,
at least in thevicinity
of the rpoint (which
is the mostimportant
to discuss the incinstability).
The force constant model we have chosen, is of the
simple
Bom,Von Karman central forcetype,
as thatrecently
usedby
Bethke et al.[25]
to fit the wholedispersion
curves ofp
quartz.One considers the interactions between 5 different kinds of atom
pairs
:(Si-O), (O-O)i, (Si- Si), (O-O)~
and(O-O)~.
The former two areintratetrahedral, nearest-neighbour
interactions.The other three are intertetrahedral interactions
((O-O)2 corresponds
to interactionsbetween oxygen atom
pairs
like(04-06)
and(04-O~)
bothseparated by
a distance~ ~
(O-O)~
to interactions between atompairs separated by
~ where a is~
~
~/~
~
/~
the lattice
parameter).
There are then 10 force constants
(5 longitudinal (L
and 5 transverse(T)
forceconstants).
According
to ourapproximation,
L(Si-O)
is considered to be infinite. The other two strong force constants L(O-O )i
and L(Si-Si)
which are best determined fromfitting
the hard modes have been fixed to values close to those foundby
Bethke et al.[25],
Theequilibrium
conditionimposes
one relation between the 5 transverse force constants so that 6independent
force constants are left asadjustable parameters.
Thedispersion
curves for qalong
3 have beenfitted to determine these parameters. As shown in
figure
6 a shallowdip
can be obtained near qo =0.035 a*
along
the lowest 3 branch.(In
Ref.[25]
thisdip
couldonly
bereproduced by introducing
an ad hocphenomenological coupling
between the SM andTAT modes.)
In order toreproduce
thetemperature dependence
of themodes,
it was found sufficient to allow for asmall linear
change
of the force constants(mainly T(Si-Si) (cf.
Tab.IV)).
Asexpected,
theTA~
mode is found to beonly slightly coupled
with the other3~ modes,
so that thedip
close toT;
ismainly
due to the interaction of the RTMQ~(3~)
with the pure acoustic componentQ~(3~),
as assumed in thephenomenological theory. Furthermore,
theeigenvector
of thedynamical
matrix relative to the lowest branch isquite
close to the RTM « mixed » modeQa,
for any qlarger
than 0.005 a * Inparticular
at the inc wave vector theeigenvector Q
is :Q
=
[0.96 Qa,
0.27Qcl
/
~ o II
~ i
/~ _--, , O/
~ i
/~
/
, / /
y/ /~
' /
~
/~
' /
"
O o
u
~ u
0 ° °
A r Z 0.00 .02 .04 .06 .08
a) b)
Fig.
6.Dispersion
curves of the lowest energyphonons
of p quartzalong
the 3 and the A directions of thereciprocal
space. The lines are the results of the« nearly
rigid
tetrahedron model» with the force
constants of table IV. The
points
areexperimental
values (Ref. [I]). (~ D) TT,
=
0.75 K, (... 6)
T T~ = 50 K, (- O) T T,
= 400 K. a) Dispersion curves along the whole Brillouin zone. b)
Enlarged
view of thevicinity
of the incommensurate wave-vectoralong
the 3 direction.Table IV. Force constants
ofthe
«
nearly rigid
tetrahedronapproximation
»ofsection
4. L and Trefer
to thelongitudinal
and transverseforce
constantsof
the Born-Von-Karman model.t = T
T;.
The values are inN/m.
(si-o) (o,o)i (si,si) (o-o)~ (o,o)~
L oo
(17.487
0.006t) (48.7
+ 0.0164t)
2.0 5.96T 14.737