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Fluctuation effect on the incommensurate transition of quartz
P. Borckmans, G. Dewel, D. Walgraef
To cite this version:
P. Borckmans, G. Dewel, D. Walgraef. Fluctuation effect on the incommensurate transition of quartz.
Journal de Physique I, EDP Sciences, 1991, 1 (7), pp.1055-1062. �10.1051/jp1:1991189�. �jpa-00246385�
Classification
Physics
Abstracts 64.70R 64.70Fluctuation effect
onthe incommensurate transition of quartz
P. Borckmans
(*),
G. Dewel(*)
and D.Walgraef (*)
Service de
Chimie-Physique,
Universitd Libre de Bruxelles, Bd duTriomphe,
CP 231, B-1050, Brussels,Belgium
(Received Jo December J990,
accepted
infinal form
2J MarchJ99J)
Rksumk. Dans la
description
auchamp
moyen de la transition vers [es structures incommensu- rabies du quartz, lesphases
3-q,J-q
et flapparaissent
au mdmepoint critique.
On montre que [esfluctuations
critiques
[Event cetteddgdndrescence
et transforment la transition du second ordre entransitions du premier ordre. De
plus,
il existe unerdgion
de l'espace desparamdtres
off laphase
I-qapparait
entre lesphases
fl et3-q,
mdme en l'absence de tensionappliqude,
comme lemontrent des
expdriences
rdcentes.Abstract. In the mean field
description
of the incommensurate transition of quartz, the triangular 3-q, thestriped
I-q and the flphases
meet at the same criticalpoint.
It is shown that critical fluctuations lift thisdegeneracy
and transform the second order transition into first orderones. Furthermore, there is a
regime
of the parameter space where the I-q phase should appearbetween the fl and 3-q
phases,
even in the absence of anyapplied
stress, as seen in recentexperiments.
The
a-p
transition in quartz has been known for almost a century[Ii.
It is a structuralphase
transition which
corresponds
to the rotation ofSi04
tetrahedra around the threefold axis. The order parameter 1~ can be taken to have amagnitude equal
to thedisplacement
of agiven
Si ion as shown infigure1 [2].
It is zero in thep phase
and increases when thetemperature
islowered into the
a
phase
where it can take twoequal
butopposite
valuescorresponding
to the so-calledDauphinb
twin domains. Morerecently,
an incommensuratephase
between the low- temperature aphase
and thehigh
temperaturep phase
has been observed[3-6].
This is one of the manyexamples
where transitions occur between normalcrystalline phases
and incommen-surate modulated structures
[7],
but its interest lies in the fact that modulated structures of differentsymmetries
may besimultaneously
stable.Effectively,
the theoreticalanalysis
basedon the Landau free energy derived for this system
[8, 9]
concluded to the existence ofstriped
modulated structures defined
by
onepair
of wavevectors(I-q phase)
or of modulatedstructures of
triangular
symmetry definedby
threepairs
of wavevectorsseparated by
2
ar/3 angles (3-q phase).
(*) Research Associates, National Fund for Scientific Research
(Belgium).
1056 JOURNAL DE
PHYSIQUE
I bt 73 y ~
x
~ 3
1
Fig. I. Basal plane
projection
of the silicon ions in theWigner-Seitz
cell of the quartz structure. The full circles indicate theposition
of the silicon atoms in the flphase
while the arrows show the directions of the silicon displacements in the transition to the aphase.
In most
experimental conditions,
well-defined3-q
structures of about 10 nmwavelength
have been observed which
persist
in a small temperature range(IA K)
around the criticaltemperature (846K). According
to the mean field Landaudescription,
thisp
-
3-q phase
transition should be second order and occur at a well-defined criticalpoint 7j [8, 9]. However,
in the presence of uniaxial stresses, astriped I-q
modulatedphase
appears between thep
and the3-q phases [10]. Furthermore,
recentexperiments [11, 12]
concluded to the existence of theI-q phase
between thep
and the3-q phases,
even in the absence of anapplied
stress, andthis seems in contradiction with the theoretical
prediction
that the3-q, I-q
andp phases
should meet at the critical
point 1j.
The existence of uncontrolable local stresses or defects can be invoked toexplain
thisphenomenon. However,
an alternativeexplanation
may be found in the effect of critical fluctuations on this transition.Indeed,
in a renormalization groupanalysis,
no stable fixedpoint
has been found in the e= 4 d
expansion [13]. Usually
this indicates that the transition is first order. On the otherhand,
it has been shown that criticalfluctuations can
strongly
affect the nature of the transition between a uniform state and aperiodic
structure. It is the main purpose of this note to assess the effect of the orderparameter
fluctuations near the criticaltemperature 7j
where thep, 3-q
andI-q phases
meet.According
to thephenomenological description
of thea-p
transition of quartz[14],
the free energy can beexpanded
in a power series of the Fourier components 1~~ of the orderparameter
and of the strain field. After elimination of the elasticdegrees
offreedom,
thequadratic part
of the free energy may bewritten,
in scaledvariables,
as[8]
:~2
"I (~
~ +d(~~ ~~)~
+hQ~C°S~(~ ~ )) l'lq
(~(l)
q
where e
=
(( T)/(, ( being
thep-INC
transitiontemperature
go is thelength
of the critical modulation wavevectors andj
theangle
between q and the two-fold x axis of thea
phase (cf. Fig. I).
Thecorresponding marginal stability
surface which limits thestability
domain of thep phase
in the(e,
q space is shown infigure
2. One sees that 6 unstable modesare
expected
at T=
Tj,
whichcorrespond
to modulation wavevectors oflength
go and of orientationj
=
(2n +1) ar/6.
Hencesingle-
andtriple-q
structures may inprinciple
be nucleated for T< T; but their
stability
has to be determinedby
thehigher
order terms of the Landau functional.6
~.
qy
o
.s
-o
5 o
qx
Fig.
2.Representation,
in the(e,
q) space, of the surface which limits the stability domain of the flphase
of quartz,according
to the Landau free energy (Eq.(I)) (d
= I, qo
= I, A
=
0.5).
Effectively,
thehigher
order contributions to the free energy may be written as~~2
"I G( (q)
lJq lJq~ lJq~ 3(q
+ q1+~2)
q,qi,q2
+
I H( (q)
lJq lJq~lJq~lJ
q~ 3
(q
+ q1+ ~2 +~3)
q.q].q2.q3
~ 2
1
~
~q i ''lq'
~ ~i '~qi'lq-q]
~~~q.qi
The detailed
dependence
of the coefficientsG, H,
K andv on the elastic constants of the system can be found in references
[8, 9].
Inparticular,
it may beshown,
in the mean fieldapproximation,
that theangular q-dependence
of G allows the formation of stabletriple-q
structures via a second order transition. The transition
temperature
is the same for thesingle-
and
triple-q
structures and one should thusexpect
an extremesensitivity
of thisdegenerate
critical
point
to thermal fluctuations.Hence,
let usanalyze
the influence of the most relevant fluctuations on these two types of structures.4.I
SINGLE-q
OR STRIPED PHASE. In the mean-fieldapproximation,
the existence andstability
of asingle-q
structure of wavevector q oflength
qo and orientedalong
one of thedirections defined
by j
=
(2
n + Iar/6
mayeasily
be deduced from the Landau free energy(1-2) [8, 9]. However,
critical fluctuations are known to be able to affect the result of the mean-fieldanalysis,
and this is also the case here.Indeed,
if ones takes into account the contribution of thesefluctuations,
theequation
of state may bewritten,
at the Hartreeapproximation [15, 16]
:~ ~
~'~@~
~~'lqo~ ~'l@)
~ ~~'lqo) l~/(
~2
~'lk 'l-k) (~)
where
(... )
represents theequilibrium
mean, and where theintegral
is taken over the«critical
shell»,
I-e- over wavevectorspointing
in the domain definedby
d(q~ q()~
+Aq
~cos~(3 j
< e.
1058 JOURNAL DE
PHYSIQUE
I bt 7This
equation
isgeneric
for a second order transition from a uniform state to one-dimensional modulations. The coefficient u may
easily
be obtained from thecorresponding
Landau free energy
(for quartz
or berlinite the evaluation of u from the free energy(1, 2)
maybe found in
[8, 9]).
The correlation function(1~~1~_~)
may be evaluated at the sameapproximation through
the self-consistent schemek~r
~~~
~~
r +
d(k~ q()~
+Ak~ cos~ (3 j )
r=-e+2u((1~~~)(~+u ~(2'r)
~~~(1~~1~_~) (4)
where
k~
is the Boltzmann constant and r=
TIT.
As aresult,
theequation
of state may be rewritten as~l
i'lqol
~l'~qol l'~qol
~ ~°
(~)
with
e = rj +
CmK(m) (6)
uk~
rwhere C
= and
K(m)
is thecomplete elliptic integral
of the first kind with~2
arfi~
m~
=
~~°
~.
Since
K(m diverges
at rj =0,
thecorresponding
modulated structure arises ri +Ago
with a finite
amplitude (I.e.
via afirst-order transition)
:'~% "
~~~ I
~at ej =
e(rj~),
wheree(rj~) corresponds
to the minimum of the curvee(rj) given
inequation (6),
and is thus definedby
the condition :Cm/ E(m~)
= ~ ~
(7)
2
Aqo(
I m~)
where
E(m
is thecomplete elliptic integral
of the second kind. In the weakanisotropy
limit(uk~
r » d~'~(Aq()~'~),
one has~
3
luk~
r2'3
~
/$
~~~~while in the
strong anisotropy
limit(uk~
r «d~/~(Aq()~'~),
one finds3ukB
rAq/
~i =
(8b)
~ ~
/p~~
UkB TOne however needs to be aware of the fact that the Hartree or
one-loop approximation
consists in
neglecting higher
order contributions in theexpansion [17]. Following Brazovskii,
a contribution of order n behaves as
CmK(m ) (rj
+Aqj)~
~ and should thus benegligeable
in theregion
ofinterest,
I-e- whereuk~
r>
rj11/K(m).
Thisconsistency
argument,supplemented by
the failure of the renormalization groupanalysis
to find a stable fixedpoint [13]
thussuggests
that the transition should be firstorder,
and we have here anotherexample
of the so-called Brazovskii effect
[16]
where fluctuationsmodify qualitatively
the character of the transition.4.2
TRIPLE-q
OR TRIANGULAR PHASE. A similar discussion may beperformed
for the3-q
structures. In this case, the cubic term of the free energy
couples
theamplitudes
of the three modulations and behaves as l~j 1~~1~~ cos(3 j ).
The minimization process then shows thatcos
(3 j )
isproportional
to1~
(leading
to the observed rotation of thetriangular
structure anda
slight
variation of itswavelength),
so that the cubic termeffectively
behaves as1~~, as shown in
[8, 9],
and thepotential corresponding
to these structures may be written as3
F
=
Z (-e+d(Ql-Ql)~ i~Jq,i~+( i~Jq,i~+2u i~Jq,i~ Z ~lq~l~)j
,=i j,,
j2 j2 j2
g
~~'
~~~~~~
(9)
I l'lq,
,
If
needed, explicit
values for the coefficients u and g may be obtained from the Landau free energy.The
amplitude
of the threecomponents
of the order parameter which minimize this free energy aregiven by
0
(E
< 0
~~'~
~~~ ~~ ~~~5 u
~
2 w ~ "
~
'
~'~
~°' ~~/
~~~~and the mean-field transition is thus second order as for
I-q
structuresprovided
w <
~)
For w »~)
the transition should be firstorder,
and one needs to considerhigher
order contributions to the Landau free energy.
The
stability
domain of this structure mayeasily
be deduced from the free energy, and one finds that it isonly
stable for w »(. Furthermore,
onincluding
the dominant contribution from critical fluctuations in theequation
of state,namely
thediagonal
correlationfunctions,
one obtains
[15]
:If the correlation functions are evaluated at the same
approximation
level as in theI-q
case,one finds
[15]
r~-
(u+2w) (1~~) (~=
0(12)
and
e =
(I
+ y r~ +CmK(m) (13)
1060 JOURNAL DE
PHYSIQUE
I bt 7where Y
"~/+2w
Therefore the
3-q
modulated structure also arises with a finiteamplitude
ll~q,I
=J~ (~i
~ ,
(14)
and a finite rotation
angle j~, given by
cos
(3 j~)
ccJ~~~
,
(15)
u + 2 w
at e~=
e(r~~),
wheree(r~~) corresponds
to the minimum of the curve definedby equation (13),
and is thus definedby
the conditionCm/ E(m~)
'~ ~ ~
2
Aq((
Iml)
In the strong
anisotropy limit,
one has :~
3
uk~
r~~
Aq((I
+ y)~'~~~~~~
/$~ ~~B
~while in the weak
anisotropy limit,
one has~~
2
uk~
r 2j3
~3 "
~(l
+ Y~
d(17b)
Hence,
the thresholds forI-q
and3-q
structures are different(for example,
in the strong 4uk~
ranisotropy limit,
e~ ej=
In
(I
+ y)),
and/$
e~ » e j for w
< u
(18)
Thus,
as shown on thephase diagram
sketched infigure 3,
for ~< w < u, a
I-q
modulated 3structure should occur between the
p
and3-q phases,
even in the absence of uniaxial stresses in agreement with recentexperimental
observations[11, 12].
To
conclude,
we see that critical fluctuationsprovide
an intrinsic symmetrybreaking
effect which lifts thedegeneracy
of the mean field transitionpoint
between thep, I-q
and3-q phases. They
alsomodify qualitatively
the incommensuratephase
transitions of quartz, whichshould be
effectively
first order. Infact,
thisphenomenon
should occurgenerically when, according
to the mean fieldapproximation,
incommensuratephases
of differentsymmetries
meet at the same critical
point,
as in the case of somelayered
CDWcompounds
and rare gasmonolayers
adsorbed ongraphite [18].
Acknowledgments.
Fruitful discussions with Profs. S.
Amelinckx,
J.Lajzerowicz,
J. VanLanduyt,
G. Van Tendeloo and Dr. C. Leroux are
gratefully acknowledged.
This work wassupported
in
part by
theBelgian
Governmentthrough
the «Pbles d'Attraction Interuniversitaire»program.
W .,~~
5u/ 2
'
3q a
~
~
u/3 ~q
o ~
W &,
~
~ j,
3q~(
(
a (b)u/3
',~_~(
lq
E
Fig.
3. Phasediagram
of the incommensuratephase
transitions of quartz deduced from the Landau free energy(Eqs. (1,
2)),(aj
in the mean fieldapproximation
and(b) by taking
into account critical fluctuations (w, which is defined in Eqs. (9) andlo),
represents the intensity of the nonlinearcouplings
between the wavevectors
underlying
thetriple-q
structure).References
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(1889)
1046.[2] SCOTT J. F., Rev. Mod.
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