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HAL Id: jpa-00246634

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Submitted on 1 Jan 1992

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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�

(2)

Classification

Physics

Abstracts

63.20D 64.70R

Origin of the incommensurate phase of quartz

:

II. Interpretation of inelastic neutron scattering data

M.

Vallade,

B.

Berge

and G. Dolino

Universitd

Joseph

Fourier (Grenoble I), Laboratoire de

Spectrom£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 diffusion

indlastique

des neutrons des modes de basse

frdquence

du quartz p, ddcrits dans l'article

pr6cddent

[Ii, sont

interpr6tds

h l'aide de deux

approches

diff6rentes : I) un modkle

ph6nom6nologique,

directement issu d'un

ddveloppement

du type

Landau-Ginzburg

de

l'6nergie

libre ; cc modkle n'est valable que pour la

panic

du spectre relatif aux

phonons

de grande

longueur

d'onde, mais il perrnet d'6tablir une connexion aisle avec les donndes

therrnodynamiques

it) un modme

microscopique

de

dynamique

de r6seau, qui est

une extension du modme de Grimm-Domer (modkle h t6trakdres

rigides)

on montre que les

principales caract6ristiques

du spectre des

phonons

de basse

ft6quence,

et en

particulier

l'amollissement d'un mode

3~

h un vecteur d'onde incommensurable

prks

du centre de zone, peut Etre

compris

par une

analyse

des mouvements de t6trakdres

Si04

Presque

rigides.

Abstract. The results of an inelastic neutron

scattering investigation

of the

low-frequency

modes of p quartz, described in the

preceding

paper [I], are

interpreted using

two different

approaches:

I) a

phenomenological

model

directly

derived from a

Landau-Ginzburg

type

expansion

of the free energy ; this model is

only

relevant for the

long-wavelength

part of the

phonon

spectrum but it allows an easy connection with

therrnodynamical

data ; it) a

microscopic

lattice

dynamical

model, which is an extension of the Grimm-Domer model ; it is shown that the main

properties

of the

low-frequency phonon

spectrum and, in

particular,

the

softening

of a

3~

mode at an incommensurate wave vector close to the zone,center, can be understood

by analysing

the motions of

nearly rigid

Si04 tetrahedra.

I. Introduction.

The various

physical

mechanisms

leading

to the occurrence of incommensurate

(inc) phases

in dielectrics have been an active field of research

during

the recent years

[2].

From a

phenomenological point

of

view,

inc

phase

transitions in dielectrics have been related to the presence of the so-called « Lifshitz invariant »

j3] (which

can

only

be found when the order

(*) Assoc16 au C-N-R-S-

(3)

parameter has several

components)

or to a «

Lifshitz,type

invariant»

[4] (when

the order parameter is

coupled

to another

thermodynan~ic variable).

On the other hand the

microscopic

mechanisms

leading

to the existence of an inc

phase

have been

clearly

elucitaded

only

in a restricted number of materials : for

biphenyl,

the

competition

between intramolecular and intermolecular interactions has been invoked to

explain

the occurrence of a modulated structure

[5].

In

NaN02

the inc

phase

is

thought

to

result from the

coupling

of

large amplitude

reorientations of

N02

groups with the

translational motion of Na

[6]. Microscopic

models have also been

proposed

for some other systems e,g.,

K~Se04 17], propylammonium

tetrachlorometallates

[8].

The relative

simplicity

of the quartz structure makes attractive the

study

of the mechanism

leading

to the inc

phase existing

near the a-p transition in this material

[9]. According

to the

phenomenological theory

of

Aslanyan

et al.

[10, iii

the occurrence of an inc

phase

in quartz type

crystals

would result from a «

gradient coupling

» between the elastic strains and the

gradient

of the order parameter 1~ of the

a-p

structural transition. This kind of

coupling corresponds,

in the soft-mode

picture,

to an interaction between an

optical

mode and an acoustic mode close to the Brillouin zone-center as shown in reference

[12].

A

striking

illustration of the

physical meaning

of this kind of

coupling

in

quartz-type crystals

is

provided by

the so-called «

exaggerated gradient

method » of Heine and Mc-Connell

[13].

The order parameter 1~ of the

a-p phase

transition

corresponds mainly

to altemate rotations of

Si04

tetrahedra around axes

lying

in the basal

plane

of the

hexagonal

lattice. It

corresponds

to a

zone center

optical

mode. In the «

phase

1~ can take two

opposite

values

(according

to the two

possible signs

of rotation of each

tetrahedron), leading

to

Dauphind twinning.

A very thin domain wall between these twins

(as represented

in

Fig, I) corresponds

to a strong

(and probably quite exaggerated) gradient

of 1~ but one can

easily

see that deformations of the unit cell

(-I.e. strains-)

are present in the wall.

Furthermore,

the

comparison

between

figures

la and 16

clearly

shows

that, according

to the direction of the

gradient

of

1~, the strains are either pure shear

(VI~ along

the

Oy

type

directions)

or

purely compressive

strains

(VI~ along

the Ox type

directions).

In

spite

of their

qualitative

character these

pictures

are of some

help

to

understand the mechanism

leading

to the incommensurate

phase

in quartz: the actual

gradient

of

1~ which is present in a

long-wavelength

inc

modulation, although

much smaller than that described in

figure I,

is associated with strains of different

kinds, according

to its

direction. One is then

logically

lead to ascribe the

origin

of the inc

phase

to an

interplay

between two modes of atomic

displacements

:

optical,like

and acoustic-like. A controverse took

place

some years ago about the relative

weight

of the two modes

[14].

In a recent

preliminary work,

Gouhara et al.

[15] reported

on an

X-ray

determination of the inc structure

and

they

confirmed that the modulated atomic

displacements correspond

to a

mixing

of

acoustic and

optical

components

(with

a

large

contribution of the acoustic

one).

As the inc

phase

arises from the

high

temperature p

phase through

a 2nd order

transition,

the

dynamical

critical fluctuations above the

p-inc

transition

point T,,

must also involve a

mixing

of acoustic and soft

optical phonons.

This

point

was

already

evidenced in

preliminary

inelastic neutron

scattering experiments [16]

and a more detailed

investigation,

described in the

preceding

paper

[Ii, brings

a

stronger support

to this

point

of view. The purpose of this paper is an attempt to

give

a

quantitative interpretation

of the temperature

dependence

of the

low-energy phonon

branches in the

p phase

and thus to propose a mechanism

leading

to the inc

phase.

The

analysis

will be made at two different levels :

.

First,

as the inc wave vector is

only

a small fraction of the

reciprocal

lattice unit vector

(qo>0.03a*),

a continuous-medium

approximation

is relevant. We consider a

simple

phenomenological theory

which follows the

original

model of reference

[10] by considering

only

a soft

optical

mode

(SM)

and acoustic

phonon modes,

with small wave vectors. The main

(4)

x x

a)

b)

Fig, I.

-Exaggerated

gradient

picture of

a

Dauphind

twin wall in

The

figure

the

arrangement

of the

comersharing Si04 tetrahedra,rojected on the (0

0

) lane : a) wall

erpendicular to the Oy axis.

The

radient of the order

parameter

(v,u~ )

is associated with a

unit

cell. b)

Domain wall erpendicular to

the

Ox axis. The gradient (v~u~) is associated

with

a

compressive strain

of

the unit cell. In figure la the two twins have been

translated

along

order

deformed.)

interest of

this

approach

is

to

provide an easy connection

macroscopic operties,

Sect. 2).

. In a second step, an ttempt

is

ade

to

interpret the

of the

modes over

the

whole

Brillouin zone, by considering

a

icroscopic model. As a

starting point

for this

study, we use the

Grimm-Domer model

[17,

18] which assumes that

frequency ptical modes are those hich leave the Si04 trahedra

The

method

used to find these modes is

described in

ection 3.

A

imple

Bom,von rman

force

constants

and a uasi-harmonic

approximation)

is hen oposed in

section

emarks.

2. henomenological radient

coupling model.

As usual

in the

soft-mode

theory of

phase

transitions, the phonon requencies

within the

pproximation,

using

an effective otential energywhich

has

the

same

form

as the andau-Ginzburg free

energy.

In

the

high emperature

p phase

of

has already

been shown that the potential

energy

corresponding

to

the long velength

soft

optical phonon

mode

and

to

(5)

In this

expression ~(q)

is the

amplitude

of the

uncoupled soft-optical

mode with a wave vector q, and

wj(q, T)

is the

corresponding frequency.

Close to the Brillouin zone center we

assume that :

wj(q, T)

m A

(T To)

+

gq~

+

hq~

U~~~(q), UT~~(q)

and

U~~(q)

are the

amplitude

of the two transverse acoustic modes

(polarized respectively

in the

(0 01) plane

and

perpendicular

to this

plane)

and the

longitudinal

acoustic mode. The

uncoupled

acoustic mode

frequencies

are :

W(Ai(~)

~

j~ ~~ W(A2(~)

"

~ ~~, W/A(~)

~

)~ ~~

(p

=

volumic mass,

C~~ = elastic

constants).

The bilinear

coupling

between

1~

(q)

and

U~A (q)

or

UTA~(q),

in

equation (I) corresponds

to the

Lifshitz-type

invariant introduced

by Aslanyan

and

Levanyuk j10].

This term exhibits

anisotropy (since

it

depends

on the

angle

~b between q and the twofold Ox axis of the

hexagonal p phase).

One can note that for

4

= 0

(mod ar/3)),

~

(q )

is

only coupled

with the LA mode, whereas for

4

=

(ar/2) (mod (ar/3)),

1~

(q)

is

only coupled

with the

TAT

mode.

This agrees with the «

exaggerated gradient picture

» of

figure I,

since q is

along

the

gradient of1~.

A bilinear

coupling

between

1~(q)

and

UT~~(q)

is also allowed

by

symmetry but it is

proportional

to

q~ and,

for small q, it can be

neglected.

A similar

description

of the interaction between a soft

optical

mode and an acoustic mode has

already

been used

by

Axe et al, to

explain

the anomalous

dispersion

of acoustic branch in

KTaO~ j19].

In order to describe the finite linewidth of the

phonon

groups, a

damping

y has to be introduced for the soft

optical

mode

(the damping

of acoustic

phonons

is

proportional

to

q~

and it can be

neglected

in the small wave vector

limit).

The

coupled

mode

complex frequencies

are then obtained from the secular

equation

:

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

0

0)

directions of the

reciprocal lattice)

cos

(3 #)

= 0 and

equation (2)

reduces to a 4th order

polynomial equation

for w.

Explicit

solutions can

only

be

obtained in the limit y

= 0 :

ml (q)

=

iwl(q)

+

WlAi(q)i

±

~/iwl(q) WlAi(q)i~

+ 4

a~q~j (3)

The lower branch

w_(q)

exhibits a minimum

equal

to 0 at the

p,inc phase

transition

temperature

T =

T;

for an inc modulation wave-vector q = qo.

Ti

and qo are related

by

the relations :

A

(T~ To )

= 1/2

£

g

q(

=

hq( (4)

66

Since h is assumed to be ~

0,

an inc

phase

can

only

occur when g <

(pa~/C~~).

When y is

non-vanishing, equation (2)

must be solved

numerically.

The solutions behave

essentially

in the same way as in the y

= 0 case except that both

frequencies

w~ are now

(6)

complex,

the mode

coupling producing

a transfer of

damping

from the soft-mode to the acoustic mode, as observed in Brillouin

scattering experiments [12].

Most of the

input parameters

of this

model,

have been deduced

by fitting

the inelastic

neutron data of

[Ii

obtained at the

highest temperature (T= Ti +400K)

in the range

[q[

< 0.I a*

along

the 3 direction.

(This

limited range of wave-vector was chosen rather

arbitrarily,

but it appears to be an upper limit of

validity

of the q

expansion

used for the

uncoupled frequencies).

The coefficient h

(proportional

to

(Tj To) according

to

(4))

was

much more

sensitively

deterJnined from the value of qo and from the spectrum at T

T,.

The elastic constants C

ii and

Cm

were taken from ultrasonic data

[201.

The numerical

values of the

parameters

are summarized in table1

[211.

The

dispersion

curves

along

3((f00))

directions and A directions

((f to))

for the

temperature

range

(T;

< T

< T

; + 400

K)

were then calculated with this set of parameters. The fit was

improved by allowing

a linear

temperature dependence

of the

damping

coefficient y

(from

0.5 THz at

Ti,

to 0.7 THz at

Ti

+ 400

K).

A

general picture

of the

dispersion

curves is shown in

figure

2.

The main conclusions which can be drawn from a

comparison

of calculated and

experimental

curves are the

following

:

I)

The overall agreement is correct. In

particular

the

strong anisotropy

of the soft modes and of the

TAj

and LA modes in the basal

plane

is

fairly

well

reproduced

with a minimum of

adjustable parameters. Neglecting

the

coupling

between the soft

optical

mode with the

TA~

mode is

justified

since the

dispersion

curve of this mode is almost

isotropic

and exhibits

no anomalous

dispersion.

ii)

The main

discrepancy

concems the value of the

parameter Ti To (calculated

to be

0.7K whereas the

experimental

value is

5±2K). Any attempt

to

adjust Tj- To

to its

experimental

value results in a

strong

increase of the value of the

parameter

h

(according

to

Eq. (4))

which leads to a curvature of the

dispersion

curve at T

= T~

by

far too steep for qo < q < 0, I. This

discrepancy

may arise from some

inadequacy

of the mean field

theory

and

(or)

of the

quasi,harmonic-approximation.

Let us recall that an anomalous temperature

dependence

of some elastic constants and of the thermal

expansion

above

Ti [221

shows the

important

role

played by

fluctuations combined with strong anharmonic

couplings.

Unfortu-

nately, owing

to the limited resolution and to the

difficulty

of a reliable deconvolution of our neutron

scattering data,

it seems

meaningless

at the present time to introduce additional

fitting parameters

in the model

(such

as non-classical critical

exponents).

On another

hand,

it is noticeable and somewhat

puzzling that,

in

equations (4),

the terms

pa~/Cm

and g

nearly

Table I. Parameters

of

the

phenomenological

model

of

section 2

(with JFequencies

in THz and wave vectors in units

of

the

reciprocal 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 *

(7)

/

~ 2

o

0

0.00 .02 .04 .06 ,08 .10

a) b)

Fig.

2.

-Dispersion

curves of the

interacting phonon

branches

according

to the

phenomenological

model of section 2. The lines are calculated with the set of parameters of table I and the

points

are

experimental

values

(Ref. [I]).

al Wave-vector

along (I

0

0)

direction

(3

or

Oy).

b) Wave-vector

along (I

2 I

0)

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 inc

phase

can

occur.

(This

is related to the small range of

temperature (1.5 K)

over which the inc

phase

exists,

and to the small value of the inc wave vector

qo).

This close

cancellation,

which appears

as a pure coincidence in the

phenomenological theory,

can be better understood in the

light

of the

microscopic

model described in the next section.

3.

Rigid

tetrahedra mode

analysis.

In this section we present an

attempt

to derive

simple physical

arguments which can shed

some

light

on the existence of an inc

phase

in

quartz, by considering

the

peculiar

structures of this material. In

principle

the occurrence of the inc

phase

should be found

by solving

the full

dynamical problem (27 phonon branches) using

an

adequate

force constant model. Several models of this kind have been

proposed [23]

most of them are relative to a-quartz but some

of them also concem

p-quartz [24, 25].

It is not

surprising

however that such models do not

predict

the inc

instability,

because the characteristic

dip

on the lowest

phonon

branch is

expected

to be a

tiny

detail in the full

phonon spectrum,

and its existence is related to a subtle

balance between weak force constants. In

addition,

even if a model were able to exhibit this

dip,

it would

probably

obscure the

physics

under

heavy

numerical calculations. Therefore it

seems to be more advised to concentrate our attention on the lowest energy

phonon

modes.

As

already

often

noted, quartz

is built of rather

rigid Si04

units which share a common comer

(see Fig. 3).

The covalent character of the SiO

bonding explains

this

rigidity

and the

relatively

open structure of

p

quartz.

Megaw [26] analysed

the

a-p

transition in

quartz

as the result of rotations of

rigid Si04

tetrahedra. This idea was then

developed by

Grimm et al.

[17]

who tried to relate the thermal

expansion

near the transition to these rotations. The same

(8)

j,

5 6

I.o

7

y3

Fig.

3.

-Projection

of the unit cell of

p-quartz

on the basal

plane.

(o) oxygen atoms, (o) silicon atoms.

assumption

of

rigid

tetrahedra was later used

by Boysen

et al.

[181

to

analyse

the low

frequency part

of the

phonon

spectrum of a and

p quartz

that

they

have measured

by

inelastic neutron

scattering.

The main

assumption underlying

their

analysis

is that intertetrahedron force constants are smaller than intratetrahedron ones. Therefore the lowest energy

phonon

modes must

correspond

to

nearly rigid

motions of

Si04 units,

if any motion of this kind is allowed

by

the structure. As a matter of

fact,

these

particular

modes

merely correspond

to the

« extemal modes »

widely

used in the context of lattice

dynamics

of molecular

crystals.

In the

case of covalent framework

materials, however,

severe

topological

constraints are

imposed

on

the motion of

rigid

molecules

by

the fact that

they

share a comer and the existence of

« extemal modes » cannot be taken as

granted

in the

general

case. The

analysis

of

Boysen

et al.

[18] only

concemed the existence of

rigid

tetrahedron modes

(RTM)

at some

high

symmetry

points

in the Brillouin-zone

(r

and

M).

In a

preceding

paper

[16]

we gave the results of a more

general analysis

valid for any

point

inside the Brillouin zone. Since no detail

was

given

in that paper

conceming

the method used to derive these

RTM,

and since this method is

thought

to be of some

general

interest to

predict

the existence of soft modes in framework

crystals,

we

give

in the

following

a more

complete description

of the

procedure.

Let us consider a 3-dimensional framework of N identical comer

sharing

molecular units with

p comers shared. The total number of

degrees

of freedom is 6N

(3

translations

T~~ and 3 rotations

R~~ (per

unit

I).

The three

displacements

of each atom shared

by

two units

(I

and

j)

can be

expressed

as a function of both the

(T~,

R~ and the

(T~, Rj).

There are then 3 relations

linking

the motions of two connected units : these

compatibility

relations will be

called «constraints». The total number of constraints in the system is

clearly ~~~

2

(neglecting

surface

effects)

since

(Np/2)

atoms are shared. For small atomic

displacements

these ~

)P

constraints lead to a

system

of ~

~P

homogeneous

linear

equations

with 6N 2

unknown

(T~~

and

R~j).

For tetrahedral units

(as

in

quartz)

p

= 4 so that the number

of equations

is the same as the number

ofunknown.

This case is

particularly interesting

since non-

trivial solutions

only

exist under

special

conditions.

Using

a harmonic

approximation,

the

equation

of motion can be written

using

Fourier components

T~;(q)

and

R~;(q)

where the index I denotes now the molecular units

belonging

to a

given

unit cell

(I

= I to

n)

and q is a

(9)

vector of the lst Brillouin zone

(BZ).

For each q there are then ~ ~P

equations

with fin 2

complex

unknown

T,(q)

and

R,(q).

Let us consider the

p

quartz structure

(with

the

assumption

of

perfect Si04

tetrahedra for the sake of

simplicity).

There are three

(Si04)

units per unit cell

(see Fig. 3).

The 18 constraints

correspond

to the

displacements

of 6 oxygen

atoms O~ = 4 to

9) (see

tab.

II). They correspond

to a

system

of 18

homogeneous equations

in which the wave vector q appears

through

the

phase

factors

e;.

For q at a

general position

in

the BZ there are no non-trivial

solutions,

but solutions exist when q lies in the

(0

0

1) plane

or

along

the

[0

0

Ii

directions

(and

also

along particular

lines on the BZ

edge).

In

solving

the

system

of

equations,

it is convenient to use

symmetry adapted

combinations of

T,(q)

and R~

(q)

which transform

according

to irreducible

representations

of the small group of the wave

Table II. Atomic

displacement

components u~~

(in

the

(x,

y,

z) reference JFame)

as a

jknction of

the translation and rotation components

of

the

Si04

units,

for rigid

tetrahedron modes

ofwave

vector q R

(

e

)

is the matrix

corresponding

to a rotation

ofangle

e around the z- axis.

T~,

and

R~;

are translations and rotations components in the local

(x;,

y;,

z,) reference frame (see Fig.

3

).

The set

of18 equations

relative to the oxygen

displacements

determine the

possible

RTM with wave vector q

(coordinates

11~D.

Si ui

~

=

Ti

j2arj~

~

u2«"R~p ~

2p

j4arj~

"3«"R«fl $

3fl

~

U4a ~

(Tl

~

~l

X Pa

)a

"

°3 ~afl ~) (T3

~

~3

X

Pd)fl

115 a " R

«fl

~)

1'~2 +

~2

X

Pb )fl "

°3 ~afl ~) (~3

+

~3

X

Pc)fl

"8

a "

~ap ~) (T3

~

~3

X

Pa)p

"

°2 ~afl ~/

1'~2

~

~2

X

Pd)p

"9

a

"

(Tl

~

~l

X

Pb)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(I

(10)

vector q, so that the system

splits

into

independent sub,systems corresponding

to each

representation.

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 translational

displacement

and is called acoustic

(A), it)

it behaves as a pure

optical

mode

(O) (center

of mass

invariant), iii)

it is a

mixing

of acoustic and

optical components (A+O).

At the BZ center

l~

it is clear that the 3 uniforJn translations leave the

Si04

units undeforJned so that

they

are RTM

(labelled Qx(r~), Q~(r~)

and

Q~(r~)).

There exists an additional solution

Q(r~)

which

corresponds

to the

order

parameter

1~ of the

a-p transition,

since it involves altemate rotations of the

Si04

around the

Ox-type

directions.

Compatibility

relations can be found

by looking

at the

q - 0 limit

along

various directions of the

reciprocal

space. For q

along [0

0

fl (A line),

one

has 3 RTM

belonging

to different

representations

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

0

1) plane

and the latter is the soft

optical

mode.

Table III.

Rigid

tetrahedron modes with wave vectors

along

the

3,

A and A directions.

T,,

and

R,;

are the

(unnormalised)

translation and rotation components relative to the I-th

SiO~

unit

(see Fig.

3

).

The

corresponding

atomic

displacements

can be calculated

using

table II. In the last line is indicated the character

of

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) sina

Ry2 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)

(11)

When q is

along

a

general

direction in the

(001) plane, only

one RTM is found and it behaves as a pure TA mode

polarized along [0

0

Ii (the

mode labeled

TA~

in Sect.

2).

No

additional RTM is found in the

particular

case when q lies

along ii I 0) (A directions),

but

one extra RTM is

actually

found when q lies

along ii

0

0) (3 directions).

This last

mode,

noted

Qa(3~),

appears to be the most

interesting

one. As a matter of fact it is the

only

RTM which exhibits a « mixed » character

(A

+

O)

:

Qa(32)

- 0.6

Q (1~3)

0.8

Qx(1~6) (The

modes have been normalized

using

:

£

m;

[u~~(q)[~

=

l.)

i, a

This

singular

behaviour deserves some comments, since actual

phonon

modes are

always

pure acoustic or

optical

modes when q goes to zero. This «

hybrid

» mode is a consequence of the infinite force constants which are

implicitly

assumed in the

rigid Si04

tetrahedron

hypothesis.

Modes which are not RTM have an infinite

frequency.

This is the case, in

particular,

for the acoustic modes

(at

q #

0)

which are not

RTM,

such as the LA mode and the

TAT

mode. The

corresponding dispersion

branches have an infinite

slope

at q # 0 for

perfectly rigid

tetrahedra. The

crossing

of this acoustic

phonon

branch with an

optical

mode

occurs

right

at the r

point,

and

hybridization

of acoustic and

optical

modes takes

place

at

vanishingly

small q.

(With

a more realistic

assumption

of finite intra tetrahedron force constants, the

crossing

would occur at finite wave vectors and the

singular

behaviour would be removed see below Sect. 4

-).

It is

interesting

to note that this

type

of behaviour is

quite

reminiscent of the TO

phonon-photon

mode interaction in the

polariton region

:

assuming

an

infinite

light velocity

results in a « mixed

photon-phonon

» excitation at q =

0 which leads to the LO-To

splitting.

This

singular

behaviour

disappears

when a finite

light velocity

is taken

into account.

An additional

interesting

feature of the

Q~(3~)

mode is found when one considers the mean

change

Ad of the

(Si-Si)

distance for this mode. As shown in

figure

4 Ad vanishes at r and at the BZ

edge point

M and it is

quite

small

along

the whole 3 line for this

particular

mode.

Since the Si-O-Si force constant is known to be the

strongest

among the intertetrahedron force constants

[2, 5]

one can expect the

Q~(3~)

mode to be flat and soft

along

the whole 3 line.

Let us summarize what kind of

qualitative

conclusions

conceming

the

phonon dispersion

curves of

p quartz

can be inferred from our

assumption

of

rigid

tetrahedra :

I)

the existence of three

low-lying

branches

(two

TA and one

optical)

for q

along [0

0

fl (A line)

it)

for q

along if

0

0) (3 lines),

a very soft and flat

branch, corresponding

to a strong

hybridization

of an

optical

and an acoustic

(TAj)

components near

l~

and a

moderately

low

frequency (TA~)

branch ;

iii)

for other directions of q in the

(0

0

1) plane,

a

moderately

soft

(TA~)

branch

roughly isotropic

as

long

as q lies in this

plane.

A

comparison

with

experimental

data

[Ii

shows that these

predictions

are

essentially

correct.

FurtherJnore,

inelastic neutron

scattering

structure factors can be calculated for the various

RTM. The results

conceming

the zone-center soft-mode

Q(r~)

and the soft-branch

Q~(3~)

are shown in

figure

5. It is

striking

that the

largest

calculated structure factors are found

along

the « fourth

hexagon

», in

agreement

with the

large

scattered intensities observed

along

these directions

[27].

The RTM

analysis provides

us with a

qualitative explanation

of the mechanism

leading

to an inc

phase

; the

Q~(3~)

mode possesses the two

key

features which are

required

for the

(12)

Ad

z ' /

2c '

' / /

~ //

A

r z

Fig.

4.- Mean relative change Ad of the Si-Si distance for the various

rigid

tetrahedra modes considered in the model of section 3. Ad is defined

by

Ad

=

i<J) jj

[(1~~ -1~~),r~~]~)~'~ where 1~~ is the (norrnalised)

displacement

of the I-th silicon in the mode and

r~~ the unit vector

along

the

equilibrium

Si- Si direction. (Ad for the shear mode

Qc(3~)

is also

represented

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 atomic

displacements

of the

Q~(3~)

mode (Tab. III). The size of the bars is

proportional

to the squared modulus of the structure factors. The circles are relative to the zone-center optic-mode Q

(r~).

Maximum

scattering intensity

is found along the «4th

hexagon»

in agreement with

experimental

observations. (The

figure corresponds

to the f

= 0 strate of the

reciprocal space.)

(13)

occurrence of a modulated

phase, according

to our

phenomenological approach

: a flat soft

dispersion

branch

along

3

(g small)

and a

large SM-TAT hybridization

at small q

(gradient coupling

coefficient a

large).

The ratio r of the

optical

mode

component

to the TA mode

component

is r= 0.75 in our model and it can be

compared

with the ratio of the

corresponding

static

displacements

in the inc

phase recently

determined

by

Gouhara et al.

[15]

(r

<

0,15).

It is noticeable that all the above conclusions have been deduced from

purely geometrical considerations,

without any

adjustable parameters.

In order to be a bit more

quantitative

one has to choose a

specific

force constant model.

4. Lattice

dynamical

model of fl quartz within the

nearly rigid

tetrahedra

approximation.

To follow on the lines of the

analysis

of the

preceding section,

we shall

attempt

a calculation of the

dispersion

curves of

p

quartz

by assuming

almost undeformable

Si04

units. As we are

mainly

interested in the lowest

frequency phonon branches,

we do not

try

to

diagonalize

the full 27 x 27

dynamical

matrix but we assume that it can be truncated to a 4 x 4 sub-matrix

corresponding

to the lowest energy modes

(acoustic

and soft

modes).

Such an

approximation

is better near the Brillouin zone center

(where

these modes have

frequencies

much lower than other

modes)

than near the zone

edge

where

they

are

relatively

close to the hard modes. Our

aim is to

keep

a maximum

physical transparency by introducing

the minimum number of

fitting parameters.

The set of modes chosen to write the 4 x 4

dynamical

sub-matrix includes the RTM

complemented by

non-RTM

purely

acoustic

components.

For q

along

A the 3

acoustic modes and the soft mode

belong

to different irreducible

representations.

The two TA modes and the

optical

mode are then the RTM of table III ;

only

one LA

component

should have to be

added,

but since it

belongs

to the irreducible

representation Ai

it does not

couple

with the

previous

modes and it is of no interest for our purpose. For q

along 3,

one LA component

(with

symmetry

3j)

and one

TAT component (with symmetry 3~)

should be added to the two RTM

Q~(3~)

and

Q~(3~).

One must note that there is a

large

arbitrariness in the choice of the non-RTM modes since

only

their behaviour close to q = 0 is well defined. A reasonable

guide

in

building

these modes is to select those which

keep

the Si-O bond

length invariant,

since the

corresponding

force constant is

by

far the strongest one

[25].

Unfortu-

nately

this

prescription

is not sufficient to

uniquely

define them. One has

found, however,

that the

shape

of the

dispersion

curves does not

depend

very much on a

particular choice,

at least in the

vicinity

of the r

point (which

is the most

important

to discuss the inc

instability).

The force constant model we have chosen, is of the

simple

Bom,Von Karman central force

type,

as that

recently

used

by

Bethke et al.

[25]

to fit the whole

dispersion

curves of

p

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 are

intratetrahedral, nearest-neighbour

interactions.

The other three are intertetrahedral interactions

((O-O)2 corresponds

to interactions

between oxygen atom

pairs

like

(04-06)

and

(04-O~)

both

separated by

a distance

~ ~

(O-O)~

to interactions between atom

pairs separated by

~ where a is

~

~

~

/~

~

/~

the lattice

parameter).

There are then 10 force constants

(5 longitudinal (L

and 5 transverse

(T)

force

constants).

According

to our

approximation,

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 from

fitting

the hard modes have been fixed to values close to those found

by

Bethke et al.

[25],

The

equilibrium

condition

imposes

one relation between the 5 transverse force constants so that 6

independent

force constants are left as

adjustable parameters.

The

dispersion

curves for q

along

3 have been

(14)

fitted to determine these parameters. As shown in

figure

6 a shallow

dip

can be obtained near qo =

0.035 a*

along

the lowest 3 branch.

(In

Ref.

[25]

this

dip

could

only

be

reproduced by introducing

an ad hoc

phenomenological coupling

between the SM and

TAT modes.)

In order to

reproduce

the

temperature dependence

of the

modes,

it was found sufficient to allow for a

small linear

change

of the force constants

(mainly T(Si-Si) (cf.

Tab.

IV)).

As

expected,

the

TA~

mode is found to be

only slightly coupled

with the other

3~ modes,

so that the

dip

close to

T;

is

mainly

due to the interaction of the RTM

Q~(3~)

with the pure acoustic component

Q~(3~),

as assumed in the

phenomenological theory. Furthermore,

the

eigenvector

of the

dynamical

matrix relative to the lowest branch is

quite

close to the RTM « mixed » mode

Qa,

for any q

larger

than 0.005 a * In

particular

at the inc wave vector the

eigenvector Q

is :

Q

=

[0.96 Qa,

0.27

Qcl

/

~ 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 energy

phonons

of p quartz

along

the 3 and the A directions of the

reciprocal

space. The lines are the results of the

« nearly

rigid

tetrahedron model

» with the force

constants of table IV. The

points

are

experimental

values (Ref. [I]). (~ D) T

T,

=

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 the

vicinity

of the incommensurate wave-vector

along

the 3 direction.

Table IV. Force constants

ofthe

«

nearly rigid

tetrahedron

approximation

»

ofsection

4. L and T

refer

to the

longitudinal

and transverse

force

constants

of

the Born-Von-Karman model.

t = T

T;.

The values are in

N/m.

(si-o) (o,o)i (si,si) (o-o)~ (o,o)~

L oo

(17.487

0.006

t) (48.7

+ 0.0164

t)

2.0 5.96

T 14.737

(-

1.375 0.006

t) (-

1.31 + 0.0164

t)

1.61 1.70

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