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Note on ultrasonic effects due to third-order elastic coefficients in icosahedrally symmetric systems
Shmuel Goshen, Joseph Birman
To cite this version:
Shmuel Goshen, Joseph Birman. Note on ultrasonic effects due to third-order elastic coefficients in icosahedrally symmetric systems. Journal de Physique I, EDP Sciences, 1994, 4 (7), pp.1077-1084.
�10.1051/jp1:1994185�. �jpa-00246965�
Classification
Physics
Absn.acts43.25 61.50E 62.65
Note
onultrasonic effects due to third.order elastic coefficients in icosahedrally symmetric systems
Shmuel Y. Goshen
(1)
andJoseph
L. Birman(2)
(') Physics Dept.,
Nuclear Research Center, Negev, P-O- Box 9001, Beer-Sheva 84190, Israel (2)Physics Dept.,
CityCollege
of theCity
University of New York, New York, NY10031,U-S-A-
(Received 6
September
J993, ievised14 Maiih 1994, accepted 2/ Maic.h 1994)Abstract. The identification of
alloy
systems of Almn and other compounds with macroscopic icosahedral symmetry bas been reported. In this work we discuss severalmacroscopic
tensorproperties
which maydistinguish
between icosahedralpoint
group symmetry I, from either fuit isotropic SO (3) symmetry, or cubic O symmetry.Emphasis
is given to trie structure of trie third order elastic coefficient tensor and the non-linear elastic coefficients which ansein I-symmetry systems.
Corresponding
sound velocities are obtained these can permitexperimental
measure-ments using ultrasonic
techniques.
One of the very
interesting
recentdevelopments
m condensed matterphysics
has been thediscovery
andsynthesis
of avariety
of cristalline systems whose symmetry isnon-crystallogra- phic.
That is neither thepoint
group symmetry nor the space group symmetry are among the32,
or 230(respectively)
groups of 3-dimensionalcrystallography.
The first of these new discovenes to our
knowledge
was thesynthesis
of an Al-Mnalloy
with
stoichiometry approximately Al~mn by
Shechtman et ai.il ]. They
carned out electron- diffraction studies which demonstrated that the pattem of scattered electronspossessed
icosahedral symmetry. In
addition, algorithms
have beendeveloped
formdexing
of thelocations of observed diffraction spots, consistent with the
predictions
ofquasipenodic
translational order.
Quite recently, large perfect samples
ofquasicrystals
have been available owmg to newdevelopments
in materialpreparation.
This haspermitted
the first observation ofdynamical
X- ray diffraction effects as earlierpredicted [2],
on aquasicrystal
of « f-c-c- » Al-Pd-Mn,including
the observation of the Borrmanneffect,
or « anomalous transmission at theBragg angle
»[3]. Samples
on which the expenments wereperformed
were of centimeter size. With suchsamples available,
it can bepossible
to determine novelmacroscopic
properties of theseicosahedral materais.
In this note we restnct attention to some of the novel
physical,
measurable macroscopicconsequences of icosahedral
point
symmetry. Tophrase
theproblem
moreexactly
we ask what type and order of tensonal response coefficient can be used to charactenze the presenceJOURNAL DE PHYSIQUE -T 4 N' 7 JULY J994 ~9
1078 JOURNAL DE PHYSIQUE I N° 7
of icosahedral symmetry, and
distinguish
fromisotropic (complete
SO(3)),
or cubic(point
group
O) symmetries
? We suppose asingle crystal
of suitable size isavailable,
and can bealigned
so that suitablepolarized
measurements can be made.As a first step we recall
[4]
that the components of thephysical
response functions forcrystal
systems can be classified as cartesian tensors, the indices of which possess somepermutational symmetries.
These tensors are reducible into a sum of irreducible components. Thus in anisotropic
SO(3)
system the response functions transform as a sum ofsphencal harmonics,
and the irreducible representations areconventionally
denotedD~~'.
In the presence of G point groupsymmetry
the bases of eachrepresentation
D~~~splits
into irreduciblerepresentations
of G
D~~~
= D~~ e D~"~ e
where D~'~,
D~'~
are irreducible
representations
of G. Thenby
measunng the components associated with different irreduciblerepresentations #1',
effects which arespecific
to the lower («spht »)
symmetry can be identified. The number ofphysical
parameters is determinedby
the number of times that theidentity representation
appears.Applymg
this to our case, m table I we grue the standard character table of the icosahedral group I and thecompatibility
(orsplittings)
table of the representationsD'~~
under I. From this table, and the earlier workby Ripamonti [5]
we can find a vanety of «higher
order» tensonal
properties
which may be used to differentiate betweenO,
I, and SO(3).
These are given intable II.
Table I.
a)
Chaiac.tel tabledefining
theiii educible representations
of
the icosaheclial point groiip I.b) Compatibility
tablefoi-
ieductionof
D~~~of
SO(3),
iestricted to point gioiip I.a)
E 15
C~
20 C~ 12 C~ 12Cl
A
~ ~ ~
,à
+ ,,<'5
' ~
2 ~ 2
~ ~ j ~
,,1- ,/j
+
~ ~
2 ~ 2
G 4 0
H 5 0 0
b) Do
=ADj =F,
D~=
H D~
=F~+G
D~
=G+HD~
=Fi+F~+H
D~ =A+Fj+G+H
An interesting and
practical
case is of nonhnear elastic wavepropagation
where the third order elastic(TOE)
coefficients are used. For the icosahedralsymmetry
there are fourTable II.
Highei
oider tensoipiopeities (see Ref [2]).
Physical
property, Number of parametersPhysical
propertyrepresenting
relationbetween : Isotr. I
Symmetric
tensor and 3 4 6 56 Third order elasticsquare of
symmetric
coefficientstensor
subject
also to Maxwell relationSymmetric
tensor and 4 5 9 126 Second orderphoto-
square of
symmetric
elastic coefficientstensor
Second rank
symmetric
2 3 6 90 Second order resis-tensor and a
totally
tance second ordersymmetric
fourth rankmagnetothermal
con-tensor
ductivity
Second rank
general
2 3 7 135 Second order magneto-tensor and a
totally
electric powersymmetric
fourth rank tensorSecond rank
symmetric
5 6 12 216Piezomagneto-
tensor and a fourth resistance
rank tensor
symmetric
inside the first
pair
and the second
pair
parameters, while for the
isotropic
case there are three. For the second order elastic coefficients of the linear elastic wavepropagation
bothsymmetries,
the isotropic and icosahedral haveonly
two parameters. The 2 +4 = 6 parameters of materais of icosahedral symmetry can be
jnvestigated by
ultrasonics. Five of the parameters are the same as t'orisotropic
symmetry.How
significantly
the sixth parameter differs from zero will grue thespecial
properties relatedto the icosahedral symmetry.
By
theseinvestigations
it isimpossible
to decide about the existence of a center of symmetry becausethey
are based on second order tensors. Nonlinear effects in elastic wavepropagation
may anse from several different causes. We shall discuss and calculate the
following
twocases. First, the
amplitude
of the elastic wave may besufficiently large
so that finite stramsanse. An
initially
sinusoidallongitudinal
wave of a givenfrequency
distorts as it propagates,and energy is transferred from the fundamental to the harmonics. The amount of energy
transferred
depends
on the TOE coefficients and is a way ofexperimentally determmmg
them.Second, a materai which in its undeformed state behaves m a lmear fashion may behave in a
nonhnear fashion when mfinitesimal ultrasonic waves are
propagated, provided
that asufficient amount of externat static stress is
imposed. Usually
this is in the form of uniaxial orhydrostatic
compression. The formulas for the velocities forlongitudinal
and transverse1080 JOURNAL DE PHYSIQUE I N° 7
modes, in the different directions under different extemal stresses
permits
theexperimental
determination of TOE coefficients. We use the well-established notation of Green
[6].
The
Lagrangian
symmetric strain matrix y isgiven by Mumaghan [7]
asy =
(ÀJ à) (1)
where J is the Jacobian matrix :
ôXj
J~t
w(2)
ôat
Here a,
(1=1, 2, 3)
are the cartesian coordinates of a point in the unstrainedsolid, X,
(1 = 1, 2,3)
are the coordinates at time t of the point in the deformed solid, and à is the unitmatrix.
The
engineering
stress tensor(which
is notsymmetnc)
is definedby
T=J~ (3)
Y
where
#
is the strain energy, and its form isspecified by
the symmetry of the solid. The equations of motion in theLagrangian
coordinates for the deformationsu~ are
~Î
ôT~~$
~ P° ~i~~l
j J
where u, =
X,
a, (1= 1, 2, 3 ), po the undeformed
density,
and ü isÎ~
~ in theLagrangian
formulation.
Now
wnting
for the strain energy çS, when the z axis has a 5-fold symmetry, and the y-axis isof a ?-fold symmetry
~ ÀL
(Y22
Y33 Y23 Y32 + Y33 TII Y13 Y31 + TII Y22 Y12Y21)
++ ~~ ~
~'~~
(Yjj
+ Y?? + Y33)~3
2
m(yjj
+ y~~ +y33)(Y22
Y33 Y23 Y32 + Y33 Yl1 Y13 Y31 + Yj Y22 Y12 Y2j ++
n(yj
y~2 Y33 Y11 Y23 Y32 Y21 Y12 Y31+ Y21 Y13 Y32 + Yii Y12 Y23 Y31 YiiY22)
+
~[YÎ3
+(TII
+YÎ2)
Y33YÎ3(Yll
+Y22)
+ 2 TII Y22 Y33+ ~ Y13 Y31 TII + ~ Y23 Y32 Y22 ~ Y13 Y31 Y3~ ~ Y23 Y32 Y33
+
(Y13
+Y31)(Yll
Y22)~ +~(Y22 Yll)(Y12
Y23 + Y32Y21)
~ Y12 Y21
(Yl~
+ Y~l + 4 Y12 Y23 Y31 + ~ Y13 Y~2 Y211(5)
The five terms whose coefficients are (2 M +
),
M, f + 2 m, m and n,respectively,
areisotropic. The calculation of these terms is descnbed in Green
[6].
The last term, which is anisotropic but hasonly
icosahedral symmetry, was calculatedby
Butler's tables. We shall also need the expression for çS when the z axis has a 3-fold symmetry and the y axis has a 2-foldsymmetry. Then this last term becomes
~
ÎÎ °'~' /7
°'~~°'~'
°'~~~°'~'
~ °'~~~ °'~~ ~ °'~~ °" ' ~ +j YÎ3(Yll
+
Y22)
+)
TII Y22 Y33 + Y12
Y21(~
Y22 ~ TIIY31)
+ Yl~
Y31(~
Y3~ ~ TII ~Y22)
+ Y23
Y32(~
Y33 Y22 ~ TII +(Y12
Y23 Y31 + Yl~ Y32Y21)
/j
+
'j (Y13
+Y31)(5 YÎI
~YÎ2
~ Y11 Y22 ~ Yl1 Y3~ + 8 y22 y~3~ Y12 Y21 + 16 Y23 Y32
~/
Y13 Y31 ++'~~ (yj7
y71+ y17 y7j)(16
vii 4 yjj 12~~)j
(6)
9First case.
Harmonic distortion of a finite
amplitude
harmonic wave. For a pureLongitudinal
ultrasonicwave we get
Po =
(2
» + À)(u,,u fia,,11,,,,) (7a)
p
is thenonlineanty [6] parameter
:P
=
3
+
~~Îi/ i
i~~~ (7b)
Here :
K
=
3 g in the direction of 5-fold axis K
=
0 in the direction of 2-fold axis
(7c)
K
=
~
g in the direction of 3-fold axis 9
The solution up to the second harmonic
[6]
r (a, t =
Ai
sin(ka
wt + A7 cos 2(ka
mi(8a)
Ai
is the fundamental waveamplitude.
A~,
theamplitude
of thegenerated
second harmonicA~ =
j (A)
k2 ap). (8b)
Therefore,
thediscontinuity
distance[6]
is :~
p
2po(~f)~
ii~ ~~~~where w
=
?
~f
and uo is theamplitude
of the wave at a 0.Second case.
Measurement of the variation of ultrasonic wave
velocity
withapplied
externat stress.1082 JOURNAL DE PHYSIQUE I N° 7
Let us define
[6]
:il : the wave
velocity,
pjj the unstrained
density,
P an
imposed
externathydrostatic
pressure,T an
imposed
externat uniaxial stress in aspecified
direction.We get the
following
equations for thevelocity,
V, of the waves in the directions of symmetry, with constraints indicatedExtemal
hydrostatic
pressurelongitudinal
wavealong
ail symmetry directions.poil~= (2p
+À)- ~(7À +10p +6i+4m +2g). (9)
3À +2 p
II. Externat
hydro~tatic
pressure ;transverse wave
along
ail symmetry directions.pov~=p-
~[6p
+3À +3m-~nj (10)
(3À +2p) 2
III. Externat compressive stress
along
5-fold axis ;longitudinal
wave I stress.p~V~=(2p+À)-~~~~~ ~(~~~(4À+10p+4m+6g)+~~~+À+2ij,
+-R R R
(11)
IV. Externat compressive stress
along
2-fold axislongitudinal
wavealong
5-fold axis 1 stress.Po~'~= ~2/l+À)~~~ l~~~12f-~/
(m+À+2JL)l~(2À +JL)1. ('2)
V. Externat
compressive
stressalong
3-fold axislongitudinal
wave I stress,v~~?/~+~~-~~iili~jil~io~+~m~+~+2fH~'2~+~/~~'.
"~~
VI. Externat compressive stress
along
2-fold axislongitudinal
wavealong
3-fold axis 1stress.T
[~(_~~(m+À+2Rl+@~~~~~~~Î
~~~~p~~i'2=(2p+À)-~~~
+2p)
RVII. Externat
compressive
stressalong
5-fold axi~longitudinal
wavealong
2-fold axis 1 stress,p~V~= (2p
+À)- ~[2i-~~ (m+À +2p~+~~~ ~~~gj (15)
(3À +2p)
p RVIII. Externat
compressive
stressalong
2-fold axislongitudinal
wave I stress.p~V~= (2p +À)-
~[~
~~(4À
+10p+4m)-~~
+À
+2ij. (16)
(3À +2p)
p pIX. Extemal
compressive
stressalong
5-fold axistransverse wave I stress with
particle displacements along
?-fold axis.p~V~=p-
~
~
[m+4p+4À +£-~~~~~~~~j. (17)
À
+2p)
p pX. Externat
compressive
stressalong
2-fold axistransverse wave
along
5-fold axis 1 stress withparticle displacements
I ~tress.p~v2=
~_
T
[~~~
~ ~nÀ
(3À+2p)
~~~~~/~)
~ ~~4p~
p
~' ~~~~
XI. Externat compressive stress
along
?-fold axis ;transverse wave
along
5-fold axis 1 stress withparticle displacements
1 stres~.p~
V~
= p
~
~
m
2 ~~ ~ ~ ~~
(
+2p) 2p
(19)In conclusion we have
presented
results which can be used in the determination of the icosahedral component of macroscopic elastic response of aquasicrystal.
Ii would be of considerable interest to have such measurements made on the new,large-size
materais, in order to check these results, and aise with an atm ofrelating
tomicroscopic
theories ofelasticity
ofquasicrystals recently proposed [9].
A recent
expenmental
review of thephysical
properties ofquasicrystals (10] heightens
interest in the measurement of macroscopic properties of these systems. A
noteworthy
relatedwork
by
Amant, de Boissieu and Zarembowich[1Ii
measures elastic propertiesultrasonically
under
hydrostatic
pressure. No anisotropy was found andthey reported
measurement ofonly
two
independent
linear combinations of the four TOE coefficients (see hereEqs. (9, 10)
and Tab. I in[1Ii).
Acknowledgments.
We thank Prof. F. Fumi, and a referee for
pointing
Dut the relevant work of reference [5].
One of us (JLB) thanks Prof. A.Goldman forsending
thepreprint, reference[3(,
beforepublication,
aise Prof. R. Colleta for discussions ofpossible Dynamical
Diffraction exper-iments which can be carned Dut on the
large quasicrystals,
and Prof. A. Zarembowitch andDr. B. Perrin for discussions of their recent work
[1Ii
The work wassupported
in partby
aPSC-FRAP-CUNY grant.
1084 JOURNAL DE PHYSIQUE I N° 7
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inChengde,
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