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Amplitude expansion for the Grinfeld instability due to uniaxial stress at a solid surface
P. Nozières
To cite this version:
P. Nozières. Amplitude expansion for the Grinfeld instability due to uniaxial stress at a solid surface.
Journal de Physique I, EDP Sciences, 1993, 3 (3), pp.681-686. �10.1051/jp1:1993108�. �jpa-00246748�
J. Pltys. I France 3
(1993)
681-686 MARCH 1993, PAGE 681Classification Physics Abstracts
68.45
Short Communication
Amplitude expansion for the Grinfeld instability due to uniaxial stress at
asolid surface
P. Nozilres
Institut
Laue-Langevin,
B-P. 156, 38042 Grenoble Cedex 9, France(Received
8 December1992, accepted 5January1993)
Abstract The physical origin of the Grinfeld melting instability at the surface ofa uniaxially strained solid is briefly discussed. The calculation of the energy is pushed to the fourth order in interface displacement h. It is thus shown that the instability is usually subcritical
(first order).
Moreover, harmonic generation leads to grooves on the back side
(that
of thesolid).
As shown
by
Grinfeld in 1986[ii,
the surface of a solidsubject
to anon-hydrostatic
stress maydevelop
instabilities: amelting-freezing
wavedevelops
in such a way as to reduce the elastic energy. Note that theinstability implies
a transfer of matter, either from aliquid phase
or
through
surface diffusion. The interfacedisplacement
is due togrowth,
not to elastic strain.The
physical origin
of thatinstability
iseasily
understood [2, 3]. Consider a flat interfacez = 0 with a
liquid
at pressure pL. A uniaxial stress isapplied
to thesolid,
such that?zz = -PL, ?z~ = 0, a~~ = -pL + ao
(I)
The "effective chemical
potential"
that controls solidmelting
isfs
«zz~s = ~~~
Ps
where
fs
is the free energy per unit volume and ps thespecific
mass. For ahydrostatic
situation(ao
"0),
thephase equilibrium corresponds
to the nominal pressurep[.
When we stress thesolid,
we increase its energy, and thus we make it less favourable ascompared
to theliquid.
The
equilibrium liquid
pressure thus increasesby 6pL
the interface goes down [4]. Theexplicit
calculation is
straightforward.
Let aij, uij be the stress and strain tensors in the solid. In an infinitesimal transformation ~s variesby
6~~ =
j,»6uu if
6U«ll~
-
II
~"~~ll~
(2)
iseasily integrated. Assuming
that u~y =0,
we find6ps
=~~ (~ al
+~~ (3)
Ps Ps
where E and a are
Young's
modulus and Poisson's coefficient. Atequilibrium
spa
=6pL
= ~~~(4)
PL
from which we infer
6pL
and thehydrostatic
surfacedisplacement.
Assume now that the interface is
displaced by
an amounth(z),
as shown infigure
I. The uniaxial stress ao is reduced in thebumps:
theequilibrium 6pL
is smaller than the actualone
the solid grows further.
Conversely~
ao increases in thetroughs: 6pL
is too small in order to maintainequilibrium
the solid melts. Hence the Grinfeldinstability,
counteredby gravity
atlong wavelength
andby capillarity
at shortwavelength.
ds
dF~
i
I
~
x
Fig. 1. Geometry of the Grinfeld instabiity.
In order to describe the bifurcation it is
simpler
to calculatedirectly
the freeenthalpy
of the distorted state,G[h(x)].
The latter contains trivialgravity
andcapillarity
terms, which are bothpositive (I.e. stabilizing)
Go
=f
dzI( (ps pL) gh2
+~7h'2 (7h'~ (5)
the surface energy involves
@).
The stressgives
rise toa
negative
elasticcontribution, leading
toinstability(~).
Theorigin
of this contribution is onceagain
clear. If thegrowth
occurred at constant strain, the cost of energy would be zero
(both phases
are inequilibrium
to start
with).
But wethereby
break mechanicalequilibrium
at the surface: a forcedF~
= aodz
must be
applied
in order to compensate the bulk stress. If we do notapply
thatforce,
the solid relaxeselastically, thereby lowering
itsenthalpy by
an amount(I
These three contributions are additive. It is easily shown that cross terms arenegligible
as longas each contribution is small compared to internal energies +~ E per unit volume
(e.g.,
the change in density due tocapillary
pressure is very small !).N°3 AMPLITUDE EXPANSION FOR GRINFELD INSTABILITY 683
tie,
=f aodx
uz +
f
dra;ju;j
=
-( f
dra;juu
(61 where d, fi, are the
changes
due to relaxation.We limit ourselves to the
simplest
case of a semi-infinite solid medium. The calculation to order h2 for aplane
wave distortion was carried out in(2).
The netenthalpy
costis(2)
AG
=
(ps
+
pL)
g 2~~~~~ «(k
+k2j
(7)
The bifurcation threshold occurs at finite momentum
l~
~~(Ps PL) j
~~~7
(8)
?#
"~~
[(Ps
PL)g7)~~~
The obvious
question
is the nature of this bifurcation: is it first or second order? For thatpurpose, we must
push
the calculation of AG to order h~ this is thepurpose of the present
note.
As usual in similar
problems,
the calculationonly
makes sense if we allow for harmonicgeneration
due to non-linearities. We thus write thedisplacement
ash(z)
= a cos kz +fl
cos 2kz + 7 cog 3kz Due to translationalinvariance,
AG will contain termsa~, a~, fl~, li~..
,
a~fl, a~7, all?
Thus,
harmonicsautomatically
appear, withamplitudes fl
+~
a~,
7+~
a~ etc. The
leading
non-linearity
containsa direct part a~ and an induced part due to the second harmonic
coupling a~fl.
What we need is a detailed calculation of each term inAG(a, fl).
We then minimize withrespect to
fl
in order to obtainAG(a).
1)
Calculation of the elastic energy: We use the standardrepresentation
of stress in terms ofan
Airy
functionx(z, z).
The extra stress due to relaxation is~"
0~'
~~~0~'
~~~OZ~Z' ~~~
~For a
given displacement h(z),
we choose x such that theboundary
conditions aresatisfied,
?nn " ~PLI ?nt " 0
where n and t denote normal and tangent to the local interface.
Up
to orderh~,
theseboundary
conditions read
lazz
+ h'2 jw~~fizz]
2wm hi +,o h,2 = o(9)
azz + hi
jazz azz]
2azz h'2 +,o h' 11 +h'2)
= o(~)
For an absorbed epitaxial layer with small thicknessd(kd
< 1), the role of gravity is played byvan der Waals interactions.
The Airy function contains both harmonics I and 2
x = cos kz e~~
[al
z + ao) + cos2kx e~~~[biz
+ bo)(10)
Matching
the cos kx and cos 2kz terms in the twoboundary
conditions(9) provide
fourequations
that fix the four constants in terms of a andfl.
The calculation isheavy
as(9)
must be written atheight
h and not atheigth
0. But it isstraightforward, yielding
° )~ ~"~
~i ~~
al = -ao« + ao
(k~«~
+
(k Pi ii)
bo =
ao~, bi
= ao~)~ lj
It remains to be checked that the harmonic 0
(constant term)
in(9)
is satisfied: it is indeedidentically, ensuring
that the interfacedisplacement
does not induce uniform stress(which
would penetrate
throughout
thesample).
We thus have
h(z)
and aij(r).
It remains to calculate the freeenthalpy (6).
We canactually
calculate the two termsseparately~
and check that theidentify (6)
isobeyed (it
follows from thelinearity
of Hooke'slaw):
wethereby
have a check of ouralgebra.
The first term ofAGej
isAG[)~
= -aof
dzh'u~ (12)
The second term is
AG[)~
=~@ f
dr(2&)~
+(l a)
[&(~ +d)~] 2a&~~
&zz This can be transformed into~~S~
"~@ /
~~
l(~ ')i~Xi~
+ 2lX11Xix Xizl
Integrating
the last termby
part, wefinally
obtainAG[)~
=~
)~ / dr[Ax]~ l' f x[
dz,
dsi (13)
The steps of the calculation are now obvious
(I)
From &ij infer the strainflu
=jj' ldu
a d«
Sol (I
= xiz)
(it)
Then calculate thedisplacement
vi at interface z= h.
We thus obtain
AG[)~
=-2AG[)~,
as it should.Altogether
The
quadratic
terms were known(their
coefficient are+~
k).
Thequartic
terms are new.N°3 AMPLITUDE EXPANSION FOR GRINFELD INSTABILITY 685
2)
Minimization of the totalenerjy:
With the samenotation,
thegravity
andcapillary energies
are
Ggr
=
~~~
~~~~
~la~
+fl~l
~2 3 ~~~~
~~~~~
~4
~~
~
~~~ 6~~"~~
We must minimize the total AG.
(I)
At thebifurcation,
k=
kc,
ao = ac, AG becomesAG =
~~~ ~~~~
fl~
+
~~
k~a~
+ka~flj
4 16
The minimum is achieved for
fl
= -2ka2~~ (Ps
pL)
g 43~ ~
(16)
~
jk
aWe conclude that the bifurcation is first order
(subcritical),
a somewhatunexpected
result.Note the
importance
of second harmonichybridization:
without it the bifurcation would besupercritical.
We also note that b isnegative:
the interface thus flattens on theliquid
side anddevelops
grooves on the solid side~ as shown infigure
2., ,
' '
'
x
,
Fig. 2. A negative b develops grooves in the rear.
(it)
Atlarge
stress aojgravity
isnegligible.
All the modes between km and2km
areunstable,
with~~'
'~ ~~
~~~~
(the instability
is strongest at k=
km).
If we fixk,
we find that minimizationcorresponds
tolka~ ~ 2k2k kmkm (18)
2km 2 4
3
km 3k$
~~ ~
4
~~ ~
k ~ ~ ~
2 k 16 k
(k km)
(fl diverges
at k = km because the second harmonic is"soft").
Thequartic
term isnegative
if k < 1.87km, becoming positive
very close to2km.
3)
Evolution atlarge amplitude:
theexpansion
in powers of o is of no avail. Onepoint, however,
should be stressed: as it
displaces~
the interface cannot overcome the level z= 0 it had in the absence of
strain,
ao= 0. If the interface is
locally flat,
the distancehi
is such that11
,2)
(ps pL) ghi
=al (19)
2E
where al is the residual uniaxial stress on the upper terrace. hi
always implies
alowering
as
compared
to z = 0.Qualitatively,
it seemslikely
that rather flat parts shoulddevelop
near z =
0, separated by
narrow grooves(whose
role is to release the excessa~~).
Areally
reliabledescription
willnecessarily
be numerical. Note thatexperiments
seem to confirm sucha behaviour
(5).
Acknowledgements.
The author is indebted to S. Balibar for many fruitful discussions
(especially
for thesuggestion
that the interface cannot exceed its zero stress
position).
A related calculation was carried outby
J. Grilhd [6], who did not include the effect of harmonics: discussion with him was veryhelpful.
References
[ii
GRINFELD M.Ya, Dokl. Akad. Nauk SSSR 283(1985)
1139.[Sov. Phys. Dokl.
31(1956)
831].[2] NOzIERES P., Lectures at Collbge de France
(1988),
unpublished notes.Lectures at the Beg Rohu Summer School
(1989),
in "Solids far flom equilibrium" C. Godrkche Ed.(Cambridge
Univ.Press,1991).
[3] SROLOVITz D.J., Acta Metall. 37
(1989)
621. An extension to finite thickness layers is given in SPENCER B-J-, VOORHEES P-W-, DAVIS S-H-, Phys. Rev. Lent. 67(1991)
3696.[4j BALIBAR S., EDWARDS D-O-, SAAM W-F-, J. Low Temp. Pllys. 82
(1991)
l19.[5] See for instance TORII R-H., BALIBAR S., to be published in J. Low Temp. PA ys., and references therein.
[6] GRILHE J., to be published in Acta Metall.
J. Phys. I France 3
(1993)
687-692 MARCH 1993, PAGE 687Classification Physics Abstracts
61.50E 61.55H
Short Communication
Icosahedral quasicrystals: tilings of icosahedral clusters
Marek Mihalkovit and Peter Mrall~o
Institute of Physics, Slovak Academy of Sciences, CS-842 28 Bratislava, Czecho-Slovakia
(Received
13 October 1992, accepted in final form 10 December1992)
Abstract Tiling of four canonical cells, proposed by Henley
[1],is
a
promising
alternative to the Penrose-tiling and six-dimensional approaches to the structure of icosahedral quasicrystals.In this paper we briefly summarize the firts results of the structural modeling in the I-Almnsi and I-AlcuLi systems. The understanding of the structure of the stable quasicrystals, like I-
AlCuFe and I-AlPdmn, is of course of greatest interest; a possible canonical-cell approach is outlined.
1 Introduction,
The
advantage (and disadvantage)
of the canonical cell conceptis,
that it does notanticipate
any
simple description
inhigher (six)
dimensional space, nor within the 3D Penrosetiling scheme,
but is derived from thephysically grounded requirements
on the cluster-based icosa- hedral network. It seems that the two criteria(I)
maximaldensity
of the network and(it)
the two allowed kinds of icosalledrallinkages
b and c =bvi12,
which are inferred from the familiarstructures of
Frank-Kasper phases (a-Almnsi, (AlZn)49Mg~~)
areenough
to force a reason-ably simple
solution:tiling
of four canonical cells(TCC). Although
the constructiveproof
of thequasiperiodicity
of suchtiling,
as well as theproof,
that TCC is the densest bc-network(where
b and c are the two icosahedrallinkages)
still does notexits,
tranfer matrixtechnique
generates allexamples
of the TOG'S up to5/3
[3] and the Monte Carlo maximization of thedensity
at smallbackground phason
strain [4]produce random,
butperfect (without defects)
TCC
approximants
up to13/8
case(2440-2472
vertices per cubiccell).
2.
Tiling
of canonical cells.There are four kinds of canonical cells denoted A
(a
'bcctetralledron'),
B(half
of atrigonal
antiprism),
C(triangular pyramid)
and D(trigonal prism).
In anarbitrary
TCC structure,the B and C cells are
always paired
and heretoforethey
will be treated as a virtual BC cell.An
important point
is that the cells and bonds(b
andc)
can be decoratedby
the Penrose rhombohedra without gaps andoverlaps (the drawings
of cells and Penrose rhombohedra dec-orating
them can be found in Ref.[I])
and this decoration defines a set ofpacking
rules for the cells. The nodes of the TCC become 12-fold vertices of the inscribed rhombohedraltiling,
but these are not identified with the set of12-fold vertices in theperfect
Penrosetiling.
With thegain
of10il in thedensity
of the TCCcompared
to the 3DPT based 12-foldpacking
[2], thesimplicity
of thehigher-dimensional description
is lost.An
unique
property of the TCC isadjustability
of the nodes(and c-bonds) density,
which is controlledby
the parameter(,
related to a ratio of A and D cells. At zerobackground phason strain,
50il of the volume isoccupied by
the BCcells,
but it isconjectured
[4], that D-cells volume fraction isadjustable
from 8A to 15.8il(A
cells fill the rest of thevolume).
Considering
the known structures ofapproximant phases,
one can choose to maximize either Aor D cell type decoration at
(close to)
zerobackground phason
strain. Besidesthis,
TCC is an ideal candidate for thedescription
ofapproximant
structures: from allpossible
rhombohedralpackings,
it selectsonly
fewphysically
most relevantexamples
with maximal number of12-foldvertices without short b-fold
linkages
between them.Thus, given
the decoration of canonical cells andassuming
thatchemical/topological properties (atomic
local environments, chemicalcomposition)
of the decoratedA,
BC and D cells are neverexactly identical,
the relation betweenquasiperiodic
andperiodically
locked icosahedral clusterpackings
can be studied in terms of the relativedensity
of the cells.From the
modeling point
ofview,
the canonical cells are viewed as an interstitials in thepacking
of(interpenetrating)
icosahedralclusters, decorating
TCC vertices. The rhombohedral decoration of the TCChelps
one to see how the atoms are shared amongneighboring
clusters and to fill the voidsby
an additional atoms in arigid
manner.The
following
brief reports on the structural models and their agreement withX-ray /neutron
diffraction are based on the
816
TCCapproximant
with 592 nodes per cubic cell and Pa3 space symmetry [4, 5].Decorating
itby
the icosahedralclusters,
onestraightforwardly
obtains 97- 98it of the atomicpositions
in the structure. Whencompleted by a'glue'
atom, the modelscontain
43908,
51752 and 40356 atoms per cubic cell for the casesI-Almnsi,
I-AlcuLi andI-Alcufe, respectively.
3. Model of I-Almnsi.
There are many indications that the structure of I-Almnsi h
intimately
related to the o-Almnsi FrankKasper phase [6-9],
which isnothing
but the bccpacking
of(Mackay)
icosahedralclusters,
or a pure
periodic packing
of A-cells with ico clusters centered at thetiling
nodes. To define thequasicrystal (and arbitrary approximant crystal
based onTCC)
model we nowneed, only
to
specify
the decoration of theremaining
types ofcells,
BC and D.This can be done
quite easily, utilizing
the refinement of a-Almnsi structure [10] and acombination of
large
126-atom three-shell and 54-atom double-shell icosahedral clusters thatoccupy
respectively
'even'and 'odd'TCC nodes[iii.
The 3-shell clusters arecomposed
ofa small
Mackay
icosahedron(MI) (12 atoms),
an icosidodecahedron(30 atoms),
alarge
MI(12 atoms),
a triacontahedron truncatedalong
3-fold axes(60 atoms)
and a r-inflatedlarge
MI
(12 atoms),
where r=
Ii
+v$)) /2
is thegolden
mean. The detailsconcerning
atomic decoration will bepublished elsewhere,
but it can beshown,
that in such model 97il of the atomicpositions
aredirectly
determinedby
the a-Almnsi structure, ascompared
with about 70it in the 6D models[12,
13]. Due to(weak)
even-oddordering,
inherited froma-phase,
theN°3 ICOSAHEDRAL QUASICRYSTALS 689
quasicrystal
has fcc Bravais lattice in 6D. The calculateddensity
agree with theexperimental
value
(see
Tab.I)
and thereliability
factors are 9it forX-ray
and lsit for neutron diffraction(experimental
data were taken from Ref.[14]).
Table I.
Density
in the canonical-cells based models.Note that for the first two systems, where there exists a cubic 'I
Ii' approximant Frank-Kasper phme
with lattice parameterequal
to b(the
purepacking
ofA-cells,
12 A-cells per unitcube,
A-cells in the model have the same
density. Experimental
densities are taken from references[24],
[18] and [25]respectively.
'Glue'are called the atoms, notbelonging
to the icosahedralclusters, defining
a model.ALLOY PA pBc pD
calc.j (exp.)
GLUE ~BONDtat/b~l tat/b~l tat/b~l g/cm3 g/cm3j
li~l iii
138.0 136.0 130.7 3.63 3.63 3.3 12.66
A157CuiiL132
160.0 161.0 162.7 2.44 2.47 2.2 13.90A163Cu25Fe12
126.0 125.2 122.7 4.44 4Al 3.6 12.304. Model of I-AlcuLi.
The
I-phase belongs
toI-AlmgZn family
ofquasicrystals.
Like in previous case, its local structure isobviously
related to the structure of cubicFrank-Kasper phase (R-AlcuLi), though
the 5-shell icosahedral clusters [15] are of different type so called Samson
complexes capped by
rhombic triacontahedra. A structural refinement [16] leads to afollowing description: (I)
a small MI
(12 atoms); (2)
apentagonal
dodecahedron(20 atoms); (3)
a double-size MI(12 atoms); (4)
a 'soccer ball'(60 atoms) (5)
a triacontahedron(32 atoms).
Shells(2)+(3)
formthe so called small
triacontahedron,
r-times smaller than the one in 5-th shell.Utilizing
the network of canonical cells andpositioning
theselarge
clusters seen in the cubicR-phase
on the TCC vertices leadsagain
to a model that agrees well with theexperimental density
andcomposition (see
Tab.I).
Glue decoration iseasily
obtainedby
analgorithm, decorating
rhombohedral vertices,edges
andbody-diagonal points
ofprolate
rhombohedra[iii, decorating
BC and D cells.The model
predicts
aslight
decrease in the Li atomic concentration in thequasicrystal:
R-phase,
which is a purepacking
ofA-cells~
contains 32.Sit ofLi,
and in the present model BC and D cellsyield
31.I and 29.Sitrespectively (on
average 31.6ilLi).
Anotheradvantage
is~that with the icosahedral-cluster
description,
there is a well definedcorrespondence
between the classes of atomic sites of theR-phase
and thequasicrystal
that allows us tooptimize Al/Cu ordering~ minimizing
the R-factor of thecalculatedlexperimental single-crystal
diffraction data [18]. Theresulting reliability
factors are 6.lit forX-rays (56 independent reflections)
and 6.6ilfor neutron
(40 reflections)
diffraction. The details andcomparison
with other structuralmodels will be
published
elsewhere[19].
In both I-Almnsi and I-AlcuLi structures
a very small fraction of
glue
atoms can be con- sidered as a directproof
that thelarge
icosahedral clusters,experimentally
found in related FrankKasper phases~
can bearranged nonperiodically nearly
asefficiently
asperiodically.
5.
Preliminary
model of I-Alcufe and I-AlPdmn.The structure of the
'perfect'
and stablequasicrystals [20, 21]
with resolution-limited widths of the diffractionpeaks
attracts thegreatest
attention. Here we shall discussonly
the atomicskeleton of the TCC based
model~
blind to the atomicspecies.
Clearly,
the structure is of I-Almnsi type: atomsoccujy
with someprobability vertices,
faces andbody diagonals
of the rhombohedraltiling
and there are nomid-edge
sites. InI-Almnsi,
it is still reasonable to describe the first shell of icosahedral clusters as a smallMackay
icosahedron andassign
the atoms to theedge midpoints
of(some)
12-foldvertices,
whiledisplacive
modulation isexpected
to accommodate stresses, introducedby
too shortmid-edge/vertex
andmid-edge/mid-edge
distances. However, this iscertainly
not the case in I-Alcufe andI-AlPdmn,
where the diffractionanalysis
leads to a firstpseudc-icosahedral shells, represented by
apartially occupied pentagonal
dodecahedron[22].
The second shell of the icosahedral clusters(icosahedron
+icosidodecahedron)
is the one observed in I-Almnsi.We propose the
following
atomic structure for this class ofquasicrystals:
(I)
the two types ofpseudc-icosahedral
clusters 'even'(E)
and 'odd'(O)
are located at theeven and odd TCC vertices.
(ii)
thepositions
of the'glue'
atoms in C and D-cells interiors arestrongly
constrainedby
the ico clusters and are similar to thoseproposed
for I-Almnsi [11].E-type
cluster consists of the three shells:(1)
8 atoms on the vertices ofpentagonal
dodecahedron in < itI>-type
directions. There are fiveindependent
choices of the<ill>-type
directions with respect to the 20 ico 3-fold axes.(2) 'large'icosahedron
+ icosidodecahedron(42 atoms)
(3)
r-inflated icosahedron + triacontahedron truncatedalong
3- fold axes(yielding
20mutually nonsharing triangles)
12 + 60 atoms.Starting
from the secondshell~
theproposed
cluster is identical to that observedby
Fowler [10] in a-Almnsi. Note that the atomic sites of the r-inflated triacontahedron areprojections
of the
body
center motif in 6D.O-type
cluster is likeE,
but without the 3-rd shell.Along
3-fold icosahedraldirections,
all inter-clusterlinkages
are of E-O type and the 3-rd shell atoms of the E-clusters are the icosidodecahedron atoms of the O-cluster.Along
ico 2-folddirections,
O-O connection isagain perfectly compatible,
but in E-E case thepairs
of atoms of the truncatedtriacontahedron, falling
on the'top'
and 'bottom'faces of rhombicdodecahedron, decorating
thisbond,
are tooclosej
while in the I-Almnsi casethey
are shifted towards I and 2 thirds of the facediagonal (from
the r~~ and r~2points),
we assume there isonly
one atom at these two sites and occupy the two 'canonical'positions
with theprobability 1/2.
Anotherdegree
of freedom in the model is connected with thepossible
atomicjumps
in the I-st and from the 2-nd to the I-st(pseudo)-icosahedral
shell. This is due to the fact thatfully occupied
I-st shell can accommodate without conflicts 14 atoms 8 on 3-fold and 6 on 2-fold axes(on
the vertices of the r-deflatedicosidodecahedron)
which isnothing
but the usual bcc local environment.We have
already
checked that thedensity
of the structure(when
the atoms areassigned
masses of the
constituting
elementsweighted by composition)
match with theexperimental
value
(see
Tab.I).
Thespecification
of the chemical order and aprecise comparison
of thecalculatedlexperimental
diffraction data is on the way.N°3 ICOSAHEDRAL
QUASICRYSTALS
6916. Discussion.
All of the TCC-based models of icosahedral
quasicrystals
discussed here have their 6D ana-logues:
I-Almnsi [12]~[13],
I-AlcuLi[18], [23],
I-Alcufe[25].
As a matter of thefact,
thefrequent
occurrence of the icosahedral clusters in the model structure isanticipated
in bothapproaches, directly
in TCC-based one andthrough
theprocedure
oftailoring appropriate
atomic surfaces in
6ll-type
models. While in 6Dapproach
thequasiperiodicity
is apriori guaranteed,
thecomplexity
of the atomic surfaces increases whenadjusting
thedensity,
the TCC guaranteessignificantly higher density
of cluster-centers than any knownquasiperiodic bc-network,
but the 6D motif ofquasiperiodic
TCC is still not known and can beexpected
to be(very) complex.
In fact, recent results [26]suggest
that animportant questions might
be raised: if the details of the 'atom~c surfaces'(though
burried for anexperimental
observation inmodulation
of thelow-intensity
diffractionpeaks)
arephysically important,
the realisticpicture
of suchhypersurface might
include(cylindrical)
fractal features around the lines in- tersections of the 2-foldplanes [26].
But suchhypersurface
would be veryhardly,
if atall,
derivableanalytically.
At the sametime~
there arequite
strong reasons to seek the densestquasiperiodic packings (I)
both two main classes of the knowntruly quasiperiodic
icosahedralsphere packings l'unit sphere'
and'12-fold')
contain a small amount of a very poorsphere
localenvironments;
(it)
assuggested by
the TCCexample,
the densestpackings might
prove to be much moresimple
and uniform [27] inreal-space.
Weconjecture
that these considerationsmight
be valid on both inter-cluster as well as interatomic distance scales: theperfection
of the short and medium range orderproduces
fractal-like deterministic chaos around theedges
of the 2-fold
planes
of the atomic surfaces inperpendicular
space.References
[ii
HENLEY C.L., Phys. Rev. B 43(1991)
993.[2] HENLEY C.L., Phys. Rev. B 34
(1986)
797.[3j NEWMAN hi. and HENLEY C-L-, preprint.
[4) hiIHALKOVIC hi. and hiRAFKO P., accepted to Europhys. Lett.
[5] The coordinates of the TCC'S up to
13/8
case are available on request from the authors [6j CAHN J-W-, GRATIAS D. and MOZER B., J. Pllys. France 49
(1988)
1225.[7] ELSER V. and HENLEY Cl., Phys. Rev. Lett. 55
(1985)
2883.[8] GUYOT P. and AUDIER M., Philos. Mag. B 52
(1985)
L15.[9] MA Y. and STERN E.A., Phys. Rev. B 38
(1988)
3754.[10] FOWLER H.A., MOzER B. and SIMS J., Phys. Rev. B 37
(1988)
3906.[11] MIHALKOVIC M. and MRAFKO P., to appear in J. Non-Cryst. Solids
(Proceedings
of the LAM-8 Conference, Wien1992).
[12j DUNEAU hi. and OGUEY C., J. Pllys. France 50
(1989)
135.[13) YAMAMOTO A., in Quasicrystals, Ed. T. Fujiwara and T. Ogawa
(Springer-Verlag 1990).
[14j GRATIAS D., CAHN J-W- and hiOZER B., Pllys. fleb. B 38
(1988)
1643.[15] There might be a confusion, what is meant by cluster's shell: in case of I-Almnsi, the 'three-shell' 126-atom cluster has 5 shells~ when one considers a shell as a set of vertices of polyhedron, like in I-AlcuLi case. We have followed the terminology of cited works.
[16j AUDIER hi., PANNETIER J., LEBLANC hi., JANOT C., LANG J.-M. and DUBOST B-j Physica B 153
(1988)
136.[17j HENLEY C-L- and ELSER V., Pllilos.
Mag.
B(1986)
L59.[18jde BOISSIEU M., JANOT C., DUBOIS J-hi-, AUDIER M. and DUBOST B., J. Phys.: Cord. Matt.
3
(1991)1.
[19j MIHALKOVIC M. and MRAFKO P., submitted to J. PAys. Cond. Matt.
[20] TSAI A.P., INOUE A. and MASUMOTO T., Trans. JIM 29
(1988)
521.[21j TSAI A-P-, INOUE A., YOKOYAMA Y. and MASUMOTO T., Pllilos. Mag. Lett. 61
(1990)
9.[22j BOUDARD M., JANOT C., DUBOIS J-hi- and DONG C., Pllilos. Mag. Lett. 64
(1991)
197.[23] YAMAMOTO A., Phys. Rev. B 45
(1992)
5217.[24] AUDIER M. and GUYOT P., J. Phys. CoJloq. France 47
(1986)
405.[25j CORNIER-QUIQUANDON M., QUIVY A., LEFEBVRE S., ELKAIM E., HEGER C., KATZ A., GRATIAS D., Phys. Rev. B 44
(1991)
2071.[26j SMITH A-P-, preprint
[27] The uniformity of the rhombohedral tiling, inscribed into arbitrary TCC
(via
the classification of the vertex local environments defined in [2]) is surprisingly greater than in the perfect 3DPenrose tiling, I.e, the number of allowed local environments is smaller.