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A 6-D structural model for the icosahedral (Al, Si)-Mn quasicrystal

J.W. Cahn, D. Gratias, B. Mozer

To cite this version:

J.W. Cahn, D. Gratias, B. Mozer. A 6-D structural model for the icosahedral (Al, Si)-Mn quasicrystal.

Journal de Physique, 1988, 49 (7), pp.1225-1233. �10.1051/jphys:019880049070122500�. �jpa-00210805�

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A 6-D structural model for the icosahedral (Al, Si)-Mn quasicrystal

J. W. Cahn (1), D. Gratias (2) and B. Mozer (1)

(1) Institute for Materials Science and Engineering National Bureau of Standards, Gaithersburg MD-20899

U.S.A.

(2) C.E.C.M./C.N.R.S., 15 rue G. Urbain, 94407 Vitry, France (Reçu le 24 fgvrier 1988, accepté le 25 mars 1988)

Résumé.

2014

Un modèle périodique 6-dimensionnel est proposé pour décrire la phase quasipériodique icosaédrique Al-Mn-Si. Ce modèle est construit à partir de la représentation à 6 dimensions de la phase

cristalline cubique approximante 03B1. Dans le formalisme de Janner-Janssen-Bak, il consiste en trois couronnes

sphériques concentriques, l’une de manganèse et les deux autres d’aluminium centrées autour des n0153uds du réseau hypercubique à 6 dimensions, et deux couronnes additionnelles d’aluminium centrées au milieu des

diagonales principales de l’hypercube. Ce modèle vérifie les données des diagrammes de diffraction X de

poudre avec un facteur d’accord résiduel de 0,128.

Abstract.

2014

A 6-dimensional (6-D) periodic model is proposed for the Al-Mn-Si icosahedral quasiperiodic crystal. The model results from an embedding of the periodic cubic 03B1 structure in 6-D. In the Janner-Janssen- Bak description, it consists of three concentric spherical shells of respectively Mn, Al and Al aligned in perpendicular space around the lattice nodes and two additional shells of Al around the body centers. This

model is shown to match the X-ray powder diffraction data with a satisfactory residual R-factor of 0.128.

Classification

.

Physics Abstracts

61.10

-

61.50E

-

61.55H

-

64.70E

1. Introduction.

One of the principal problems in the study of the recently discovered quasiperiodic crystals (quasicrys- tals) [1, 2, 3] is the determination of their structure,

a prescription for the localization of the atoms. For

periodic crystals, the description of the structure of a single unit cell suffices ; for aperiodic crystals, the algorithm must include additional information. Be-

cause quasiperiodic structures can be described by a

known irrational cut of a periodic higher-dimension-

al structure, this additional information is contained in a single higher-dimensional unit cell.

We propose here a 6-D structure of an (Al, Si)-

Mn icosahedral quasicrystal, suggested by the results

of a Patterson analysis performed in both 3 and 6 dimensions with neutrons and X-ray powder dif-

fraction data [4, 5]. The 6-D auto-correlation or

Patterson function (PF) was found to be surprisingly simple (Figs. la, b) : only two structured peaks are found in the unit cell, one around the nodes and one

around the body centers, implying that all distance

vectors in 3-D belong to two sets : one set that is

close to being quasilattice translations, i.e. projec-

tions of 6-D translation vectors (nodes to nodes) and

the other being motif translations, that are all close

to being projection of body-centering translation vectors (nodes to body-centers). Comparison of X-

ray with neutron PF’s shows that these peaks have

well defined chemical structure : the body centering

translations are mostly heteroatomic distances as are

the outer reaches of the nodal peaks (Fig.1b). Such

a simple result suggests that all atom positions in the

3-D structure are either on or near quasilattice nodes (coming from projections of nearby 6-D lattice

nodes), or on points that are near projections of nearby body centers.

As confirmed by our PF’s [4], the periodic cubic

a phase [6] with 138 atoms per unit cell (in 11 orbits)

of the same elements is known to have an atomic arrangement quite similar to that of the icosahedral

phase [7-11]. Embedding the atoms of the a struc-

ture on the rational 3-D planes in 6-D shows that all atoms can be associated with either a nearby cell

node or body center. Therefore, we will assume in this paper that, in 6-D, crystal and quasicrystal have essentially the same structure, that the difference between them arises solely from the cut orientation, rational for the periodic crystal and irrational for the

quasicrystal, and thus we propose a 6-D model that is consistent with both the crystal structure and the simple two-peak 6-D PF of the quasicrystal. With a simple one parameter refinement procedure, the X-

ray intensities are fit with a residual R-factor of 0.128.

In the process of starting with diffraction data, and

Fourier transforming it to obtain PF’s, we were naturally led to the higher dimensional structural

Article published online by EDP Sciences and available at http://dx.doi.org/10.1051/jphys:019880049070122500

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1226

Fig. 1.

-

X-ray (a) and neutron (b) Patterson functions

displayed in the 5-fold plane spanned by [1, 0, 0, 0, 0, 0]

and [0, 1, 1, 1, 1, T ] basis vectors. The dashed lines in the neutron map represent negative contours and depict

atomic distances that are primarily heteroatomic.

descriptions of the Janner-Janssen-Bak [12-15] type, rather than those descriptions that are based on

decoration of tilings [16-18].

2. Experimental.

X-ray and neutron powder diffraction data show that the finely powdered rapidly solidified A173Mn21Si6

used is almost entirely icosahedral phase [19] con- taining only 2 % of the hexagonal crystalline {3 phase

and 1 % of f.c.c. Al [20]. On heating at 30 °C/hr, the alloy eventually transforms entirely into the {3 hexagonal phase at 700 °C. A fine powder specimen

of the « cubic phase Al73Mn16Si11 was also prepared

and studied by both X-ray and neutron diffraction.

The positions of the X-ray reflections of the icosahedral phase have been shown to fit a 6 integer indexing [21] in 3-D, related to a 6-D icosahedral

primitive lattice of parameter A

=

0.6497 nm at

room temperature, with a relative accuracy better than 5 x 10- 3. X-ray integrated intensities have been carefully formulated in absolute units (square

of a number of electrons per A3) using a well defined

standard of Ni3Fe alloy. The patterns were indexed according to the scheme proposed by Cahn, Shechtman and Gratias [21]. Since no systematic

extinctions were found in either X-ray and electron

microscopy diffractions that would reveal the pres-

ence of glides mirrors and/or screw axes in 6-D, we

assumed the 6-D space group of the structure to be the direct product of m35 with the simple hypercubic

6-D lattice. Details of the X-ray data analysis are reported elsewhere [22].

The average width of the peaks as measured both by X-rays and neutrons leads to an average corre- lation length better than 40 nm. The peak widths depend on both the perpendicular and the parallel components of the 6-D K-vectors in good agreement with the frozen-in phason model of disorder origi- nally proposed by Bak [23] and elaborated by others [24-26].

3. Crystallography in 6-D.

It is necessary to choose between two structural

descriptions of atoms in the 6-D unit cell. In one, the atoms are assumed to be localized at points in 6-D,

as they are in 3-D. The 3-D structure is then obtained by collecting all the atoms in a carefully

defined neighbourhood of a 3-D plane and projecting

them onto this plane [27-29]. This is the construction for obtaining the quasilattice from 6-D, and also for

generating aperiodic tilings from higher dimensional lattice points.

In the other description, the atoms in 6-D are

characterized by 3-D surfaces [30] ; the 3-D structure

is obtained by cutting the 6-D structure with a 3-D plane, the points of intersection of the physical 3-D plane with the atom surfaces in 6-D identify the

actual locations of the atoms in the physical 3-D

space. This simple cut-without-projection is the

standard mathematical construction relating a quasi- periodic function to a higher dimensional periodic

function [31]. It is, for example, how the 3-D PF is obtained from the 6-D PF. Although these two descriptions can often be made equivalent, the latter

method lends itself more naturally both to analysing

the experiments and the subsequent modeling of the

structure : the experimental procedure is more nat- urally understood as a collection of data in reciprocal

space issuing from a 6 to 3-D projection (correspond- ing to a cut in direct space) rather than cuts in

reciprocal space that would seem to obliterate inac- cessible data.

Most of the conventional concepts used in 3-D

crystallography remain valid in the higher dimension-

al space. The space group is defined as the set of the 6-D isometries which superimpose the equivalent

atom surfaces ; the little group of the atomic site is the normalizer of the corresponding atom surface,

i.e. the subset of the symmetry elements of the 6-D space group which leaves the atom surfaces globally

invariant. The atomic sites of the j-th orbit are

defined by their associated 3-D surface Vj, which, in

the general case are functions of both the physical

(4)

space (usually called parallel space and denoted by

its basis vectors Ell) and the complementary space

(more often called perpendicular space and denoted

by E_L). The Fourier coefficient of a reflection K of the 6-D reciprocal lattice is obtained by :

where fl is the volume of the elementary 6-D unit cell, k¡ and kl are respectively the parallel and perpendicular components of the 6-D momentum transfer vector K, fj are the atomic form factors,

which depend only on k¡, and uj is a 6-D space variable running over the atom surfaces Vi. For the

special case where the atom surfaces are aligned along the perpendicular space, the points uj that belong to Vj can be decomposed into a parallel component, say rj, and a perpendicular component

ul ; the relation (1) transforms into :

where the integration is now over a volume in the

perpendicular space.

Because of the irrationality of the cut, each point

’ contained in the 6-D unit cell will be explored once

and only once in the real structure extended to

infinity. The stoichiometry and the density of the

real structure are therefore those of the 6-D model.

Designating by 03BC the multiplicity (defined as the

index of the normalizer of a representative atom of

the j-th orbit onto the point group of the 6-D space

group), one obtains the atom fraction cj of the species in the j-th orbit by the relation :

and the mass density p :

where Mj is the atomic weight of the species j.

4. A tentative model.

The simple 6-D PF suggests a model in which all atom surfaces V J are aligned in E 1. and centered about either nodes or body-centers, and are

stretched out entirely in E 1. with icosahedral sym- metry. This is, of course, an idealization that ignores

the small displacement in parallel space away from such symmetric positions found in the EXAFS

[9, 10], the a crystal and confirmed in our PF’s.

The strong similarity between the PFs of the

a crystal and the quasicrystal suggests that we examine the a crystal in 6-D. In the rational

approximant geometry [32, 33], T (=1.618... ) is replaced by 1 in the equations for the cut plane [21],

each of the three cubic basis vectors becomes a

specific 6-D vector : for example the (1, 0, 0) basic

vector of the a structure becomes (1,1,0, 20131, 1, 0 ) in 6-D, and atoms localized at (x, y, a ) in 3-D

appear at

in 6-D. In this way, all 138 atoms (in 11 orbits) of the

known a structure can be placed as points on

rational planes in 6-D. Table I shows that 8 of the 11 orbits, including both Mn orbits, project along El onto the vicinity of nearby nodes, while the remaining 3 Al orbits project closely to nearby body

.

centers. The parallel and perpendicular components of the distances of each orbit from these points is

also given in this table. Because there is a small

parallel component for each orbit, we conclude that

all atoms of the a structure in 6-D are indeed fit into

a space that is close to being entirely perpendicular

to nodes and body centers (the three orbits around the body centers could have been fit around edge

centers, but that would not have been consistent with the PF). Since both the PF and the a structure revealed that the atom surfaces in 6-D are approxi- mately confined to the 3-D perpendicular subspace surrounding these points, we assume that the orbit surfaces are 3-D volumes in El with icosahedral symmetry. The simplest shapes consistent with these facts, thick concentric spherical shells in El , are the

basis of the model. From each orbit of the a crystal,

we obtain :

(a) whether the shell from this orbit is centered

on node or body center ;

(b) the radius of the atoms from the center, which

we will take as the mid-point of its shell ; and (c) the thickness of the shell, which will be taken

as proportional to the multiplicity of that orbit. The total volume of all orbits is fixed by the density and composition of the icosahedral phase, rather than

that of the a phase.

Applying these rules, we find that the 11 orbits in the crystal can be merged into just 5 orbits in 6-D ; a

Mn and two (Al, Si) shells around the node, and two (Al, Si) shells around the body center. All inner and

outer shell radii are completely determined by the stoichiometry, the density of the a structure and the

above rules. There should have been a sixth orbit from the Al(7) Wyckoff position of the a structure,

but we found that it made very little difference if this

was distributed among the Al(I) and Al(II) 6-D

orbits. Density and composition (see relations (2)

and (3) give two constraints. The remaining par-

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1228

Table I.

-

The 6-D embedding of the cvstructure showing the closest approach to node and body center of

atoms projected along E 1. ; bold face highlights the parallel and perpendicular distances from these points to

the attached a-orbits.

ameters for the initial model come from the crystal

orbit radii and the apportionment of atoms among the orbits, as shown in table II and figure 2.

The two manganese orbits of the crystal merge into a single nodal shell. Five aluminum orbits merge to form a contiguous shell surrounding the mangan-

ese shell ; thus 96 of the 138 atoms in the a structure

belong to a single compound shell (manganese on

the inside and aluminum on the outside) around the

6-D nodes, comprising the entire second Mackay [34] shell plus 6 aluminum atoms from one of the a-

orbits (Al(7)) that has been called glue. Around this

compound shell is another aluminum shell containing

12 atoms from the glue orbit Al(6) plus the remaining

6 of the previous Al(7) orbit.

The remaining 30 aluminum atoms are merged

into two orbits about the body centers. One of them,

with 24 atoms, arises from the inner Al shell of the

Mackey icosahedra. Although these atoms in 3-D

are approximately half-way between the central vacancy and the Mn icosahedron, it is important to emphasize that this orbit is not associated with the

midpoint of an edge. The last orbit of 6 Al atoms

that belongs to the body center originates from the remaining glue atoms in the a structure.

5. Refinement parameters.

In the present model, the orbit surfaces are taken as

the volumes within 3-D spherical shells in El ,

centered on points of high symmetry, and having

unit occupancy. The orbit is specified with just two parameters, the inner and outer radii, that are taken

from the a structure and not obtained from optimi-

zation. As such, the model does not allow for

disorder, which is an interesting features of these quasicrystals. A simple way to handle disorder is to introduce Gaussian terms in the structure factors,

like static Debye-Waller terms (SDW), which spread

the orbits as in ordinary crystallography, but, in 6-D,

take on additional meaning. While the spread in parallel space displaces the atoms by small amounts,

the perpendicular components of the spread dis- places atoms in 3-D by a large quasilattice translation vector having a small perpendicular component. The effect is a gradual decrease in site occupancy espe-

cially at the fringes of the orbit. This method of

introducing the SDW into the model specifies which

kind of disorder is expected in 3-D : when the SDW

causes orbits of two chemical species to spread into

each other, a chemical disorder results, including the

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Table II.

-

The initial 6-D model showing the merging of the eleven ce-orbits into five 6-D orbits.

(1) Cooper and Robinson notation [5].

(2) Adjusted for density p

=

3.587 glcm3 and stoichiometry Al79Mn21.

(3) In 6-D lattice parameter units (A

=

0.6495 nm ).

Fig. 2.

-

The proposed 6-D structure seen in the 5-fold

plane ; the glue atoms, found around the edges of the main nodal Mn-Al shells (gray region), can be viewed as bridges

between adjacent nodal shells.

possibility of Mn close neighbors ; when the shells spread into empty space, it leads to an occupancy disorder. The disorder would mostly affect those

vacancies and atoms generated by cuts at the fringes

of the 3-D surfaces.

In this simple model, 20 optimization parameters

are possible : each orbit has a maximum and a

minimum radius and could have two SDW terms.

Since there are relatively few peaks in the powder

diffraction spectra that are well defined and not

affected by either the f3 hexagonal phase or the f.c.c.

Al (among the 39 reflections that have been de-

tected, only 17 have significant intensities and not

altered by the other phases), we introduced only one global SDW, denoted Bll, into the refinement by :

Since the experimental intensities were converted into absolute units, no additional parameter was

required for scaling. Both primary and secondary

anomalous absorption terms AF’ and AF" were

introduced in the calculated Fs.

The minimization was performed using the follow-

ing functional:

where u F2 = 21 Flu F, and 0- F is the standard devi- ation of the reflection F. If we make no correction for background intensity, 0-F is well approximated

by -11 -A 1 L-P,with /.k as the multiplicity and Lp as the

P

Lorentz polarization factor [35]. For a direct com- parison with what is conventional in crystallography,

we also calculated the residual R-factor defined by [36] :

and a more meaningful weighted residual factor

w R defined by :

The results of the refinement procedure are given

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1230

in table III and displayed in figure 3. The optimized

value of the SDW parameter is Bll

=

3.14 A2 giving

residual factors of R

=

0.128 and wR

=

0.257. Cal-

culating the intensities for all the possible reflections

.

2

.

with kl less than 2,/-,- (where A is the 6-D lattice A

parameter) revealed no missing experimental peaks compared to the calculated intensities in the exper-

imentally accessible range of kll. A reconstruction of the electron density map in 6-D along the 5-fold

plane has been performed by Fourier transforming

the experimental structure factors, each being given

Table III.

-

General characteristics of the final refined model compared to experimental data (N and M

notations for indexing the peak are defined in reference [21] of the text).

(1) Defined as k; = 2 sin 0 A with A

=

1.79028 A (CoKa radiation). ° (2) In number of electrons/ Å 3 .

(3) AF = (Fobs - F cal ) .

y Fobs

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Fig. 3.

-

The observed and refined calculated X-ray structure factors versus the parallel momentum transfer.

the sign of its corresponding theoretical value

(Fig. 4).

We examined the sensitivity of X Z with respect to

changing orbit radii, and to the introduction of a

global perpendicular SDW factor. Although the gradient of X 2 with respect to the perpendicular

SDW was slightly negative, none of these additional variables had a strong enough effect on X 2 to

warrant their introduction into the minimization.

Fig. 4.

-

Density map obtained by Fourier transforming

the experimental structure factors with the signs obtained

from the calculated ones.

6. Discussion.

This model was suggested by two observations on

Patterson maps of the icosahedral phase and the prototypic crystalline a structure, and the assump- tion that these two structures are simply different

cuts of a single 6-D structure :

(1) finding only two 6-D peaks in the quasicrystal

PF implied that all interatomic distance vectors in 3- D could be associated with two sets ; quasilattice translations, that are projections of 6-D node to

node vectors, and motif translations that are projec-

tions of 6-D vectors from nodes to body centers ;

(2) finding that for short distance vectors ( 2 nm) there was a one-to-one correspondence

between the interatomic distance vectors in the known a structure, and those in the icosahedral

quasicrystal.

Embedding the a structure in 6-D revealed that it too was consistent with only two peaks in the PF and, knowing how we wanted to group the atoms in 6-D, permitted us to use the atom positions in the

a structure for constructing a model. The simplifi-

cation of the a structure in 6-D is remarkable.

The satisfactory agreement between calculated and observed diffraction intensities is an indication that this model is a good starting point for possible

further refinement. Solid spheres aligned in perpen- dicular space are only approximations to forms having icosahedral symmetry to be used as cut surfaces to give structures in which identical atoms decorate vertices of a 3-D generalized Penrose tiling.

When the radius is 1.14, the sphere has the same

volume as the cut triacontahedron that gives the

vertices of the 3-D Penrose tiling in which the edges

of the rhombuses are along 5-fold axes and have length 0.46 nm. The hollow spherical shells with outer radii less than this, e.g. the Mn shell, can be interpreted in the 3-D structure as such tilings with

an ordered decoration of atoms and vacancies. Most of the vacant sites arise from the central hollow,

which itself is an approximate tiling in which the shortest distances are 1.09 nm along the 3-fold axes,

and 1.24 nm along the 2-fold axes. These are the distances between vacant centers of Mackay

icosahedra in the a structure. With respect to the basic tiling, these sites correspond to high local symmetry vertices which are centers of a tesselation of 20 prolate rhombi ([37] Henley, Duneau and Katz, private communications). There are also

aluminum atoms substituting for manganese atoms

owing to the difference in the outer radius and 1.14.

If this were an abrupt edge to the shell, it would give

rise to an ordered set involving all quasilattice

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1232

distances, but we suspect it to be the result of disorder and accounted for by a possible perpendicu-

lar SDW factor. Similarly, the larger radii of the nodal Al orbits can be interpreted as tilings with

shorter edge vectors.

Because the 6-D embedding of the « structure

does locate atoms as points and not as 3-D surfaces,

there is considerable latitude in the construction of the atomic surface in a 6-D structure of a that is also

a model for the quasicrystal. For the simplest model,

we chose spherical shells aligned in perpendicular

space, centered on either nodes or body centers.

Because we forced all atom surfaces to lie along perpendicular space in 6-D, atoms in 3-D are on

exact projections of nodes or body centers. As a result, all distances are of the form In +-mr, with

special restrictions on n and m. For instance the Mn atoms in the a crystal are 0.46 nm from the center,

and the inner Al atoms at 0.28 nm instead of 0.48 and 0.24 nm respectively as reported by Cooper and

Robinson [6] for the a structure.

Our treatment of the data led us naturally to choosing the Janner-Janssen-Bak description of ideal quasiperiodic structures, i.e. those that have discrete diffraction patterns with a finite basis, and formu- lated on the mathematical theorem that all quasi- periodic functions can be described as planar cuts of higher dimensional periodic functions [30]. This description is thus completely general for all ideal quasiperiodic structures. The descriptions based on

a finite set of decorated tilings are less general and represent a first approximation where only local

environments (those within each tile) have been

taken into account. In a general quasiperiodic struc-

ture, the curving of the atom surfaces permits infinitely varied configurations. Because we aligned

our surfaces, we did not, in this initial model, avail

ourselves of this generality : our structure can be

considered as a relatively complex superposition of

different tilings resulting from projections of a 6-D, mostly vacant, body-centered cubic lattice ordered to give a primitive translation group.

The atom surfaces in this model are disjoint, but

there are obvious regions in 6-D of close approach

and it is there that the « glue » atom orbits appear.

Glue atoms have recently been shown to be inti-

mately involved in third and to some extent shared

shells in the structural description of the a crystal [38]. The place of closest approach in the icosahedral

phase is seen, in the 5-fold plane, to involve all three glue orbits. Here, glue atoms could link adjacent

nodal shells, just as these atoms do in the a structure. Such linkages are apparent in the PF. One of the glue orbits seems to be the outer part of the

large 6-D shell containing all of the second shell of the Mackay icosahedra. The gap between the two

nodal glue orbits may just be a way of representing decreasing site occupancy. The body centering glue

orbits are partially inserted into the region of closest approach between two nodal orbits.

The present model includes all atoms and has the correct density. Examination of the predicted 3-D

structure (without the SDW disorder) reveals rela- tively few complete Mackay icosahedra just as there

are few decagons in a 2-D Penrose tiling ; instead,

there are many recognizable fragments that inter-

penetrate. The initial model is, of course, exactly quasiperiodic ; even the way the SDW factor intro- duces disorder in the optimization, leaves discrete peaks, with a Laue monotonic background and no

other diffuse scattering. The refined value of the SDW in parallel space is rather large, approximately

four times what is usually observed in good quality crystals, which is the confirmation of the appreciable

disorder expected in quasicrystals.

There have been a number of models that consider

packing of identical units because such models have factorable structure factors. In an earlier paper [11],

we proposed a model with a strictly quasiperiodic

array of perfect two-shell Mackay icosahedra, with

the remaining Al (glue) atoms omitted. The density

was therefore low. The fit with the spectra was poor, but still an improvement over that calculated from models that place a single scatterer on a 0.46 nm 3-D

Penrose tiling. There are other factorable models that pack Mackay icosahedra in 3-D, most notably a

random instead of a quasiperiodic packing [39, 40]

with the principle concern being the prediction of

line broadening.

With two parameters per orbit, the 6-D spherical

shell description is comparable to the three coordi- nates that describe a general Wyckoff position in 3-

D crystals. Instead of 11 orbits with more than 20 coordinate parameters needed to give the 3-D atom positions in a, we found that, because of the

merging of the orbits in 6-D, five shells (ten par-

ameters) and a single global SDW fitting parameter sufficed to give a good fit of the diffraction spectra of the icosahedral phase. Considering that we are modeling an aperiodic phase, these represent few parameters. We did not use the radii as fitting parameters, but took them directly to conform with

the known a structure. They could have been used to improve the fit with data. It is noteworthy that the

6-D description of the a crystal also has an economy of parameters. The 3-D a-orbits calculated from the 6-D structure are a good fit, with the Mackay

icosahedra having m3 rather than icosahedral sym- metry. A similar 6-D CsCI type description was.

successful for the R-phase in the Al-Cu-Li system.

Whether or not other types of Frank-Kasper phases, especially those with higher coordination numbers,

can also be economically depicted in higher dimen-

sions remains to be seen.

(10)

Acknowledgments.

We gratefully acknowledge our colleagues Dr Y.

Calvayrac, S. Lefebvre, M. Bessiere and A. Quivy

to have allowed us to use their X-ray data prior to publication. We thank Drs P. Bak, M. Duneau, C.

L. Henley, M. Jaric, A. Katz, S. C. Moss and E.

Prince for their many stimulating suggestions and

discussions on the subject. Finally, we would like especially to thank Dr J. Bigot, Mr A. Dezellus and Mrs S. Peynot who prepared the samples, in a remarkably reliable and reproducible way.

References

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(1985) 1005-1012.

[2] SHECHTMAN, D., BLECH, I., GRATIAS, D. and CAHN, J. W., Phys. Rev. Lett. 53 (1984) 1951-

1953.

[3] For a complete bibliography, see MACKAY, A. L.,

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[4] CAHN, J. W., GRATIAS, D. and MOZER, B., Phys.

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[5] GRATIAS, D., CAHN, J. W. and MOZER, B., Phys.

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[6] COOPER, M. and ROBINSON, K., Acta Crystallogr. 20 (1966) 614-617.

[7] GUYOT, P. and AUDIER, M., Philos. Mag. B 52 (1985) L15-L19.

[8] ELSER, V. and HENLEY, C. L., Phys. Rev. Lett. 55

(1985) 2883-2886.

[9] MA, Y., STERN, A. and BOULDIN, C. E., Phys. Rev.

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