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Submitted on 1 Jan 1990
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Cubic approximants in quasicrystal structures
V.E. Dmitrienko
To cite this version:
Cubic
approximants
in
quasicrystal
structures
V. E. Dmitrienko
Institute of
Crystallography,
117333, Moscow, U.S.S.R.(Received
7 mai 1990,accepted
infinal form
7 August1990)
Abstract. 2014 The
regular
deviations from the exact icosahedral symmetry,usually
observed at the diffraction patterns ofquasicrystal alloys,
areanalyzed.
It is shown thatshifting, splitting
andasymmetric broadening
of reflections can be attributed tocrystalline phases
with the cubicsymmetry very close to the icosahedral one
(such pseudo-icosahedral
cubicapproximants
may be called the Fibonaccicrystals).
The Fibonaccicrystal
is labelledas Fn+1/Fn>,
if in thiscrystal
the most intense vertex reflections have the Miller indices{0,
Fn,
Fn + 1}
whereFi
are the Fibonacci numbers(Fi
= 1, 1, 2, 3, 5, 8, 13, 21,34...).
The deviations of x-ray and electron reflections from their icosahedralpositions
are calculated. Thecomparison
with availableexperimental
data shows that at least four different Fibonaccicrystals
have been observed in Al-Mn and Al-Mn-Sialloys :
2/1>
(MnSi
structure), 5/3> (03B1-Al-Mn-Si), 13/8>, and 34/21>
with the lattice constants4.6
Å,
12.6Å,
33.1Å,
86.6 Å respectively.
It isinteresting
to note that there are noexperimental
evidences for the intermediate
approximants 3/2>, 8/5> and 21/13>.
Thepossible
space groups of the Fibonaccicrystals
and theirrelationships
withquasicrystallographic
space groups are discussed.Classification
Physics
Abstracts61.16 - 61.50e - 61.55H
1. Introduction.
Among
manyproblems
concerning quasicrystals
the mostimportant
ones are1)
thecharacterization of
quasicrystalline
atomic structure and2)
the nature of the disorder inquasicrystalline alloys
[1,
2]. Imperfectness
ofquasicrystal
structures is observed aspeak
splitting, shifting
andasymmetric broadening
in x-ray and electron diffractionpattern
[1-9J.
Inthe icosahedral
glass
model,
the disorder lies in the basis of thequasicrystalline
structure. Inother theoretical
models,
theperfect quasicrystalline
structures arepossible
and theimperfectness
of realsamples
issupposed
to be a result of frozenphason
strains[1,
2, 5,
6].
In the
present
paper anotherapproach
isdeveloped.
It is shown that in many cases theasymmetry
and deviations of theBragg
reflections from the icosahedralpositions
can be connected with the presence ofcrystalline ,phases
whichapproximate
thequasicrystalline
phase
veryclosely.
Below, only
cubicapproximants
are considered in detail(they
are calledthe Fibonacci
crystals).
The sequence of Fibonaccicrystals
with everlarger
unit cells forms achain between conventional
crystals (with
small unitcells)
andquasicrystals.
Thus,
aboveall,
the Fibonaccicrystals
give
us a convenientstarting point
for theunderstanding
of thequasicrystalline
phase.
Although
thepossibility of crystal approximants
has been discussed in many papers[1,10-17],
the solidarguments
for their real existence are not numerous(excepting a-Al-Mn-Si).
Itcan be shown from the
comparison
between theoreticalpredictions
and availableexperimental
data that at least four different Fibonaccicrystals
can exist in Al-Mn and Al-Mn-Sialloys ;
their lattice constants are about 4.6
À (MnSi
type
structures),
12.6Á
(a-Al-Mn-Si),
33.1 À
[15],
and 86.6Á (see below). Although
the latterapproximant
looks rather fantastic(the
unit cell contains more than 4 x104 atoms !),
its existence seems to be confirmedby
x-ray and electron diffraction. In otheralloys (Al-Li-Cu, etc.)
the deviations from the icosahedralsymmetry
are also observed[6-9]
and theiranalysis
will begiven
elsewhere. Fortwo-dimensional
quasicrystals,
theperiodic approximants
have been considered in details earlier in reference[18],
where theimportance
of suchapproximants
was shown.The remainder of this paper will
proceed
as follows : in section 2 we discuss thesymmetry
of the Fibonacci
crystals
and relations between theBragg
reflections in cubic and icosahedralstructures. In sections 3-4 the deviations of cubic reflections from their icosahedral
positions
are calculated.
Then,
in section5,
thepossible
structure of the Fibonaccicrystals
is illustratedby
thesimple
low-orderapproximant
with 8 atoms per unit cell(MnSi
structure,P213
spacegroup). Finally,
in section 6 thecomparison
of our results with theexperimental
data aregiven.
2.
Crystallography
of Fibonaccicrystals.
Both the icosahedral
quasicrystals
and their Fibonacciapproximants
can be obtained from the suitableprojection
of six-dimensional cubic lattice on our three-dimensional space[10-12,
16,
17,
19].
In this paper we use moresimple approach, considering quasicrystal (or crystal)
as asuperposition
ofdensity
waves with some set of thereciprocal
lattice vectorsQ :
where p
(r )
is adensity.
Thisapproach
is convenient if one focuses on the diffractionpatterns
rather than on thereal-space
structure.Any reciprocal
lattice vectorQ
of icosahedralquasilattice
may be written as a linear combination of six basic vectorsQm :
where the
Nm are integers
and may bethought
of as the six-dimension Miller indices of theBragg
reflections. At first we consider theprimitive
icosahedral lattices. As the basic vectorswe will use six vertex vectors
Qvm
directed toward the icosahedron vertices(the
fivefoldaxes).
We have chosen as(100 000)
the most intense reflection of thisseries,
which for Al-Mn occursat
2.9 Â -
and corresponds roughly
to interatomic distances :d
= 2 w/
1 Qv.
1
= 2.17Á.
Theadvantage
of this choice is that the most of the intense reflections can be indexed with a smallnumber of nonzero
Nm [19]. Using
three-dimensional Cartesiancoordinates,
those six basicvectors
Qvm
may be written asbasic vectors
Qvm by
six vectorsQnm
of a cubic lattice with the Miller indicesequal
to theFibonacci numbers :
an is the lattice constant. The n-th order
approximant
is convenient to label as(F n + 1/ F n> ;
its latticeconstant an
increases with n :The
relationship
between an
and aR was first obtained in reference[10].
Forexample,
in ournotation the well-known a-Al-Mn-Si
crystal
should be labelled(5/3)
(because
of another choice of basic vectors, in reference[10]
thisapproximant
waslabelled (1/1),
but thisproduces
some difficulties inlabelling
of low-orderapproximants
with n =1, 2).
To avoid confusion it should be noted that in the
crystallographic
literature some definitechoice of cubic axes is used
[20] ;
if the space group is Pa3,then,
as a result of thischoice;
thefirst index of hk0 reflections must be even ; to meet the case,
Fn
andF n +
1 inequation (4)
must be
permuted
ifFn +
1 is even(see
anexample
in Sect.5).
Using equations (2)
and(4),
theh,
kand f
Miller indices can beexpressed
viaNm:
For another
indexing
scheme,
that of reference[21],
thequasicrystal
reflection(h /h’,
k/k’,
f /Î’)
corresponds
to the cubic reflection with the Miller indiceshFn-3
+ h’
Fn-2’
kF,,-3 + k’F,,-2
and iF,, -3 + iF,,
-2-The cubic vectors
Qnm
canapproximate
the icosahedral vectorsQvm
veryclosely,
even if theorder n is not very
large.
Forexample,
theangular
deviation from the fivefold axis is about 2° for(230),
0.75° for(350),
0.29° for(580),
and 0.11 ° for(8,
13,
0).
Using Qnm
as the basic vectors inequation (2),
we obtain a set ofreciprocal lattice
vectorswith cubic
symmetry.
Infact,
for cubic lattice any three basic vectors may beused ; however,
it is convenient to use those six-vector
basis,
because in this case the vectors of cubic latticeare close to the vectors of
quasicrystal
with the sameNm
(examples
aregiven below).
Thepoint
symmetry
of cubic lattice is 23 orm3 (that is,
thesymmetry
is lower than icosahedralpoint
symmetry
532 or532/m).
TheLandau-theory
calculations of thespatial
structure of Fibonaccicrystals [15]
show that the mostpossible
space groups arePm3
orPa3
(if
bothFn
andFn +
1 areodd,
thepossible
space groups areIm3
orI213).
It isinteresting
to note that the Landautheory
predicts
the same absolute values of thestrongest
harmonics inPm3
and inPa3,
whereas thesigns
of p Q
arepredicted
to be different.Although
theLandau-theory
approach
ishardly
suitable for a detaildescription
ofcrystal
structure, there is ahope
that the
qualitative
results,
such asspatial
symmetry
of a cubicphase
and thesigns
of theFourier harmonics
p Q,
are correct.If n = 1,
the basic vectorsbecome 111 0}
andsymmetry
of the Fibonaccicrystal
isIm3m
[17].
When the
point
symmetry
reduces from icosahedral tocubic,
the icosahedralsymmetry
axes(planes)
becomeunequal.
As aresult,
the icosahedral reflections maysplit
up into severaltypes
of cubic reflections.Inequality
of thesymmetry
axes(planes)
isespecially
evident if weput
icosahedron into cube(see
Fig. 1).
Fig.
1. - Therelationships
between symmetry axes in cubiccrystals
and icosahedralquasicrystals.
Thesymbols
of axes andpseudo-axes (with asterisk)
are evident from thefigure.
It is clear that instead of
thirty
twofold icosahedral axes,only
sixtwofold (100)
axes areheld in cubic
crystal.
The othertwenty-four (,r 2 r 1 >
directions may beregarded
as twofoldpseudo-axes,
because for these directions the deviations from twofoldsymmetry
are not verylarge (in
the Fibonaccicrystals
but not in anarbitrary
cubiccrystal !).
Then,
insteadof twenty
threefold axes, in a Fibonacci
crystal
we haveeight
threefold (111)
axes and twelve threefold(7» 2 Io>
pseudo-axes.
The twelvefivefold (lrO>
axes are turned into twelvepseudo-axes (all
of them are
equivalent). Finally,
instead of fifteen mirrorplanes,
we have three mirrorplanes
and twelve
pseudo-planes
which are normal to twofold axes andpseudo-axes
of cubiccrystal
respectively.
The
inequality
between axes andpseudo-axes
leads toinequivalence
andsplitting
of reflections. Forexample,
one caneasily
obtain from(2)-(4)
thatthirty
twofold(110000)
reflections(directed along
icosahedronedges) split
up into twotypes
of cubic reflections : six(2
Fn,
0,
0 ?
reflections andtwenty-four
{F n +
1,Fn,
F n - 1}
reflections which are directedalong
twofold axes andpseudo-axes (approximately).
The vectors of these reflections formdeformed « icosahedron » in the
reciprocal
space of the Fibonaccicrystal.
The threefold icosahedral reflectionssplit
up also into the cubic reflections of twotypes ;
forexample,
the( 110 001 )
reflections are turned intoeight
{Fn - , F n -1’ F n - 1}
reflections and twelve{F n’
Fn - 2,
0}
reflections. Those icosahedralreflections,
which areparallel
to mirrorplanes,
split
up into cubic reflections of threetypes :
twelve of them areparallel
to mirrorplanes
of cubic lattice and the rest 48 reflections are close topseudo-planes.
As aresult,
the(111 000)
reflections
split
up into{F n + 1 + F n - , F n + , O} ,
{F n + 2, F n - 1, F n - 1 } ,
, and{2
Fn, Fn,
F n +
t}.
Finally,
anarbitrary
icosahedral reflectionsplits
up into fivetypes
of cubic reflections(5
x 24 = 120 reflections inall).
Thequantitative description
of reflectionsplitting
and
shifting
isgiven
in the next sections.At the same
time,
the Fibonaccicrystals
have many common features withquasicrystals.
The
general
feature ofquasicrystalline
lattices is the inflation of the reflectionwavelengths
with factors T orr 3[
1, 2].
In the Fibonaccicrystals
theapproximate
inflation takesplace [ 151.
Forexample,
in addition to the basic « icosahedron », formedby thirty
vectors{F n +
1,F n,
F n - 1}
and ( 2
Fn,
0,
0 ) ,
we see(for
rather smallNm
in(2))
the sequence oflarger
(2
Fn +
k,0,
0 },
where k = ±1,
±2,
... ; each « icosahedron » differs from the basic oneby
factors about
r k (the
T inflation).
The Fibonaccicrystal,
of course, contains the smallest« icosahedron », formed
by
thevectors (21 1 ) and {200},
(or
verydegenerate
«icosahed-ron », formed
by
vectors ( 1 1 0) and ( 200 )
of the sameseries)
whereas thereciprocal
space ofquasicrystals
contains(in
thegeneral case)
the infinite series of ever smaller icosahedra. Onthe other
hand,
theapproximate
T3-inflation
takesplace
for thepseudo-fivefold
{F n’ F n + l’ O}
reflections: if allNm are
not verylarge,
one obtain from the basic{F n’ F n + l’ O}
vectors the{Fn - 3, F n - 2, O}
reflections,
but neither{Fn - l’ F n’ O}
nor{F n -
2,F n -1,
O}.
However,
in the Fibonaccicrystals
the inflation rules are notrigorous
and,
for
example,
the{F n - 3’ F n - 2’ O}
reflections can be obtained forsufficiently
large
Nm
(but intensity
of reflections is small ifNm
arelarge).
It is
interesting
to note that theapproximate
T3-inflation
becomes morepronounced
in theFibonacci
crystals
withPa3, Im3,
andI213
space groups because of the extinctions rules and because of theparity
of the Fibonacci numbers whosecycle
is three(odd,
odd,
even,...).
Forexample,
let us considerPa3
group ; if n = 2 and the basic reflections are(210) ,
then theT3-inflated {850}
reflections arepossible,
whereas the intermediatereflections (320)
and{530}’
are forbiddenby
the extinction rules ofPa3
group(in
{hkO}
reflections h must beeven).
In the end of this section we discuss the
symmetry
of those Fibonaccicrystals
whichapproximate body-centered
and face-centered icosahedralquasilattices.
In thebody-centered
quasicrystals E
Nm
is even ; in this case, h + k+ f
is even for all reflections and the Fibonaccim
crystals
are bcc too. Moreintriguing
situation is in the case of the face-centeredquasicrystals
(like
A165Cu2oFe15),
where allNm
are of the sameparity :
it follows fromequations (6)
that all Miller indices are even for all reflections of thecorresponding
Fibonaccicrystals.
Thus,
choosing
another cubic unit cell(twice
smaller in eachdirection),
we return to the sameindexing
of the Fibonaccicrystal
as in the case ofprimitive
icosahedral lattice(with
oneimportant exception :
the inflation factor is now about T for alltypes
ofreflections).
3. Déviations of cubic reflections from icosahedral
positions.
In the Fibonacci
crystal,
the deviationAQ
of anarbitrary
cubic reflection from its icosahedralposition
can be written as a sum of the deviationsâQnm
of the basic reflections :where
àQ_ = Qnm - Qvm.
To obtain theexplicit
form ofAQ,,.,
we use therelationship
between an
and aR(see
Eq.
(5))
and thefollowing expression
forFn :
After
simple
calculations we obtain forâQnm :
where m =
1,
For any Fibonacci
crystal,
dQnm
are normal to thecorresponding
basic vectorsQvm;
thus,
the deviations of the absolute values ofQnm
from the absolute value ofare
very small(of
the order ofA n 2
Qv,,,
This is also valid for any fivefold reflection.For other
strong
reflections the deviations ofQ
are of the orderof
1 An 1
for weak reflections(large Nm)
the deviations may be not very small. Thesimple
calculations show(see figures
below)
that both the vertex vectors and theedge
vectors of the Fibonaccicrystals
fit thecorresponding
icosahedral vectors veryclosely.
Therefore,
carefulanalysis
of x-ray and electron diffractionpatterns
is needed todistinguish quasicrystals
and their Fibonacciapproximants.
,4. Diffraction
patterns
of the Fibonaccicrystals.
To show the main features of the cubic distortions of icosahedral
quasicrystals,
we illustratethe above
equations
withcomputer-simulated pictures.
Atfirst,
let us consider the x-raydiffraction on
powder
samples.
In this case,only
the absolute values of thereciprocal-lattice
vectors are relevant(but
not theirdirections). Figure
2 shows acomputer
simulation of x-raypowder
diffractionpatterns
for three Fibonaccicrystals.
The half-width at half-maximum of individual reflection is chosen 0.009Â-
1 andquasicrystal
parameter
aR = 4.60 À
(about
those ones observed in real
samples) ; positions
of icosahedral and cubic reflections arecalculated from
equations (2)-(4).
Forsimplicity,
the total intensities of all reflections(before
splitting)
are chosen of the same value and the intensities of thesplit
components
of eachreflection are
supposed
to beproportional
to theirgeneral multiplicity
factors(24
forhkf,
12 forhk0,
8 for hhh and 6 forh00). Figure
2 shows that inthe (5/3)
approximant
thesplitting
ofstrong
reflections iscomplete.
Inthé (13/8)
Fibonaccicrystal,
the values ofsplittings
arecomparable
with the reflectionwidths ;
as aresult,
the reflections are broadenedasymmetrically
and theirapparent
widths are different. Forthe (34/21)
Fibonaccicrystal,
theFig.
2. -Computer
simulation of x-raypowder-diffraction picture
for (5/3),
(13/8),
and(34/21 )
Fibonaccicrystals.
Thepeak positions (when
notevident)
are markedby
vertical lines ; forsplittings
are so small that the reflections are almostsymmetrical
and their shifts from theicosahedral
positions
arehardly
observable(see
belowFig. 7).
For non-shown intermediateapproximants (8/5) and (21/13),
thesigns
of thesplittings
and, hence,
thesigns
ofasymmetry
areopposite.
The electron-diffraction
pattern
is shown atfigure
3 for the case ofpseudo-fivefold
symmetry
(here
and below the incident beam is assumed to fallalong -
z direction so that thex, y and z axes form the
right-hand triad).
Thispicture
is universal for the Fibonaccicrystals
ofany
order ;
theonly
difference is on a scale. The scale can be determined from thepositions
of thestrongest
edge
reflections(2
Fn,
0,
0 }, {Fn + l’ F n’ F n - 1}
which are at about 3Â-’.
Thepositions
of allspots
infigure
3 are determined from theprojections
of thereciprocal-lattice
vectors
hkf
on theproperly
chosen xand y
axes : xhk p = h and yhk p =(Tk + f ) / It
isimportant
that the most of relevant vectors deviate from their icosahedralpositions
notonly
in the
plane
of thepattern
but inoff-plane
direction too : Zhkf =(rf2013A;)/B/1+T;
suchoff-plane
deviations can cause adisappearance
of some weakspots.
Fig.
3. -Universal
pseudo-fivefold
electron-diffraction pattern of the Fibonaccicrystals (incident
beam fallsalong -
zdirection).
All x-coordinates areinteger :
xhkl = h.Only
about one fourth of the pattern isshown ; the
eomplete picture
can be obtainedby
the mirror reflections : x --+ - x and(or)
y - - y. The scale of the pattern are determinedby
thepositions
of the most intenseedge
reflections(Q =
3 A - 1 ) ;
for the different Fibonaccicrystals
thosepositions
are markedby
arrows. The Miller indices are shown for outer reflectionsonly ;
the indices of :inner reflections can be obtained from theouter ones after
multiplication by
factor T -i (i
= 1, 2,3, ...)
andround-up
to the closestinteger.
Theinnermost ten reflections are of the
type (200)
and ( 21 1 ) .
Theapproximate
T inflation isclearly
seenin the
figure (pentagons
with strongest distortions are marked with solidlines).
Pseudo-twofold axes areshown
by
dashed lines.Several features of the
pattern
should be noted. The reflections are deviated from theiricosahedral
positions
in x-directionmainly ;
therefore,
the twofold h00 reflections aredeviated at radial
direction,
whereas thepseudo-twofold
reflections(shown
with dashedlines)
pseudo-twofold axis directed at 72° to the
x-axis).
For(pseudo-)twofold
reflections the deviations areusually
smaller than for other reflections withcomparable
1 Q 1.
. Note also the« zigzag »
character of the deviations
(this
isclearly
seen atglancing angle).
The deviations arelarger
for reflections withsmall
[ Q
1
and(or)
withlarge Nm ; they
areespecially
visible when at least oneof the Miller indices becomes small. The inflation process
(multiplication
ofhkf
by
the factorT and
round-up)
decreases the distortions of thespots
from their icosahedralpositions (see,
for
comparison, proposition
4 from Ref.[16]).
The
(pseudo-)threefold
patterns
are obtained as aprojection
of thereciprocal-lattice
vectors on any axes which are normal to a
(pseudo-)threefold
axis. Thesepatterns
can be of three differenttypes ;
two of them are shown atfigure
4 and the third one is the mirrorreflection of
figure
4a(the
choice of axes isdisplayed
at thefigure).
At the threefoldpatterns
the spots
are deviated intangential
directions inzigzag
manner, whereas at thepseudo-threefold
pattern
the deviations are directedalong
x-axis and all x-coordinates areinteger.
Fig.
4. - Threefold(a)
andpseudo-threefold (b)
electron-diffraction patterns. Other outer reflectionscan be indexed for
(a) using
60°-rotation(cyclic permutation
of the indices andchange
of theirsigns)
and for(b) using
the mirror symmetry(x - -
x and(or) y - - y).
The indices of inner reflections can be obtained as for thepseudo-fivefold
pattern. The twofold andpseudo-twofold
axes are shown with the dashed lines. The third type of the pattern(the
threefold one with zIl 111 ])
is the mirror reflection of(a).
There are also three different
types
of(pseudo-)twofold
patterns
(see
Fig. 5).
To avoidconfusion,
it should beemphasized
that thepseudo-twofold
patterns
(which
correspond
theincident beam direction
along
thepseudo-twofold axes)
have the exact twofoldsymmetry
because of the inversion
symmetry
of the electron-diffractionpatterns.
The differenttypes
ofspot
displacements
are observed for the reflectionslying along
symmetry
axes(radial
displacement)
andalong pseudo-axes (tangential displacement mainly).
Theoff-plane
deviations are also
present
both at thepseudo-twofold
and at thepseudo-threefold
patterns.
5. A
simple example :
MnSi cubiccrystal.
It was shown earlier that two
approximants
were observed in Al-Mn and Al-Mn-Sialloys :
Fig.
5. -Twofold
(a)
andpseudo-twofold (b)
electron-diffraction patterns ; the third type of the pattern(pseudo-twofold)
is the mirror reflection of(b).
The spots show thepositions
of reflections but not their intensities.approximant
of this seriesshould
be(2/1)
with the space group eitherPm3
orPa3
[15] (or
close tothem)
and with thefollowing
strong
reflections:{ 210 } , {211}
and{200}, {231}
and{400} ;
the lattice constant should be aboutT 2
smaller than that of a-Al-Mn-Si.Turning
to thecrystallographic
handbooks,
we find apossible
candidate[22] :
MnSicubic
crystal
(a
= 4.6Â)
withP213
space group
(close
toPa3).
This structure containsonly
eight
atoms per unit cell : Mn in 4apositions
x, x, x with xMn = 0.138 and Si in 4apositions
with xs; =0.846 ;
each Mn atom is surroundedby
seven Si atoms and vice versa. There are alot of
compounds
with this structure :FeSi, CoGeSi,
AlNi2Si, NaBr03,
AIPt,
Al4GePd5
andeven
AI,Mn,,,Si2; they
may be used for the search of newquasicrystals.
To demonstrate the hidden icosahedral
symmetry
of MnSicrystal (both
in the real space and in the diffractionpatterns),
let us consider the idealized structure AB with xA =1)/4=t
and xB = 1 - xA = 0.845. This structure looks like aperiodic
system
ofinterpenetrating
dodecahedra(see Fig. 6) :
each A atom is at the center of an idealdodecahedron and seven vertices of the dodecahedron are
occupied by
B atoms(and
viceversa) ;
the closest A-B distance is/3/(2 )
and the closest A-A(or
B-B)
distance isT - 1.
If we do notdistinguish
A and B atoms(A = B ),
the space group becomesPa3
insteadofP2t3
forA =1= B)
asexpected
from the Landautheory [15].
The structure factorF(hkf)
for suchPa3
crystal
isgiven by
thefollowing equation
where
f = f (h 2+ k 2+ J2)
is the atomic factor. From thisequation
theapproximate
icosahedralsymmetry
of diffractionpatterns
can be seen(at
least,
inhigh-Q region).
Forexample,
the structure factors of the twofold andpseudo-twofold
reflections are almostequal
Fig.
6. -Idealized MnSi structure. Cube with the inscribed dodecahedron shows the unit-cell dimensions
(conventional
unit cell has anotherorigin [20]).
Full circles : A-atoms and empty circles :B-atoms. Atom 1 is at the center of the cube and atom l’ is at the cube
diagonal ;
the rest atoms are at the cube faces.whereas 1 F (Fi ,
1Fi Fi - 1 ) 1
8If 1.
. This is also valid for the threefold andpseudo-threefold
reflections : if i = 3 k then
and if i =A 3 k then
All these
approximate equalities
become more and more accurate withgrowing i
(to
provethis,
one should remember thatFi +
17-F,
and that thecycle
of theparity
of the Fibonacci numbers is three :odd, odd,
even,...).
It is
interesting
to note that there is a connection between MnSi structure and moresimple
1 / 1 >
approximant.
The latterapproximant
should haveIm3m
symmetry
if A = B[17]
orPm3m
symmetry
(like FeAl)
ifA =F
B. We can see atfigure
6 that there is a cluster ofeight
atoms which are
arranged
as inIm3m
cubic structure(A-atoms
marked with1, 5, 6,
7 and B-atoms marked withl’, 5’, 6’, 7’).
The threefold axis of the cluster is directedalong
thethreefold axis of
MnSi,
whereas the fourfold axes ofIm3m
structure are directedalong
pseudo-twofold
axes of MnSi structure. It seems that MnSi structure looks likemicrotwinning
ofFeAl-type
clusters ;
it would be veryinteresting
togeneralize
this connection betweenneighbouring approximants
for thehigh-order
case.Note also that the hidden icosahedral
symmetry
of MnSicrystal
results in somephysical
properties.
Forexample,
the elasticproperties
of MnSi are almostisotropic (the
ratio of theshear moduli is very close to unit : 2
c441 (CI I -
C12) = 1.05) ;
then,
the tensor form of thetensor structure
amplitudes [23]
of MnSi is close to that ofquasicrystals [24].
The direct
proof
shows that there is notendency
to theweakening
of those MnSi reflectionswhich
correspond
to the forbidden reflections ofnonsymmorphic
icosahedral space groups[25].
That’swhy
we should conclude that thenonsymmorphic
MnSicrystal
is theapproximant
6. Discussion.
Now we turn to the
high-order
Fibonaccicrystals
((13/8)
and(34/21 )
andbegin
with discussion ofexperimental
evidences insupport
of their existence. The direct evidences of thissort can be seen at diffraction
patterns.
Most of the x-ray diffractionpatterns
were obtainedfrom
powder
samples ;
in this case(see
Fig. 2),
one cantry
toidentify (13/8)
approximant
using
carefulanalysis
of theshape
of reflections. Theonly
availableexample
of suchanalysis
provides
reference[4],
where reflection withQ -
3.04Â -
was
fitted to two Gaussianpeaks.
It was shown that the widths of both
peaks
areequal
to the width of fivefoldpeak
(Q
2.894Â - 1) ;
their fittedpositions
are 3.031Â-
1 and 3.046A-
I(those
values aremarked
by
squares atFig. 7),
and the ratioof peak’s
intensities is about1/3.
Those values arevery close to the theoretical
predictions
for{16,0,0}
and{13,8,5}
reflections in(13/8)
approximant :
3.033Â -
and
3.045Â -
l respectively
(the
ratioof peak’s
intensities isexpected
to be about1/4) ;
icosahedralpeak
should bepositioned
at 3.043A-
1.
In thepioneering
paper[3]
thesplitting
of this reflection was alsoobserved,
but theintensity
ratio was estimated as1/1.
In any case, the properfitting
ofasymmetrically
broadened reflections(like
in Ref.[4])
maygive
decisivearguments
for the choice’ ofapproximant (or
anotherphason-strain model).
Fig.
7. - The deviations of cubic reflections from their icosahedralpositions
in different Fibonaccicrystals : (A)
for thetwofold { 2
Fi,
0,0 }
reflections and(B)
for thepseudo-twofold {Fi + h
F i, F i -
i}
reflections. Theoretical values are at the vertices of broken lines :(34/21) -
dash lines and13 /8 > -
solid lines.Experimental
data : circles[5] -
Mnimplantation
intosingle-crystal
Al ; squares[4]
-AlnMn22Si6;
rhombi - fromfigure
5 of reference[7] - A186Mn14’
Indices of reflections see atfigure
2. For(5/3)
approximant (a -Al-Mn-Si)
all deviations(not-shown)
are aboutT 4 times
greater than for(13/8)
approximant.
For
(34/21)
approximant,
thepowder
diffractionpattern
ispractically indistinguishable
fromquasicrystal
one(see
Fig. 2). Fortunately,
in reference[5]
the very accuratemeasure-ments of reflection
positions
were made for an orientatedsample
obtainedby
Mnimplantation
into Almonocrystal.
The measured deviations of reflections from theiricosahedral
positions (shown
by
circles atFig. 7)
are in well accordance with the theoreticalMore obvious
(but
may be lessaccurate)
evidences for the Fibonaccicrystals
can be foundat electron diffraction
patterns.
Although
some deviations from icosahedralsymmetry
wereobserved in many
works,
for the decisive conclusion about their natureconvergent
beam electron diffraction[7,
8]
ispreferable.
The size of the area should be less than(or,
atleast,
of the orderof)
the coherentlength
f coh
of thepositional
order ;
in AIMnSiquasicrystal alloys
thatlength
is about 300-500Â (it
can be estimated from the intrinsic width of x-raypeaks).
The shifts of reflections at the fivefoldpattern
from reference[7]
are close to thoseexpected
for the(13/8)
approximant (see
discussion in Ref.[15]);
as anexample,
the shifts of tworeflections are shown
by
rhombi atfigure
7. The deviations observed in electron diffractionpatterns
fromAl78Cr17Rus
alloy [19]
can be also attributedto (13/8)
approximant : figure
3Fig.
8. - Thesuperposition
of thepseudo-fivefold
patterns from different domains with coherentorientations ; (a), (b)
and(c) -
for the sameapproximant
with different orientations of twofold axes :(a)
- 360 and(b) -
72° between twofold axes in differentdomains ; (c) -
five different orientations, i.e. thepolydomain
diffraction area ;(d) -
for theF n + 1/ F n >
approximant
in one domain and theF n + 3/ F n + 2>
approximant
in another with the same direction of the twofold axes. Coordinate axes arelabelled for the
(Fn + 1/ F n >
approximant
with the twofold axisalong
x-direction. Note that the spots arefrom reference
[19]
is very close to the innermostpart
of ourfigure
3for (13/8)
approximant.
Thosepentagons
with theright angles,
marked atfigure
3,
can be seen atfigure
11.2 of reference[26].
On the otherhand,
theconvergent
beam electron diffractionpattern
of anAl74Mn2oSi6
alloy (Fig.
2 of Ref.[8])
seems to be close to thepattern
expected
for the(34 /21 )
approximant.
Notealso,
that the absence of some weakspots,
violating
thesymmetry
ofpatterns
[8],
may be causedby
theoff-plane
deviations ofreciprocal
latticevectors in cubic
approximants (those
deviations are stronger for weakspots).
As aresult,
some weak reflections can appear ordisappear
when the direction of incident electron beam isslightly changed.
The
qualitative
analysis
of electron diffractionpatterns
is rather difficultbecause,
even onthe best
patterns,
theshape
of diffractionspots
is distorted too : thespots
areelongated
in one or in different directions and the faintestspots
show thegreatest
distortion. Suchpicture
canbe
explained
if weadopt
different orientation of thesymmetry
axes of the Fibonaccicrystals
in different domains
(the
size of the domains is abouticoh)-
It isinteresting
that the small value ofecoh
inquasicrystalline alloys
can be alsoexplained
within this model.Indeed,
let ussuppose that there is the
phase
transition fromquasicrystal
to itsapproximant
(the
transition of this sort seems to be observed in Ref.[27]).
If the transition israpid enough,
then the domains with lower(cubic)
symmetry
can growindependently
and theirsymmetry
axes maybe orientated
along
different axes ofquasicrystal
matrix. Forexample,
some twofold axis ofquasicrystal
can transform either into twofold or intopseudo-twofold
axis of the Fibonaccicrystal ;
the same is true for any threefold axis. Such coherent orientation of axes andpseudo-axes is well known for Al-Mn
alloys.
There is no need of visiblesharp boundary
between different domains ofhigh-order approximants,
because their local structures are similar andthe differences between them are accumulated at the distance of the order of
fcoh-
In thismodel,
the natural estimation forecoh
isfcoh -
2’TT /
1 dQnm 1,
whereàQnm
is the difference between the basic vectors in cubic and in icosahedral lattices(see
Eq.
(7)) ;
at
that distance the mismatch betweenquasicrystal
matrix and its cubicapproximant
riches about oneinteratomic
spacing.
The
superposition
of diffractionpatterns
ofdifferently
orientated domains are shown atfigure
8a, b ;
the closepairs
of reflections look likeelongated
spots.
If the electron beam size is much more thanfcoh,
then allpossible
orientations of cubic axes withrespect
to those ofFig.
9. - Threefoldquasicrystal
arepresented
in the diffraction area and the calculated diffraction patterns for suchpolydomain
structure are shown atfigures
8c and 9. Note strange «triangular »
form of thespots
which isfrequently
observed in Al-Mn and Al-Li-Cualloys
[1,
19,
26] ;
the centersof the
spots
are almostexactly
atcorrespondent
icosahedralpositions.
Anothertype
of thepattern
(with
spots
elongated
in the samedirection)
may be a result of the same orientation ofaxes in domains of the Fibonacci
crystals
of different order(Fig.
8d).
7. Conclusion.
We have
presented
above thearguments
for existence ofhigh
order Fibonacciapproximants
in Al-Mn-Sialloys (for
otheralloys
and forlow-symmetry approximants
see Ref.[28]).
Thisproblem
hasgiven
rise to many controversies and in conclusion we shalltry
to relieve them. The mostpopular
argument
against crystal approximants
with a =30 Â
is that theseapproximants
cannotexplain
thelow-Q
reflections with thed-spacings
of8.85(7)
and5.42(3) Â
[29].
However,
thisargument
seems to beunacceptable
because in the Fibonacicrystals
the ratio of thesed-spacings
should be close to[(Ff+l +Ff+Ff-I)/(Ff+F’f-1 + Fl-2)]o.s
rather than toFi /Fi _
1(see
Fig. 2).
Thus,
within the
experimental
errors, thed-spacings
of8.85(7)
and5.42(3) Â
can be attributed topseudo-twofold almost-parallel
reflections (321 ) and {532}
inthe (13/8)
Fibonaccicrystal
with a =
33 À ;
therefore,
thisapproximant
cannot be ruled out.Moreover,
as it wasemphasized
above,
the averageposition
of thepartially splitted
cubic reflections is very closeto
corresponding
icosahedralposition
even forlow-Q
reflections(see Figs.
2,
8c and9).
Inany case, more careful
fitting
of reflections is desirable.Now we must
emphasize
that there is no contradiction between thephason-strain
description
of the distortions of diffractionpatterns
[19, 27]
and ourdescription.
Indeed,
theFibonacci
crystals correspond
to some fixed values ofphason
deformation[14, 16-18,
30] ;
those values are fixed
owing
to the commensurate character ofcrystal
structures.Speaking
in thephason-strain language,
we should sayaccurately
that the observed shifts of reflections can be causedby
thoseanisotropic phason
strains,
whichcorrespond (at
least,
approximately)
to (13/8)
Fibonaccicrystal (in
many cases[4, 7, 19])
orto ( 34 /21 )
Fibonaccicrystal (in
thebest case
[5]).
The next
controversy
is connected with thePauling
model[31]
(twinned
cubiccrystal
witha - 23.36
Â).
It should be noted that allreflections,
which were indexedby Pauling
atlow-Q
region
(where
the differences betweencrystal
andquasicrystal
reflections are morepronounced),
can beeasily
indexedin (13/8>
Fibonaccicrystal
because the ratio of latticeconstants
(33.1 /23.36)
is very close toJ2
(hence,
the ratios ofh2 +
k2
+ £2
are very close to2).
Moreover,
thosereflections,
which can not be indexed in thePauling
model[31 ],
may beindexed in
(13/8)
approximant;
forexample,
reflection inA174Mn2lSi5
withd-spacing
of8.98 Â
(or
8.85(7) Â
[29])
can be indexed as{321}.
Some theoretical
arguments
against crystal approximants
aregiven
in reference[32] ;
it isshown that the
gain owing
to lock-in terms in free energy is smaller than the lossarising
from thegradient
term(at
least,
forhigh-order approximants).
However,
within the model used inreference
[32],
the Fibonaccicrystals give
no loss ingradient
term, because thelengths
ofwave-vectors are
equal
for all basic harmonics(compare Eq. (3)
andEq.
(4)).
Moreover,
even more
complex
model is unstable withrespect
to variations in thelengths
of icosahedralwave vectors
[33]
and thephason
strains may be favorable.Indeed,
most of harmonics may beshifted toward lower
gradient
energy whensymmetry
is broken to cubic. The modelocking
can fix those
phason
strains on the valuescorresponding
to the Fibonaccicrystal
of someorder
(more
detail discussion see in Ref.[34]).
The fixedsign
of thephason
strains canintermediate
approximants
seem to be absent. It isunclear, however,
whetherAll2Mn
structure
(Im 3
space group, a = 7.47Á)
can beregarded
as n = 3 member of this series ofapproximants, becausein (3/2)
approximant
thereflections {320} or (230)
are expected to
bestrong
but those reflections are forbidden inIm3
structure.In the
end,
it should be noted that the Fibonaccicrystals
are notunique
and othertypes
of cubicapproximants
can exist. As a curious(but
notimpossible)
example
we can consider the(Ln + 1/ Ln)
Lucasapproximants,
where the Lucas numbersLi
are connected with theFibonacci numbers :
Li = Fi +
1 +Fi -
1(jL,
=1, 3, 4, 7, 11, ...,
i =1, 2, 3,
4, ...).
The dif-fractionpatterns
of the Lucasapproximants
are similar to thepatterns
of the Fibonacciapproximants (zigzag
shifts ofreflections,
asymmetric broadening, etc.),
whereas the values of all those effects aredifferent ;
the consideration of the Lucasapproximants
will begiven
elsewhere.Note added
during
revision : .’In the recent work
[35],
Prof. L.Pauling
also considers the Fibonacciapproximants
instead of his twinned model. Heinterprets
theexperimental
data of reference[5]
as (13/8)
approximant,
whereas it seems evident fromfigure
7that (34/21)
approximant gives
betterfitting
of the data. In reference[36],
the series of cubic and non-cubicapproximants
areconstructed
using
the canonical-celltiling (the Fn +
1 IF,
approximant
of Ref.[36]
corresponds
to
the (Fn + 4/ Fn + 3)
approximant
of thepresent
paper).
Note also reference[37],
where thecomputer
simulations of x-ray diffractionpatterns
have beenpresented
for the Fibonacci cubicapproximants
of different order.Many approximants
otherthan just
cubicapproximants
may occur both in Al-Mn-Si
[1, 28, 38]
and in otheralloys (see
Refs.[28,
39,
40]
for Al-Li-Cu and Ref.[41]
forAl-Cu-Fe).
Suchcrystal-quasicrystal polymorphism
seems to be a commonfeature of different
alloys
and further studies are needed toclarify
itsorigins.
Acknowledgments.
The author is
grateful
to Drs. V. M.Kaganer,
E. B.Loginov,
E. M.Terentjev
and S. B.Tochilin for the aid in
computer
calculations andgraphics.
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