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Generalizations of the gyroid surface
A. Fogden, M. Haeberlein, S. Lidin
To cite this version:
A. Fogden, M. Haeberlein, S. Lidin. Generalizations of the gyroid surface. Journal de Physique I,
EDP Sciences, 1993, 3 (12), pp.2371-2385. �10.1051/jp1:1993250�. �jpa-00246873�
Classification Physics Abstracts
02.40 68.00
Generalizations of the gyroid surface
A.
Fogden,
M. Haeberlein(*)
and S. LidinInorganic
Chemiswy 2, Chemical Cenwe, PO Box124, S-22100 Lund, Sweden(Received 19 March 1993,
accepted
infinal form
19 August 1993)Abstract. The deformation of Schoen's
gyroid
one of the three examples oftriply-periodic
minimal surfaces
possessing
cubic symmetry and genus 3 is discussed. Lower-symmetryvariants
(similarly
of genus 3) are shown to exist, and the one-variable family ofrhombohedrally-
distorted
gyroids
is constructed andparametrised exactly
via the Weierstrassrepresentation.
Introduction.
We
regard
structure as the manifestation of thecoupling
of our two basic concepts of force and geometry. Our scientificunderstanding
relies upon the construction of model systemsfacilitating
adecoupling
of the two concepts.By
means of thisdecomposition
we establishseparate
sets of rulesgoveming
each. These rules thenpermit
assessment of the level ofinterplay
between the two in aparticular
structure the first step towards solution of theproblem
as a whole. One may arguethat,
withincreasing sophistication
of computer simulationtechniques,
a detailedknowledge
of force laws alone maysuffice, circumventing
this first step. However geometry will remain the ultimate means of classification and
unification of
results, erecting
the framework of intuition necessary inexploring progressively
more
complicated problems.
To this end we consider here a novel set ofshapes representing plausible equilibrium
interfacial scenarios in avariety
ofmulticomponent
systems which aregenerating
great interest in the fields of science andengineering,
but lie outside the rangepresently
accessible to accurate simulation.We restrict attention to interfaces
possessing
«global uniformity
», in the sense that the entire surface iscompletely
dictatedby
any(arbitrarily)
smallpiece
of it. Forelliptic
andparabolic geometries
thesimplest representatives spheres
andcylinders, respectively
arespecified by
asingle
radius value alone, andaccordingly,
the local environment isabsolutely
identical
throughout.
Thesimplest representatives
of the less-familiar situation ofhyperbolic
geometry are minimal(I.e.
zero meancurvature)
surfaces.Any
minimal surface may be(*) Permanent address :
Department
ofInorganic
Chemistry, TheRoyal
Institute ofTechnology,
S-10044 Stockholm. Sweden.
expressed parametrically
in the form[1]
(x,
y,?)
w= Re
(i w'~, I(i
+w'~),
2w')R(w') dw', (1)
and is thus
specified solely by
itsparticular complex analytic
functionR(w ). Consequently
it may begenerated
from anyregion
viaanalytic
continuation of this so-called Weierstrassfunction. Note that
multiplication
of R(w by
the constante'~,
for real-valued o, defines a one- parameterfamily
of isometric minimalsurfaces,
referred to as the Bonnet associates of theoriginal (o
=
0)
surface[2].
One would
anticipate
thesesimplest examples (determined by
the least amount ofmathematical
input)
to be favoured asequilibrium dividing
surfaces in fluidpartitioning problems
since -theirconstruition
offers the easiest routes forself-assembly.
This is indeed thecase for mixtures of surfactant with water and/or oil
[3],
and for blockcopolymers (with
orwithout
homopolymers) [4],
in which the observed structures match theseshapes (or
straightforward
variants ofthem).
While the observation ofspheres
andcylinders (including planes
as their commonlimiting state)
conforms to our comfortablegeometrical prejudices,
theinterpretation
of the bicontinuousphases
presents a greaterchallenge.
In contrast to thespherical
andcylindrical
cases, theparametric representation (I
cannot, ingeneral,
guaranteethat continuation
givgs
rise to acomplete
surfacedividing
space into two distinctregions (I.e.
sealing
inside fromoutside).
Theglobal responsibilities
ofbicontinuity impose
aselectivity, admitting only particular
forms of the Weierstrass functionR(w).
The orderedpartitions generated by
these forms are referred to as intersection-free Infinite Periodic Minimal Surfaces(IPMS).
In thisstudy
weidentify
andparametrise
apreviously
unknownfamily
of such IPMS.The
origin
of thisfamily
is thesimplest (and
firstdiscovered) IPMS,
reviewedbriefly
in thefollowing
section.The
D,
P and G minimal surfaces.The D and P surfaces of Schwarz
[5]
mark thebirthplace
of IPMSparametrisation.
The basic element of the D surface is definedby
the two linearedges (AB
andBC)
and theplanar-curve edge (AC)
sketched infigure I, subject
to theboundary
conditions of twofold rotationalsymmetry across these two
straight
segments and mirror reflectional symmetry over the curved segment.Repeated application
of theseboundary operations yields
the 96 such elementscomprising
the fundamental unit of the Dsurface,
I-e- theprimitive
unit cell of the orientedc
Fig.
I. The D surface element ABC,lying
within thequadrirectanguiar
tetrahedral subdivision of the unit cube. The numeral I indicates that A is a first-order flat point of the surface.surface. The
topology
and symmetrycharacterizing
this fundamental unit arespecified by
the genus of 3 and the spacegroup-subgroup pair Pn3m-Fdlm, respectively [6].
In
equation (I)
w is thepoint
in thecomplex plane stereographically projected
from the Gauss mapimage
of(x,
y, z),
I-e- from thepoint
on the unitsphere given by
the direction ofthe vector normal to the surface there. We derive the Weierstrass function
R(w
of agiven
minimal surface
by interpreting particular
surface features viaequation (I)
as necessaryproperties
of therequisite
R(w ).
As acomplex analytic
function is dictatedby
itssingularity
structure, we address the
degeneracies
of the surface the« flat
»
points
at which the Gaussian curvature vanishes. Thedegree
of a flatpoint (x,
y, z is thewinding
number of the Gauss map about this site. Itsprojected
norrnal vectorw is then a branch
point
of theWeierstrass
function,
of orderequal
to thedegree
less one.The genus of an IPMS fundamental unit is
simply
related to the total of its flatpoint degrees [7].
Inparticular,
a genus of 3 the lower limit of IPMStopology corresponds
toexactly eight
flatpoints
ofdegree
two. An IPMS of genus 3 is thengenerated by
a Weierstrassfunction, possessing
first order branchpoints
at the set ofeight projected
normal vectorsw, ~ ~, of the form
8
R(W
)
=
e'~ fl
(W W,)~
~~~,
(2)
=1 w,*W
in which o is taken, without loss of
generality,
to be real(modulo ar),
and theproduct
is restricted to the finiteimages [7]. Any
such surface(e.g.
the D surface discussedabove)
thusamounts to a
particular
choice of(w,)~_
and o.The second characteristic of an IPMS fundamental
unit,
itscrystallographic
symmetry, isinterpreted
in the Gauss map as orientational symmetry,describing
the pattem of the distribution of flatpoint
normal vectors on the unitsphere,
orequivalently,
theirprojected
distribution in the
complex ~u-plane [7, 8].
The basis for classification of these pattems is the list ofregular geodesic triangulations
of thesphere [9].
Thus, for IPMS of genus3,
weanalyse
the
possible pattems
of a set ofeight points (representing (w,)~
~) with respect to theprojections
of thesetriangula# tilings
~The most
symmetric option
isprovided by
thespherical triangle
withedges given by
the three great circle arcsmeeting
at vertexangles ar/3,
ar/2 and WM. Onreflection,
48 of thesetriangles perfectly
tile thesphere,
as shown inprojection
infigure
2. The set ofeight
ar/3 vertices of the
tiling
aresymmetrically equivalent
under the group definedby
theseoperations. Choosing (w,)~
to coincide with theirpositions,
I-e-(0,
ct~,~,
'" 2
e' ~~~~, e~' ~
"'~, /, / e'"~~, / e~'"~~
,
the
resulting
Weierstrass functional/ /
form is
given
fromequation (2),
onexpansion, by
)
R(w )
=e'~ ~j
w
~ +
~
/
w
~ l ~~~
(3)
4
In this case the entire
pattem
is derivedby (projected)
reflection of thesingle triangle (the region
shaded inFig. 2).
On substitution ofequation (3),
the evaluation ofequation (I
within thisregion
of the~u-plane yields
the basic element of the surface. Reflection of thetriangle
thendefines the
analytic
continuation of the Weierstrass function to theadjoining region,
andaccordingly,
the extension of the surface element viaequation (I). Repeating
thisprocedure,
the 96triangles comprising
two identicalcopies
of thetiling
infigure
2spanning
thew
Fig.
2. The complex a-plane, decorated with thestereographically-projected tiling
of the unitsphere generated by
the (ar/3, ar/2, arm)geodesic triangle (corresponding
to the shaded region A'B'C'). The eight «/3 vertex sites(implicity including
the point at infinity), affixed with the numeral I, are the first-order branch
points
of the Weierswass function inequation
(3).complete
domain ofsingle-valued
definition of the dual-valued Weierstrass function inequation (3)
generate the 96 surface elementsforming
the fundamental unit.As mentioned
above,
thisapproach imposes
orientational order on the minimal surface, a necessary but insufficient condition to guarantee translational ordergiving
rise to an IPMS. To ascertain this property one must furtheranalyse
the real space manifestation of thesymmetries
of theimage
spacetiling [7, 8J.
For the value o = 0 the
triangle edge
reflectioncontinuing
the Weierstrass function inequation (3)
effects a purecrystallographic
extension of the surface element. Fromequation (I)
thebounding
segments AB and BC of theelement,
withimages corresponding
to thetriangle edges
A'B' and B'C' infigure 2,
must bestraight
linesdefining
axes of twofoldrotation,
while the third segment AC(imaged
toA'C')
must lie in aplane defining
mirror reflection.Hence,
on
comparison
withfigure I,
the case o= 0 is
precisely
the Weierstrass function of the D surface(given
in a formdifferent,
butequivalent,
to the usualequation [5]
due to our choice ofcoordinate orientation
implicit
inFig. 2).
The property of pure
crystallographic
extension is sharedby
the o= ar/2 surface, termed the
«
adjoint
» to the o= 0 surface. However now the roles are reversed, with the
triangle edges
A'B' and B'C'giving
rise to mirrorplane
curves AB andBC,
and A'C' a twofold rotational lineAC, bounding
the surface element. This element, inscribed in thequadrirectangular
tetrahedron infigure 3,
isprecisely
that of the P surface. The familiar(genus 3)
fundamentalunit,
constructed from the 96 suchelements,
possesses the symmetryIm3m-Pm3m [6].
I
c
Fig.
3. The P surface element, labelled analogously tofigure
1. In both cases theprojected
Gauss mapimage
of the element is the shaded triangle infigure
2 (with theprime symbols denoting
thecorresponding
verteximages).
The
crystallographic
nature of theboundary
conditions renders visualization of the D and Psurfaces
straightforward.
Forexample,
one may view the surfacepatch
boundedby
theshortest
straight
line circuit(obtained by
mirrorreflection(s)
of the elements inFigs.
I and3) by dipping
a wire frame into soap solution.Similarly
itpermits
immediate classification of thesymmetries
of these twosurfaces,
and verification that both are free from self-intersections.Now consider the intermediate range 0
< o
< ar/2 of the Bonnet associate
family generated by equation (3) (note
that the surface for o issymmetrically equivalent
to its countenlart for oby
virtue of the invariance offigure
2 under theoperation
w ~ i3, I.e. reflection in the real axis Im w=
0).
This range is more difficult to assess since theanalytic
continuation of the Weierstrass function effectedby
thetriangle
reflection does not possess asimple geometric interpretation
in real space. The surface element is nolonger
boundedby straight
lines and/orplanar
curves, and its extension viaequation (I)
now represents acomplicated hybrid
oftwofold rotation and mirror reflection. The
only point
groupsymmetries
retained from theoriginal
surface are theperpendicular
rotationalsymmetries (I.e.
the invariances on rotationabout a surface
normal,
with or without inversionthrough
the surfacepoint) [7, 8].
Translational order can
only
result if thespatial
distribution of thesepoint
groupsymmetries
isglobally
consistent with a three-dimensional space group. It is found thatimposition
of asingle
constraint is necessary and sufficient to force this lock-in of sites,reducing
theproblem
to the solution of oneequation
in the onedegree
of freedom o. Schoen discovered that there existsone
(and only one)
value : o= 0.66348
(=
38.015°) giving
rise to an ordered surface withoutself-intersections,
christened thegyroid [10].
Thegyroid (or G,
orY*, surface)
has genus 3 and symmetryIa3d-14132 [6].
The
D,
P and G surfacestogether
serve as aspectacular
illustration of theutility
of the Weierstrassrepresentation (I).
The existence of the D and P surfaces is apparent from the initial statement of theboundary
valueproblems defining
their surface elements. The solutions of theseproblems,
thensupplying
thequantitative
surface details, may be derivedby
ad hocmethods
based onassumptions
ofparticular
functional formsgoveming
theirimplicit equations [I Ii.
However thegenerality
of theparametric equation (I) provides
an economicalunification of their
descriptions
via thesimple
transformationrelating
the two surfaces.Importantly
this transformation alsoyields
the Gsurface,
inaccessibleby
any other meansowing
to theinseparability
of its existenceproblem
and its solution.The
family
of three Bonnet-related surfaces constitute theonly
intersection-free IPMS of genus 3 and cubic symmetry. As such,they
are thesimplest
bicontinuouspartitions.
One of theearliest
examples
in theirrapidly expanding
range ofapplications
involvedmodelling
theshapes underlying
« cubicphases
» oflyotropic liquid crystalline
assemblies[12J.
Closerinspection
revealed that thiscompositional region
of thephase diagram
is often sheathedby
so-called « intermediate
phase
»regions.
The available information suggests that these inter- mediates are likewise describedby hyperbolic
geometry, but of lower(typically
rhombohedralor
tetragonal)
symmetry. In certain cases[13J
the measured unit cellparameters, varying smoothly through
the intermediateregion,
pass(nearly) continuously
across thephase boundary
to the cubicregion, implying
that the cubic structure ismerely
the maximalsymmetry
endpoint
of the intermediate structuralfamily.
To
geometrically
model these transitions we considerlower-symmetry
IPMS familiesderived from cubic IPMS. In
keeping
with our limitation to thesimplest
such surfaces(D,
P andG),
we restrict theanalysis
to thesimplest
of theirgeneralizations,
for which thetopology
is
preserved throughout.
With the genusretaining
its value of3,
thepreliminary
resultsopening
this section stillapply specifically,
the Weierstrass function retains the formgiven
in
equation (2).
The task is thus reduced tostudying
the effect of symmetry reduction on(w,)~_
and o. Thefollowing
section addresses oneparticular
mode ofdegradation.
Rhombohedral
generalizations.
The abovementioned nature of the
bounding segments
of the D and P surface elementsfacilitates direct derivation of their
lower-symmetry
variantsby crystallographic
deformation of asuitably
chosen unit withboundary
definedby symmetry operations
common to both theoriginal
anddegraded
space groups. For rhombohedral deformations the unit is taken in bothcases to be the
ring-like piece (comprising
48 cubic surfaceelements) spanned by
apair
ofequilateral triangles
relatedby
ar/3 screw rotationalong
their common axis[10, 14J.
The one-variable
family
is thengenerated by stretching along
this axis. Since the D and P surfaces are bothspecial
cases of thisstretch,
their rhombohedralgeneralizations
are coincident(up
toreorientation)
and are denoted the rPDfamily.
The surface element ABDC of atypical family
member, delimitedby
theadjacent
mirrorplanes slicing
one-sixth of thering,like piece,
isdisplayed
infigure
4. Note that the element possesses an intemal twofold rotational symmetrypenlendicular
to the surface(and
to the stretchaxis).
The rPD fundamental unit,constituting
two
ring-like pieces,
has symmetryR3m-R3m(2c) [6J.
i ' ' ' , ' t
A
Fig,
4. An rPD surface element ABDC. Each of its four vertices is a first-order flat point (with thepairs
A and D,together
with B and C,interchanged
via the intemal twofoldsymmetry).
In the
projected
Gauss map the rhombohedral deformation of the D and P surfacescorresponds
tosystematic degradation
of the group of reflectionsymmetries given by
the tileedges
infigure
2[8J.
The six circles are removed,leaving
the threestraight
line reflection axes(Im (w
~) =0
), together
with the symmetryoperations produced by composition
of reflectionsacross the
pairs
of these circlesintersecting penlendicularly
at the six sitesw~
= I. The
reduced subdivision underlies
figure 5,
with the open circlesmarking
these six sites. The(genetic)
set of two vertices and sixedge points
is(0,
ct~, t, te'~"~~, te~~~"~~,
,
e~"~~, e~ ' "~~
,
where t
~ 0.
Taking
this one-variable pattem as w ,(represented
t t t
by
the filledpircles
affixed with the numeral I inFig. 5),
substitution intoequation (2),
followedby expansion, gives
-1/2
R(w )
=
e'~
w w ~+
t~
w
~ l
(4)
t~
The pattem is
generated by
reflection alone from the shadedregion
A'B'D'C' infigure 5,
theregion
ofintegration
inequation (I) giving
rise to the surface element.D'
o
o
Re6J
o o
o
Fig.
5.Degradation
offigure
2, preserving only the straight-line reflection axes atangles
«/3 and the twofold rotational symmetries at theopen-circle
sites. The shadedregion
now defines the smallestreflectional unit of the reduced
tiling.
Theeight points
labelled I are the symmetry images of the originA' and the variable edge
point
B' (w =t), e.g. thepoint
at infinity D' and the edge pointC' (w = I/t
e'"'~)
are their respective images under the twofold
operation
at w =e'"'~ These eight sites constitute the first-order branch
points
inequation
(4).For o
= 0
(respectively
o=
ar/2)
the segments A'B' and D'C'(respectively
A'C' andD'B')
become twofold rotational lines on the elementboundary,
closedby
the mirrorplane
curves from the segments A'C' and D'B'
(respectively
A'B' andD'C'). By comparison
withthe discussion in the
preceding section,
thispair
of one-parameter families definesexactly
the rhombohedral deformations of the D and Psurfaces, respectively, restoring
the cubic IPMS as thespecial
case t = Further, combination ofequations (I)
and(4)
verifies that the two are/
the same,
mapping
onto each otherby
the reorientational transformation w~
(and
w
t ~
).
Hence the rPDfamily
is definedcontinuously
anduniquely
viaequation (4) by
thet
juxtaposition
of 9= 0 for 0 < t « I and o
= ar/2 for I m t
~
0,
orequivalently by
o =
0
only (say)
for all t~ 0
(the
latter nowgiving
the D and P surfaces at t= and
/
t =
/, respectively).
In
precise analogy
with the cubic case, the in-surface twofold lines and the mirrorplanes
of these two Bonnetendpoints
are non-existent in thebridging
range 0< em ar/2
(with
the surface for oagain equivalent
to that for o since reflection symmetry in Im w = 0 ispreserved
inFig. 5), necessitating
a more detailed consideration ofglobal
surfaceproperties.
It is now found that therequirement
of translational orderimposes
apair
of extemalconstraints,
I-e- a system of twocoupled equations
in the two free variables t and o. However the solesolution in the range 0~t «1, 0~ o
~ ar/2 which further satisfies the intersection-free criterion is t
= ,
o =
0.66348, recovering
the cubic G surface of Schoen./
Thus the
generalization
of the cubic surfaces D and P to the rPDfamily
does not support acorresponding generalization
of their associate surface G.(This
corrects an earlier assertionby
one of the authors
[14J.)
Thegyroid
cannot be reduced in symmetryrhombohedrally by
composition
of this deformation of the parent D(or P)
surface with Bonnettransformation, replicating
Schoen's conclusionregarding
orthorhombic deformations[10J.
Hence thisparticular
route cannot lead to any additional freedom.Schoen extends his conclusion with the
proposition
that « there does not exist anybody-
centred orthorhombic version of
G,
however it is obtained », as evidence for his belief in the likelihood that « G may not have any variant forms of lower symmetry »ii 0]. Accordingly
it iswidely
assumed in the literature that thegyroid
isrigid
within the class of intersection-free IPMS. Assessment of thevalidity
of thisassumption
iscomplicated by
the earlier-mentionedinseparability
of existence and solution for IPMS devoid of both in-surface twofold rotation and mirror reflectionoperations.
In the remainder of thisstudy
we resolve this openquestion
via
explicit
construction of thefamily
of rhombohedral variants.The above observations
regarding
the Weierstrass functional form(4)
indicate that thepresent
rhombohedral deformation is aninsufficiently general
basis for the associatefamily.
It is necessary to consider furthergeneralization, corresponding
todegradation
of the group of symmetryoperations
infigure
5,admitting
asymmetry
reduction within itsgeneric
set ofeight points.
The obvious step is removal of the threestraight
line reflection axes,retaining
however the threefold symmetry inducedby composition
at their two intersection sites(the origin
and thepoint
atinfinity).
This reducedpattem, underlying figure 6,
fumishes the(generic)
set of~jgh~p~j~~~ jo
~ ~ ~~12w/3
~
~-,2w/3
~l1~,w/3 ~_;w/3)
~h~~~ ~ ~~ ~~~~
, , 0, 0 , 0 , ,
~ ,
, 0
W0 0 W0
complex
number.Identifying
this two-variable set as w,)
~(represented by
the distribution of filled circlesbearing
the numeral I inFig. 6), equation (2)
nowyields
(w)=e'~lw
w~+ wo ~~-w/ w~-1
~~~(5)
Without loss of
generality
we may restrict wo=
te'4
to lie in theregion
definedby
t = wo ~ 0 ar/6
<
4
= arg w~ w
I
Foran
arbitrary
such value, the smallest symmetry' 6
unit
(taken
forexample
as thisregion
arg w wI shaded in
Fig. 6)
is nolonger
delimited' ' 6
' '
' '
, J
, J
, '
, /
' / o'
' ° /
'' ,
t ' /
o ' /
' /
' ,
* '
/ ,
/ ',
~ /
/ ,,
/ . ,
/ l '
, ~ '
/ §
, '
/
i ',
/ '
/ '
Fig.
6.Degradation
of figure 5,replacing
the reflection axesby
threefold symmetry sites (trianglesymbol)
at theorigin
and at infinity. The shaded region represents a basic unit of the scheme, and contains thepoint
wo = i e". The rotationaloperations give
rise to the set of six relatedpoints
which, together with the threefold sites, define theeight
branchpoints
(marked I) of the Weierstrass function inequation
(5).by edges
of reflection it now generates the entirepattem
via the twofold(open
circlesymbol)-
and threefold(triangle symbol)- composite operations
alone.Consequently
the basic surface element, obtainedby integration
ofequation (5)
in therepresentation (I)
over thisregion,
cannot be extendedby
a «boundary segment-fixing
»crystallographic
mechanism forany o value. Instead the element is swivelled around its
boundary by
theperpendicular
rotational
symmetries
2 and 3 effectedby
thesecomposite operations,
for all o.Note that the Weierstrass function in
equation (5)
embraces allpreviously
knownexamples
of genus3,
intersection-free IPMS with(at least) trigonal
symmetry.Clearly
itdegenerates
into the two-variable form(4)
for thespecial
case4
= 0. At the other extreme, the limit 4 = ar/6gives
the two-variablefamily
-1/2
R(w )
=
e'~
ww~
Ij + t~
w
~ l
,
(6)
t
which likewise restores reflection axes in
figure 6,
nowdelimiting
theregion [arg
w w "6 ,
w w I as the smallest symmetry unit. For this orientation the values o
= ±
I correspond
to 4the
pair
of cases for which these reflection axes are realised as twofold rotational lines andmirror
plane
curvesbounding
the surface element.Specifically,
o=
fi
defines the4 one-
variable
family
of H surfaces discoveredby
Schwarz[5J,
while the o=
"
(adjoint H)
surfaces 4are
(crystallographically) self-intersecting.
Thebridging
range "< o
<
"
(with
the surface4 4
for o now
symmetrically equivalent
to that for ar/2- oby
virtue of the symmetryW ~
e'"'~
&, i-e- the reflection axis Im(e~'"'w
=
o)
wasinvestigated
in aprevious study by
one of the authors
[15J.
The two conditions in t and o necessary for translational order werefound to
yield
an intersection-free IPMS for the solutions t=o.5361 and o= o.3353
(= 19.21°).
ThisIPMS,
denoted here the HG surface, possesses fundamental unit of symmetryR3c-R32 [16J. Significantly,
it represents asimple counterexample
to Schoen'sclaim, regarding
his Gsurface,
that « it is consideredhighly unlikely
that any other intersection-freeIPMS
containing
neitherstraight
lines norplane
lines of curvature will be found »[10J.
While the G and HG surfaces are
unique
within the Bonnet associates of the one-variable rPD and H surfacefamilies, respectively, equation (5) supplies
the extradegree
offreedom,
4,necessary to relax their
rigidity.
Theoriginal
states((t,4)= ~,0
/
and(t,
4)
m
(0.5361,
"), respectively)
may now beperturbed two-dimensionally throughout
6
their
generic neighbourhood
in thecomplex wo-plane.
This will open up a one-dimensional continuum of solutions(corresponding
to intersection-freeIPMS) emanating
from the twosources. Further, the
unifying
nature ofequation (5)
dictates that these two solution curves maybe
smoothly
continued into each other. Thissingle
curve will then be therequired
one-variablegeneralization connecting
thepreviously
isolated G and HG surfaces.By establishing
thelink,
this newfamily,
denotedrG,
thusprovides
thesimplest path
ofcontinuous,
zero meancun~ature-preserving
access between the rPD and H families. The stretched rPDfamily
is relaxed to restore the cubicspecial
case(either
D orP),
which is first bent(via
the Bonnettransform)
intoG,
distorted into HG, and then bent back to the H surface toregain
itsgeneric degree
ofstretching
freedom.The
quantitative
features of thenumerically generated
rGfamily
arepresented
in thefollowing
section.Results.
The one-variable rG
family
is definedby
the twoequations
in the set of threevariables,
4, t, oimposing
translational order. Thefamily
isconveniently
indexedby
4 suchthat,
for aparticular
member I-e- 4value,
the system is solved for thecorresponding
t and o valuesfixing
the branch
point position
and the Bonnetangle.
Thepair
ofequations,
obtained via substitution ofequation (5)
into therepresentation (I),
enforce the lock-in ofparallel
threefold axis sites.As
they
are identical to the constraintsapplied previously
to the HG surface[15J,
the solutionprocedure
is not detailed here. It iscomputationally
well-behaved since thecoupling
between the two variables t and o isonly slight.
Note that the absence of
edges
of reflection symmetry infigure
6(in particular,
the axis Im w =0 for the rPDfamily
and Im(e~'"~~w)
=0 for the Hfamily)
removes anysymmetrical degeneracies
within the full range of o(modulo
ar).Thus,
in the interval OS 4 w ar/6 there exist distinctpairs
of solution familiesdiverging
in 4 m 0 from the twosymmetrically equivalent
4=
0 values
(o
m 0.66348 and o
m
0.66348)
for the G surface andsimilarly
in 4 w ar/6 from the4
= ar/6 altematives(o
m 0.3353 and o
m
I 0.3353)
for 2the HG surface. It is found that the families
corresponding
to the first-mentioned ooption
in these two cases mergecontinuously
into theconnecting
solution. The solution thusderived,
I.e. thepolar
coordinate curve t=
t(4
and the association parameter curve o=
o (4
)
for OS4
war/6,
isplotted
infigure
7.The
simple
nature of the trends in these variables is likewise manifested in the appearance of the rG surfacefamily
itself. Infigure
8 the scan of the rangedisplays
surfacepieces
of this solutionfamily
for three different 4 values. In each case thepieces
aregenerated
from identicalregions
of thecomplex w~plane
and are viewed down the common threefold axis direction. The intermediate member ~b = ar/9 infigure
8b confirms the monotonic transitionreducing
the tunnels in this direction from theirlargest
width in the G surface case 4 = 0(Fig.
8a) to theirsmallest at the HG case
4
= gr/6
(Fig. 8c).
zf4
#
(tad.)
0.33530
II
Q5
0.5361 -~
0 '
«/6
4
(rad.)
Fig.
7. The solutiondefining
the entirefamily
of rG surfaces in terms of thesingle
parameter ~b. Thecorresponding
radial ordinate i (left axis) and Bonnetangle (fight
axis) areplotted
for each ~b. Thespecial
values ~b
=
0 and ~b
=
«/6 represent the known cases of the G and HG surfaces,
respectively.
Further,
recall that there also exist solution familiesemanating
from the twospecial
cases~b =
0 and 4 = ar/6
corresponding
to their second-mentioned ooptions
above. These twoextra
families,
on reflection in theirbounding
axes(I.e.
in Imw =0 so w~ & and
4
~4, taking
o to o, and in Im(e~'"/~
w
)
= 0 so w
~
e'"~~
& and4
~ ar/3
4, taking
o to
ar/2-o, respectively)
are smooth continuations of theconnecting
solution inOS
4
w "(given by
the first-mentionedvalues)
to the ranges 4 w0 and 4 mar/6,
6
respectively.
The associated solution curves t=
t(4)
and o=
o(4)
in thesesupporting
ranges are likewise
graphed
infigure
7. The existence of these extensions is apparent fromextrapolation
of the trend illustrated infigure
8. The4
Sofamily,
for which the threefoldtunnels continue to increase in size
beyond
the G surface value(Fig. 8a),
terminatesasymptotically
with the case4
= ar/6, o= arm
(symmetrically equivalent
to4
=
ar/6,
o =
arm), corresponding
to the Hsurface,
in the limit t=
I of
infinitely-wide
tunnels(so
theperiodic
surface becomes asingle
saddletower). Similarly
the ~mar/6family,
representing
a decrease in tunnel width below that of the HG surface(Fig. 8c),
endsby approaching
~= ar/3, o
=
0
(symmetrically equivalent
to~
= 0, o
=
ar/2),
I.e. the rPDsurface,
in itsvanishing
limit t=
0.
Taken
together,
the continuous solutionspanning
the full rangeI
w ~ w " in
figure
76 3
defines the entire rG surface
family.
The symmetry of the(fundamental
unit ofthe) generic
rG surface,classifying
thedegradation
of the cubic Gsurface,
isprecisely
that of the HG casequoted above, namely
spacegroup-subgroup R3c-R32.
Thedependence
of the ratio cla of the rhombohedral celldimenions, together
with the surface-to-volume ratioS~/V~,
on theparameter
~
may bereadily
extracted from the information infigure
7.a)
b)
Fig.
8.Computer-generated
views of the samepiece
of the rG surface at (a) 4 0 (the G surface), (b) ~b= «/9 and (c) ~b = «/6 (the HG surface).
i
C)
Extensions and conclusions.
Although
thepreceding
sections focussed on rhombohedral variants of Schoen'sgyroid,
theunderlying principles
are not limited to thisspecific
distortion. Moregenerally
there exists lower symmetry derivatives of the surfacecorresponding
tosystematic degradation
of thetiling
pattemprojected
infigure
2 which preserve (at most) rotationalsymmetries only
and admit of ageneric order-eight
set.Performing
a coordinatereorientation,
theoriginal tiling
isequally
wellrepresented
inprojection
infigure
9. With the ar/3 vertices nowresiding
at theeight positions
~
*/
,i
~
*
), ~
*),
i'~
~),
substitution intoequation (2) yields
/ / /
R
(w
=
e'~ (w
~ 14 w ~ + l)~ '~~(7)
While this more familiar form
[5]
isprecisely equivalent
to that inequation (3)
onapplication
of the same coordinate transformation to the
representation (I),
it now facilitates atetragonal
mode of distortion.
Retaining
fourfold symmetry at theorigin
and thepoint
atinfinity
I.e.w = 0, ct~ and twofold symmetry at the
eight
sitesw
~
=
l on the unit
circle,
thegeneralised
group
(wo, iwo,
wo,iwo,
, ,
~,
thengives
Ma ma ~°o ma
R(w)=e'~ w~- ~~+w( w~+ll~~~ (8)
ma
Im4J
Rew
Fig.
9. Theprojected tiling
of thecomplex plane
infigure
2, after a rotationmapping
the arm vertex of the basicdangle
(shaded) to theorigin
and the «/4-«/3edge
along the real axis. The newpositions
of theeight
«/3 vertices are now the first-order branch points of the function in equation (7).Here the
complex
number w~ =te'4
may be assumed to lie within theregion
t~0, OS~< ".
Thespecial
case
~
=0,reinstating
the reflection axes Im(w~)=0
and 4w = I, defines the Bonnet associates of the one-variable
family,
denoted tD, oftetragonally
distorted D surfaces
[8].
As with the rhombohedral rPD case, thepair
ofequations
in t, o retum the cubicgyroid
t =~
,
o
m 0.66348 as the
only
intersection-free IPMS within the/
range 0
< o < ar/2
bridging
the tD and tP surfaces. However the presence of the additional parameter ~b inequation (8)
liberates a one-variablefamily
of non-trivial solutions tkom thissource
point.
These constitute thetetragonal
variants tG of thegyroid.
The results of this
study, revealing
the robust nature of thegyroid, hopefully
serve todemystify
this surface.They
illustrate thatlower-symmetry
variants of thegyroid
follow fromdegradation
of thespherical tiling pattem
in a mannerprecisely analogous
to thatpreviously
established for its « conventional »
associates,
the D and P surfaces[8J.
This observation
applies
to allIPMS, independent
of the intersection-free condition. If the o A 0(and
hence o=
ar/2)
IPMS possesses an intermediate(0
< o< ar/2
)
Bonnet associate which is likewisetranslationally ord£ed (but lacking in-surface,
twofold rotation and mirror reflectionsymmetries)
then both exhibit the same range oforder-preserving,
deformation freedom. The D surfaceonly
appearsspecial
in the sense that this intermediate member is also free from self-intersections. It is of interest to determine whether any of the(higher genus)
cubic IPMS share this property. Aprevious investigation
retumed anegative
answerregarding
the I-WP surface of genus 4
[17].
We havesubsequently analysed
thesimplest
two membersjl 8, 19] remaining
in the known set[6, 10]
of cubic IPMS the F-RD and C(P )
surfaces(of
genus 6 and
9, respectively). Again
no intersection-free associates were revealed. It istempting
togeneralise
thistrend,
since it appearsunlikely
that atopologically-complicated
IPMS may be bent to the
required
extent withoutbeing
forced to passthrough
itself.Acknowledgement.
One of the authors
(A. F.)
wassupported by
the Swedish Natural Research Council(NFR).
References
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[3] Fontell K., Colloid
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[51 Schwarz H. A., Gesammelte Mathematische
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Erd61yi
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F., Tricomi F. G.,Higher
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