HAL Id: jpa-00246477
https://hal.archives-ouvertes.fr/jpa-00246477
Submitted on 1 Jan 1992
HAL is a multi-disciplinary open access archive for the deposit and dissemination of sci- entific research documents, whether they are pub- lished or not. The documents may come from teaching and research institutions in France or abroad, or from public or private research centers.
L’archive ouverte pluridisciplinaire HAL, est destinée au dépôt et à la diffusion de documents scientifiques de niveau recherche, publiés ou non, émanant des établissements d’enseignement et de recherche français ou étrangers, des laboratoires publics ou privés.
A systematic method for parametrising periodic minimal surfaces : the F-RD surface
A. Fogden
To cite this version:
A. Fogden. A systematic method for parametrising periodic minimal surfaces : the F-RD surface.
Journal de Physique I, EDP Sciences, 1992, 2 (3), pp.233-239. �10.1051/jp1:1992138�. �jpa-00246477�
Classification Physics Abstracts
02.40 68.00
A systematic method for parametrising periodic minimal surfaces
:the F.RD surface
A.
Fogden
Department
ofApplied
Mathematics, Research School ofPhysical
Sciences andEngineering,
Australian National University, PO Box 4, Canberra 2601, Australia
(Received 23
July
1991, accepted infinal form
2 December 1991)Abstract. An
algorithm
for the exact construction oftriply periodic
minimal surfacesrecently developed by
the author is illustratedsimply
with the firstparametrisation
of the F-RD surfacediscovered
by
Alan Schoen. An exact expression for the F-RD Weierstrass function is derived, from which allquantitative
features of this surface may bereadily
established.Introduction.
While geometry has been a
key participant
in all stages of thedevelopment
of thephysical sciences, explanation
of theincreasing diversity
of bicontinuous microstructures observed in condensed matterIii provides
achallenge
to conventionalgeometric
intuition.Recently,
infiniteperiodic
minimal surfaces(IPMS)
have beenadopted
as the basis of avocabulary
for thisevolving language
of structure. It is an openquestion
as to whether thisspecific
class ofperiodic
surfaces possess any realsignificance
in the context of thephysical systems,
however theirutility
as a means of classification is undeniable. The cubic TAMS of genus three theD,
P and G surfaces are mostfrequently invoked,
inmodelling
the structuresunderlying
avariety
of molecular self-assemblies[2].
It has beenpostulated
that theseparticular
IPMS are favoured on the basis of surfacehomogeneity [3],
thatis, they
represent the most uniform interracial scenario attainableglobally.
Bicontinuousphases
related tohigher
genus TAMSmay also occur, with the
region
of their existence in thephase diagram increasing
withdecreasing sample purity.
Thisexpectation
has been bome outby
recentexperiments [4].
With the advent of
sophisticated
measurementtechniques,
theprincipal
limitation to thepossible
observation andrecognition
oftopologically complex
structures remains theincomplete knowledge regarding accompanying
IPMSdescriptions.
Thisproblem
has beenpartially
redressedby
thediscovery
of a multitude of new IPMSby
Schoen[5] and, lately, by
Koch and Fischer
[6].
These TAMS were isolatedempirically,
without theprecise
mathematicalspecification
of the surface necessary forquantitative comparison
with observed systems.Many
of the Schoenexamples
have now beenparametrised by
Karcher[7].
A
systematic procedure
for theparametrisation
of ageneral
IPMS hasrecently
beendeveloped by
the author[8].
There the method was verified with agreatly simplified
rederivation of Neovius'
description
of theC(P) surface,
then utilised inderiving
the first234 JOURNAL DE
PHYSIQUE
I N° 3parametrisations
of thehexagonal
HS2 and orthorhombic PT surfaces of Koch and Fischer,together
with those of the new orthorhombic IPMS and newpentagonal
surface(denoted
VAL and
pCLP, respectively) arising
from earlier work withHyde [9, 10].
While thegeneral
formulation of the
procedure
ismathematically involved,
the fundamentals aresimple
and itsapplication
should be accessible toexperimentalists seeking
classification of observed structures. With a view to this aim we illustrate the method here with the firstparametrisation
of the F-RD surface of Schoen. The choice of this
example
isphysically
motivated the F- RD surface is a cubic IPMS ofrelatively simple topology (in fact,
the lowest genus cubic IPMS of Schoenremaining undescribed)
and thus may beexpected
to occur in bicontinuous media.The F-RD surface.
The
topology
andsymmetry
of the F-RD surface isspecified
in Schoen's report[5]
webriefly
summarise the information relevant to the
parametrisation
here. The fundamental trans- lational unit of theIPMS, displayed
infigure I,
has a genus of six and the space group symmetry Fm3m(or
F ~3
~). Accordingly
the IPMS contains mirrorplanes
in them m
absence of any on-surface two-fold rotational axes
(as
is the case for the I-WP surface II])
sothe two
labyrinths partitioned by
the interface aregeometrically
distinct(and
are characterisedby
the types F andRD).
The translational unit is constructed from a basic surface element or Flhchenstfick(identified
inFig.
I)
delimitedby
four mirrorplanes
of the surface.Propagation
of this basic element
by repeated
reflection in thebounding
mirrorplanes,
until the full set ofsymmetries
areexhausted, generates
the translationalunit,
thuscomprising
48 such elements.The intersection of a mirror
plane
with the surface is referred to as aplane
line of curvature.Two
pairs
of such curvesdefining
the basic element intersectperpendicularly.
Theremaining
two
pairs
intersect atangles
ofw/3
andMN
atpoints
of 3-fold and 4-foldperpendicular
rotational symmetry of the
surface, respectively.
These aredegenerate points
of thesurface,
called flatpoints,
at which the Gaussian curvature is zero. Thedegree
of these flatpoints
the number of revolutions about the surface normal vector at this
point
traced outby
the normal vectoralong
any circuit on the surfaceenclosing
thepoint
is 2 and3, respectively.
Fig.
I. The fundamental unit of the F-RD surfacecomprising
48 of the surface elements shown.Parametrisation of the F-RD surface.
Mapping
a minimal surface into theplane,
such that a surfacepoint (x,
y,z)
is Gaussmapped
to the
point
of intersection of its surface normal vector with the unitsphere
centred there, and in tumstereographically projected
to acomplex
number w, the inverse function was shownby
Weierstrass
[12]
to have thegeneral
form(x,
y, z =Re
l~ (I w'~, I(I
+w'~),
2w')
R(w')
dw'(1)
for some
complex
function R(w ).
Theimage
of the basic element of the F-RD surface in thecomplex plane
under thiscomposite
map is the shadedpolygon
infigure
2. For an IPMS thecorresponding
Weierstrass function R(w )
ismultivalued,
and morespecifically,
eachgeneric
surface normal vector
image
w is shared
by
the same(finite)
number ofpoints
(x,
y,z)
on the translational unit. Hence the Gauss map of this unitgives
themultiple covering
of the unitsphere (and
thecomplex plane
onprojection) comprising
this number of sheets. This number is atopological
constant, and isequal
to the genus less one for anorientable TAMS
[9].
For the genus six F-RD surface the translational unit Gauss mapimage
must then
comprise
five sheets. This isapparent
fromfigure
2just
as successive reflections of the basic surface element in itsbounding planes yields
the set of 48 such elementsforming
the translational
unit,
in the Gauss mapimage repeated
reflection of thespherical geodesic polygon
in itsedges
generates a set of 48 suchpolygons tessellating
a five-sheetedspherical covering.
Fig.
2.Projected
Gauss mapimage
of the F-RD surface element.For the
special
surface normal vectorimages
w of flatpoints,
the number ofpoints
on the unitpossessing
this normal isonly equal
to thegeneric
value if each is counted with themultiplicity
of its flatpoint degree. Accordingly,
above theimage
w on themultiple covering,
the set of
points, numbering
thisdegree, corresponding
to the flatpoint
are identified asequivalent.
Weregard
the associated set of sheets aspinned
at this commonpoint,
which is referred to as a branchpoint
of order thedegree
less one. Theprojected
Gauss mapimage
with structure
imposed by
this identification is the Riemann surface of the Weierstrassfunction R
(w ).
For the F-RD surface the branchpoint
structure of the Riemann surface isgenerated by
thepropagation
of the first and second order branchpoints (labelled
inFig. 2,
andcorresponding
to the flatpoints
ofdegree
two andthree, respectively,
on theperiphery
of the basic surfaceelement)
at the 2w/3 and 3MN
vertices of thepolygon
in the tessellation of the five sheets.As the Riemann surface is
finite-sheeted,
the Weierstrass function of an IPMS isalgebraic,
and is hence
specified by
apolynomial equation
ofdegree equal
to the number of sheets[13].
The Weierstrass function of the F-RD surface is then the solution of the
quintic equation
a5(w)R~+a~(w)R~+a~(w)R~+a2(w)R~+aj(w)R+ao(w)
=
0
(2)
236 JOURNAL DE PHYSIQUE I N° 3
for a
particular
set of sixpolynomials a~(w ),
,
ao(w ).
Theparametrisation
of this surface is thencompleted
oncombining equations (I)
and(2)
once thesepolynomials
have beenspecified.
As the Gauss map
image
of the surface element of an TAMS tessellates aspherical covering,
this
polygon
must betriangulated by
one of the fifteen basic Schwarz tiles[14].
The TAMS of cubic symmetry are derived from the Schwarz case 4tiling
of the unitsphere by
the 48 reflectionimages
of thegeodesic triangle
with vertexangles (MN, w/3, w/2) (equivalent
toprojection
of the hexakis octalJedron onto a concentricsphere).
Thisunderlying triangular tiling
is shown instereographic projection
infigure
2. For this orientation the6,
8 and 12vertices of
angle Mm, w/3
andw/2
in thetiling
arepositioned
at(0,
cc,e~"'~e~~"'~),
~
*~~"'~)
and((/
±
I) e~"'~, l) e'~"'~), respectively (where
m is aninteger).
/
The set of roots of each coefficient
polynomial a~(w)
arenecessarily symmetric
withrespect
to theunderlying
Schwarztiling.
Thusthey
mustcomprise
the6,
8 and/or 12tiling
vertices and/or the 24
(respectively 48) images
of ageneral edge (respectively face) point.
Thepolynomials
with roots at theMm, w/3
andw/2
vertices are5
pi =
fl (w w~)
= w(w~ +1) (3a)
1=1
~
p2 =
fl (w w~)
= w~ 14
w~
+(3b)
j=1
12
p~ =
fl (w w~)
= w
~~ + 33
w~
33w~- (3c)
,=1
(where
theMm
vertex atinfinity
in the closedcomplex plane
issuppressed
inpi). Further,
foredges
of the tessellated Riemann surface to representplane
lines of curvature on theIPMS,
thedegree
ofa~(w
must be 4M(again counting
with thesuppressed
zero atinfinity) [8].
These facts are then sufficient to
specify
the form of each coefficientpolynomial
inparticular equation (2)
now becomeswhere n~,
, ao are real
numbers,
and the braces indicate the twopossibilities
for the cubic term.Additional information results from
demanding consistency
betweenequation (4)
and the known branchpoint
structure of the Riemann surface. Here we utilise thegeneral
observationthat,
local to a surface flatpoint
ofdegree bo
+I,
on thebo
+ I sheets of the Riemann surfacepinned
at thecorresponding
branchpoint (of
orderbo)
above the flatpoint
normal vectorimage
wo, the Weierstrass function branches have theasymptotic
form[8]
R~°~ ~(w ) yo(w wo)~~°
w- wo.
(5)
On the tessellation of the five
sheets,
over eachMm
vertex w~ of theunderlying tiling
infigure
2 three sheets arepinned
at a second order branchpoint
with theremaining
two sheets unbranched. The five branches are thengiven asymptotically
viaequation (5) by
R~(w )
y~(w
w~)~~ (once), R(w ) yj (twice)
: w - w~(6)
Substituting
the first form intoequation (4),
therequirement
that thequintinc
andquadratic
terms are of
leading (and equal) asymptotic
order in(w w~) implies
that thequartic
termcannot be present
(that is,
a~=
0)
and that the first of the twooptions
for the cubic termapplies.
Hence the form of thepolynomial equation
must now be"5P~P2~~
+"3P~~~
+"2P2~~+
"0 ~ °
(~)
for
which,
on substitution of the second form ofequation (6),
thequadratic
and constantterms are of
equal leading
order(namely zero),
asrequired. Similarly, equation (7)
is nowconsistent with the fact
that,
over each w/3 vertex wj of the Schwarztiling
thepair
of sheetspinned
at a first order branchpoint,
and the three unbranchedsheets, display
theasymptotics
R~(w )
~
yj(w wj)~
'(once),
R(w yj (three
timesw - w~
(8)
The final stage of the
parametrisation
is the determination of the real coefficients a~, a~, a~ and ao.Clearly
one such unknown may be divided out ofequation (7)
whileanother may be chosen without loss of
generality by
a suitablescaling
of R(w (amounting
to a choice of units for the coordinateaxes), leaving
twoparameters
to bespecified.
This is achievedby analysing
the Riemann surface structure on the five unbranched sheets above thew/2
vertices w~ of theunderlying tiling.
Fromfigure 2,
each suchpoint
is covered onceby
fourpolygons meeting
with commonw/2
vertex there, and four times as an interiorpoint
of thepolygon.
In the latter case the tourcoverings
are relatedby
reflection in the twoperpendicular underlying tiling edges intersecting
at thepoint,
andaccordingly
the fourcorresponding
Weierstrass function values at thispoint
occur as arepeated pair.
Forexample, evaluating equation (7)
at w = I(where,
fromequations (3a)
and(3b), pj(1)
=
2 and
p~(1)
=
-12)
there must exist real constants a and a and acomplex conjugate pair
(c, n)
such that-48a~R~+4a~R~-12a~R~+ao= a(R-a)(R-c)~(R-n)~. (9)
Equating
coefficientsyields
thepair
ofhomogeneous
relations16 a~ a~ = 25 ao a~, 135
al
a~=
al (10)
thus
removing
the final twodegrees
of freedom.Choosing,
say a~=I,
a~=-15,
a~ =5 and ao =
48,
the Weierstrass function of the F-RD surface is thengiven by
p)p~R~- lsp)R~+5p~R~-48
= 0
(II)
where pi and p~ are the Weierstrass
polynomials
of the I-WP and Dsurfaces, given
inequations (3a)
and(3b).
The exact
parametrisation
of the F-RD surface is thus attainedby substituting
theWeierstrass function solutions of
equation (11)
into therepresentation (I). Although
thequintic polynomial equation
cannot be solvedanalytically,
allrequired
surface information(such
as local coordinates and theglobal properties
of surface-to-volumeratio,
surface area andintegral squared
Gaussiancurvature)
can be extractednumerically
in asimple
and economical manner. The extent of thepath integration
inequation (I)
may be restricted to thepolygonal region
of thecomplex plane
shaded infigure 2,
as thecomplete
TAMS is thengenerated by
mirror reflection in thebounding planar
curves of the basic surface element. Thecorresponding polygonal region
of the Riemann surface(that is,
thecorresponding
branch of the Weierstrassfunction)
is ascertainedby determining
the five root ofequation (I I)
for a238 JOURNAL DE PHYSIQUE I N° 3
particular point
w on the real axisedge
0< w <
~
of the
polygon.
These five roots/
comprise
a real number and twocomplex conjugate pairs.
The real rootsrepresents
the relevant function branch since this real axissegment
is theimage
of aplane
line of curvature on this sheet. The function value of this branch at aneighbouring point
in theregion
is thendetermined via Newton's method
using
this real root as the initial estimate.Continuing
thisprocedure,
the entire basic surface element is thus constructedpointwise.
Thedensity
of the array of suchpoints
necessary toyield
accurate values forglobal properties
of the IPMS is foundby calculating
theintegral
Gaussian curvature of the surface element. With theGaussian curvature of the surface at the
point
with normal vectorimage
wgiven by [9]
K=
-4(1+ (w(~)~~ (R(w)(~~,
numerical
integration
of thisquantity
over the surface element must recover the exact value of 5w/12
to within the desired tolerance.Conclusion.
The above
parametrisation
demonstrates theutility
of thegeneral algorithm [8]. Application
of the
algorithm
to aparticular
TAMSonly
assumes aknowledge
of thegeneric
Gauss mapimage
of the basic surfaceelement, specified by
thedegree
of each flatpoint
and the nature of theposition
of itsimage
withrespect
to thecorresponding
Schwarzspherical tiling (I.e.
whether it lies at a vertex, or on an
edge,
or in theinterior,
of atriangular tile).
Such information may be inferred from soap filmexperiments,
and has beenextensively
tabulated for the minimal balance surfaces of Koch and Fischer[15]. Having
established the basicstructure of the Gauss map
image,
the determination of the Weierstrass functionpolynomial equation
up to a number of real constants(that is,
up to the stage embodied inequation (7)
for the F-RDsurface)
is thenstraightforward
for any TAMS.The
symmetries relating
thespecial
sets ofpoints
on the IMPS fundamentalunit, possessing
common normal vectors
imaged
at vertices of the Schwarztiling,
in tumimply
relationsbetween the
corresponding
Weierstrass functionvalues, yielding
additional constraints on thepolynomial equation.
This reduces the number of nontrivial constantsremaining
in theparametrisation
to the number ofdegrees
of freedom of the Gauss map consistent with thesesymmetries. By
definition these constraints arepurely algebraic.
For the F-D surface theconsistency
condition(Eq. (9))
for thepolynomial equation
isreadily
solved(as given
inEq. (10)).
For IPMS ofhigher
genus and/or lowersymmetry
thisprocedure
becomesalgebraically lengthy
andproduces multiple solutions,
from which the desired one must be chosen in accordance with the known Weierstrass function behaviour. However this is not asevere
deficiency
in most situations ofphysical
interest since the inferred genera andsymmetry
ofperiodic
structures observed in bicontinuous media lie within the range ofpractical applicability
of theprocedure.
The
algorithm
suffices if the number of undetermined constants isequal
to the number of free variables associated with thecrystallographic
group of the TAMS. The symmetry criteria thusimpose
a one-to-onecorrespondence
between the Gauss map and theTAMS,
andyield
apurely algebraic
surfaceparametrisation.
This is the case for the F-RD surface(in
which the cubic symmetry admits nodegrees
offreedom)
and for themajority
of the IPMS discoveredby
Schoen andby
Koch and Fischer.There are however surfaces for which the
algorithm
alone isinsufficient,
and must besupplemented
with additional considerations[7].
In these cases the number of variables unconstrainedby
thealgorithm
exceeds that of the IPMS space group. This circumstance isnot unnatural since the
approach
is based upon the Gauss map and thesymmetries
derived from it theresulting algebraic
constraints representlocally
necessary conditions which may notcompletely
fix the desiredglobal
surface symmetry. This then entails the introduction ofglobal
closureconditions, stipulating
that the IPMS is that member of the continuum oflocally
admissable surfaces which Jocks into thecrystallographic
sites. Theseconstraints, involving
determination of surface coordinates and henceintegration
of the Weierstrassfunction,
arestrictly
transcendental. Such a situation arises inanalysing
the Bonnet associatefamily
of an TAMS(obtained
onreplacing
the Weierstrass functionR(w) by e~°R(w),
0< b
<f).
As the Gauss map istotally
insensitive to the Bonnettransformation,
the 2existence of an associate TAMS to, say, the F-RD surface derived above can
only
beascertained
by
solution of acomplicated
transcendentalequation.
References
ill For a review see J.
Phys.
FranceColloq.
51 (1990) C7.[2] FONTELL K., Colloid
Polym.
Sci. 268(1990)
264-285.[3] HYDE S. T., J.
Phys.
FranceColloq.
51(1990)
C7-209-228.[4] LANDH T., preprint (1991).
[5] SCHOEN A. H., Infinite
periodic
minimal surfaces without self-intersections, NASA Techn. Rep.D-5541 (1970).
[6] FISCHER W., KOCH E., Z.
Kristallogr.
179 (1987) 31-52.[7] KARCHER H., The
triply periodic
minimal surfaces of Alan Schoen and their constant meancurvature
companions, Vorlesungsreihe
No. 7,Sonderforschungsbereich
256, Institut furAngewandte
Mathematik der Universitdt Bonn, FederalRepublic
ofGermany
(1988).[8] FOGDEN A.,
preprint
(1991).[9] FOGDEN A., HYDE S. T.,
preprint
(1991).[10] FOGDEN A., HYDE S. T.,
preprint
(1991).[I Ii LIDIN S., HYDE S. T., NINHAM B. W., J.
Phys.
France 51(1990) 801-813.[12] WEIERSrRASS K., Math. Werke~ Band 3
(Mayer
u.Mayer,
Berlin, 1903).[13] SPRINGER G., Introduction to Riemann surfaces
(Addison-Wesley, Reading,
Massachusetts,1957).
[14] ERDLLYI A, et al.,
Higher
Transcendental Functions, BatemanManuscript Project
(McGraw-Hill, 1953).[15] KocH E., FISCHER W., Acta Cryst. A 46