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The oCLP family of triply periodic minimal surfaces

Djurdje Cvijović, Jacek Klinowski

To cite this version:

Djurdje Cvijović, Jacek Klinowski. The oCLP family of triply periodic minimal surfaces. Journal de

Physique I, EDP Sciences, 1993, 3 (4), pp.909-924. �10.1051/jp1:1993172�. �jpa-00246772�

(2)

Classification

Physics

Abstracts 01.55

The OCLP family of triply periodic minimal surfaces

Djurdje Cvijov16

and Jacek Klinowski

Department

of

Chemistry, University

of

Cambridge,

Lensfield Road,

Cambridge

CB2 IEW, U.K.

(Received 12 October 1992,

accepted

in

final form

20December 1992)

Abstracto- CLP surfaces with orthorhombic distortion (OCLP for short) are a

fattily

of two- parameter

triply periodic

embedded minimal surfaces. We show that they

correspond

to the

Weierstrass function of the form ~ where

N/T~

(A + B) T~ + (2 + AB) T~ (A + B) T~ + I A and B are free parameters with 2 < A, B

~ 2 and A

> B, T is

complex

with T « I and

K real and

depends

on A and B. When B

= A, the OCLP

family

reduces to the one-parameter CLP

famfly

with

tetragonal

symmetry. The

Enneper-Weierstrass representation

of OCLP surfaces

involves

pseudo-hyperelliptic integrals

which can be reduced to

elliptic integrals.

We derive

parametric

equations for OCLP surfaces in terms of

incomplete elliptic integrals

F (#, k) alone.

These

equations completely

avoid

integration

of the Weierstrass function, thus

making

the use of the

Enneper-Weierstrass representation

unnecessary in the

computation

of

specific

OCLP surfaces.

We derive

analytical expressions

for the normalization factor and the

edge-to-length

ratios in terms of the free parameters. This solves the

problem

of

finding

the OCLP saddle surface inscribed in

given

a

right

tetragonal

prism,

crucial for the modelling of structural data

using

a

specific

surface, and enables

straightforward physical applications.

We have

computed exactly

the -coordinates of OCLP surfaces

corresponding

to several

prescribed

values of the

edge-to-length

ratio.

Introduction.

A

triply periodic

embedded minimal surface

(TPEMS)

is an surface in three-dimensional space which is

infinite, minimal, periodic

in three

independent

directions

(I,e.

has space group

symmetry)

and free of self-intersections

(embedded). Approximately

40 TPEMS have been described

by

various methods

(now mainly crystallographic) [1-4]. Previously thought

of

only

as mathematical

objects [5],

in the last 20 years TPEMS have become of

great

interest to

physicists, chemists, biologists

and material scientists

[6-7].

Of

primary

interest is the fact that these surfaces possess translation symmetry which in

principle

enables them to be matched to actual structures.

Also,

since a TPEMS divides three-dimensional space into two

disjunct regions (labyrinths)

in such way that each

region

is

multiply

connected and the structure

bicontinuous, descriptions

of

interpenetrating crystalline

structures with

large

unit cells and

complicated

networks of cages and channels are

possible.

TPEMS are a useful

crystallographic

(3)

910 JOURNAL DE PHYSIQUE I 4

concept

for the

description

of condensed matter, and are

increasingly frequently

referred to as

crystallographic

minimal surfaces

[8-13].

In

general,

the local

Enneper-Weierstrass representation [5]

w

x = Re

(I r~) R(r)

dr

w~

y = Re

l~ I(I

+

r~)R(r)

dr

(I)

w~

w

z = Re 2

rR(r )

dr

w~

where

i~

=

I and r

= r~ +

ir~,

enables us to associate with every function

R(r) (the

Weierstrass

function), analytical

in some

simple

connected

region

of

e, except

at isolated

points,

a

unique parametrized

surface

r(r~, r~)

which is

guaranteed

to be a minimal surface.

However,

such a surface is not

necessarily

free of self-intersections and its

possible periodicity

must be examined

separately.

The Cartesian coordinates of any

point

are

expressed

as the real

part (Re)

of contour

integrals,

evaluated in the

complex plane

from some fixed

point

wo to a variable

point

w. A

specific

minimal surface can be determined

by integrating

its

Weierstrass function. So

far,

the

integrals (I)

have been evaluated

analytically only

for a handful of minimal

surfaces,

such as

Enneper's

and Scherk's surfaces

[5].

However,

they

can

((ways

be evaluated

by

numerical

integration.

The crucial

problem

in

theory

of TPEMS is

deriving

the Weierstrass

function,

and since a

new method for its construction has been

developed [14-17], approximately

20 different

surfaces have been described in terms of the

Enneper-Weierstrass representation. However,

it has been shown that

one-parameter

tD

(and

its

adjoint tP) [18-19]

and CLP

[18, 20]

families of

TPEMS,

as well as

zero-parameter D,

G and P surfaces

[21]

can be

parametrized

in terms of the

special

function known as the

incomplete elliptic integral

of the first kind.

Rigourous

mathematical

description

of these surfaces

completely

avoids the

integration

of the Weierstrass

function,

and their

computation

obviates the need for

using

the

Enneper-Weierstrass representation.

We now demonstrate that his is also true for OCLP surfaces.

The main obstacle to a wider

application

of TPEMS in

experimental

science is that most of them have been described

empirically,

without the

precise

mathematical

specification

necessary for a

quantative comparison

with

physical

systems. It is therefore essential to

quantify TPEMS,

and to establish

straightforward procedures

to compare such surfaces with actual structures. Even in the case of

mathematically

well-described surfaces

(with

a known

Enneper-Weierstrass representation),

such

procedures,

as well as

quantative computation,

are

missing.

This

work,

as well as

previous

papers

[18-20]

stresses the

computational

aspects of the

theory

of TPEMS.

The

Enneper-Weierstrass representationo

We do not know how many different minimal surfaces can be described

by

the Weierstrass function of the form

~~~~ ~/r~

+ 2

pr~ +~ r4

+ 2

pr~

+ ~~~

where r

= r~ + I r~, while the normalization factor K and the coefficients p and A are real.

These surfaces can be

non-periodic,

or

singly, doubly

or

triply periodic. Further, they

can be

(4)

embedded or unembedded. The Weierstrass function

(2)

is

single-valued

on the two-sheeted

compact

Riemann surface of genus 3 with

eight

branch

points

of order one, and their

distribution makes it

possible

to

classify

all minimal surfaces described

by (2).

Here we consider surfaces with all

eight

order one branch

points

distributed on the unit circle.

Detailed

analysis

is made

possible by introducing

the

following mapping

defined in a two- dimensional domain.

= 2

~A~

~~~ ~~~

Since the

corresponding

Jacobian is

(B-A)/2,

the

mapping

is

regular

for A ~B and

A <B. We choose the former case, for which the inverse

mapping

is of the form

A=-p+ fi

~~~

B=-p- p~+2-A

provided

that p ~ + 2 A m 0. In terms of

(3),

all branch

points

of the Weierstrass function

(2)

are

given by

bj,

~ = 4/

/

b~, 4 =

bj,

~ ~~

b5

~ = 4/

/ b~

~ =

b5

~.

Further, expressions (5)

and the condition

[b,[

=

I

(I

=

I to

8) give

the values of

A and B for which all

singularities

of

(2)

lie on the unit circle. The solution is the domain

5~~= ((A,B) -2«A,B«2,A~B)

in the AB

plane,

I.e. the domain

5~~~ =

((p,A) -4p +2m0,

A

+4p +2«0,

A

-p2-2«0)

in the

HA plane,

both shown in

figure

I.

Among

all

possible

minimal surfaces

corresponding

to the Weierstrass function

(2)

with branch

points only

on the unit circle, we have one two- pararneter, 4 one-parameter and 5

special

«

Zero-parameter

» surfaces

(see

Tab.

I).

Since the

Weierstrass function R

(r )

is known for all these

surfaces, they

are

fully

described in terms of the

Enneper-Weierstrass representation. Apart

from CLP

surfaces,

no

single-parameter family

has been examined.

We shall consider in detail the

two-parameter family

of TPMES

corresponding

to the

Weierstrass function

~~~~~

~/r8- (A +B) r6+ (2

+

AB) r4- (A +B) r2+1

~~~

where A and B are free parameters with

A~B and

-2<A,B<2

K is normalization

factor,

and

r is

complex

with

jr

« I. The existence of such surfaces was established in 1988

by

Koch and Fischer

[4b]. They

have orthorhombic symmetry and are

designated

OCLP because

they

may be derived from the

tetragonal

CLP surfaces where the

bounding

unit is a

right tetragonal prism

with

edges

a, b and c

[20] by elongation

or

(5)

912 JOURNAL DE

PHYSIQUE

I N° 4

P~

t2

~

-la)

p

~

b)

i fi

~

A

~

f~

Fig. I. -rameter

for

all

possible inimal surfaces

(listed in

Tab. I)

corresponding

eierstrass R IT ) =

~ withall

lyingon theunit

N/T ~ + 2 p T ~ + T ~ + 2 p T

(6)

Table I. The Weierstrass

functions

and the parameter domain

for

all

possible

minimal

surfaces

with

eight

order-one branch

points

on the unit circle.

Minimal

surface(s)

Weierstrass function

R(r)

Parameter Position in

domain

figure

~

A p ~ 2-< 0 whole

~~~~

~~~~~

VT

~

+ 2 MT~ + A

r~

+ 2

p r~ + l

~~~~~~

r~+ pr~+1

~

K

(r~+ I)~/r~+2(p I)r~+1 ~~"

~~ ~~

(r2-1)~/r4+2(~

+

i)r2+1 ~~""

"° ~~

Scherk's first-order p

tower ~

~ 4 ~

K

(r~

+

1)~ ~~

Adjoint

to Scherk's

P3

first-order tower

~~

r

(~2 ~)2 ~4

Se'f-adj°I"t

CLP

fi PO

r + 1

(7)

914 jOURNAL DE PHYSIQUE I N° 4

compression

in either of two horizontal directions. As a consequence, the

tetragonal family

of CLP surfaces is contained within the

family

of OCLP surfaces as a

limiting

case.

We consider the

properties

of a finite minimal surface

piece

of the OCLP surface

(referred

to as the OCLP saddle

surface)

which can be

thought

of as inscribed in the

parallelepiped

with

edges

a, b and c. The OCLP saddle surface is bounded

by

four

straight-line segments (lying

on

the

edges

of the

right prism)

and four curvelinear segments

(lying

in the bases of the

right prism).

The saddle surface is

produced by integration

of the Weierstrass function

(6)

over the entire unit disk. We note

that, by

contrast, the FlhchenstUck

(surface element),

from which the infinite OCLP surface is

generated by

reflection or rotation

operations

over the surface

boundary,

is

produced by integration

over the first

quadrant

of the unit disk.

The Weierstrass function

(6) completely specifies

the first and second fundamental forms of the OCLP

family.

For

example,

the Gaussian curvature of a

specific

surface at the

point

corresponding

to w is

[5]

K=

)~

(l

+

(°'( ) (R(°')(

~.

In

principle,

the

Enneper-Weierstrass representation

of the OCLP

family (equations (I)

with function

(6)) readily

enables the

computation

of a

specific

OCLP saddle surface

(corresponding

to

particular

values of the free parameters A and

B) prior

to

scaling (normalization

factor

K is

unknown).

In

practice,

these

computations

are cumbersome since numerical

integration

is not as

straightforward

as it is often

thought.

In

particular,

numerical

integration

must be

preceded by

a careful

analysis

of the behaviour of the

integrand.

An

appropriate

numerical method must then be chosen and the

computational output carefully

examined in order to

establish confidence in the result. A distinction must be made between « well-behaved

» and

«

badly-behaved

»

integrands [23].

When used

unadvisedly,

which is

encouraged by

the

ready availability

of

sophisticated

computer programs, numerical

integration

may lead to serious

errors. Our

integrands

are «

badly-behaved

» since

they

possess

eight singularities

on the unit

circle

(I.e.

the

integrals

are

improper),

which makes them

particularly

difficult to handle.

Furthermore, large portions

of our surfaces are

generated by

small

regions surrounding

the

singularities,

and it is necessary to

employ

some

procedure

for the elimination of

singularities,

or

finding asymptotic expansions

of the

integrals.

Numerical

integration

is

normally

used when

analytical techniques

fail. Before

using

numerical

integration,

it is

important

to ensure that the

integral

in

question

cannot be

analytically

evaluated.

Parametrization of the OCLP

familyo

The

integrals

in the

Enneper-Weierstrass representation

of the OCLP

family (equations (I

with Weierstrass function

(6))

are

hyperelliptic.

In

general, hyperelliptic integrals

cannot be

expressed

in terms of a finite number of

elementary

or

special

functions. In other

words, they

cannot be

analytically

evaluated. It is thus necessary to use direct numerical

integration

or

complicated

series

expansions.

Very occasionally,

some

hyperelliptic integrals (known

as

pseudo-hyperelliptic)

can be reduced to

elliptic integrals,

I.e.

integrals involving

square roots of

polynomials

of the third and fourth

degree

with distinct roots.

Further,

any

elliptic integral

can be

expressed

as the sum of

elementary

functions and of the three

special (non-elementary)

functions known as

canonical forms of

incomplete elliptic integrals

of the

first,

the second and the third kind

[24- 25].

There are several definitions of the normal form

(Legendre-Jacobi, Riemann, Weierstrass,

Carlson,

etc.

)

of which the

Legendre-Jacobi

form is the most common. The main

advantage

of these

special

functions is that their

properties

are well-established and their

computation

is

(8)

easy. The evaluation of

elliptic integrals (I.e.

of

special

functions known as

incomplete elliptic integrals

of the

rust,

second and third

kind),

is now

mainly

based on two iterative numerical

methods which are

highly specific

to the nature of the function

[25-29].

The traditional

arithmetic-geometric

mean method was outlined earlier

[19],

and

employs

successive Landen and Gauss transformations of

elliptic integrals.

The method is

simple,

converge

quadratically

and can be

applied successfully

to

integrals

of the first and second

kind,

but is

unsatisfactory

for

integrals

of the third kind.

By

contrast, Carlson's method

[26]

is based on a new definition of canonical forms and on successive

applications

of the

duplication

theorem. The method can be

applied

to all three kinds of

integrals.

We will show that the

Enneper-Weierstrass representation

of the OCLP

family

of TPEMS involves

pseudo-hyperelliptic integrals. By reducing

them,

resulting elliptic integrals

are

expressible

in terms of

incomplete elliptic integrals

of the first kind

(in

its

Legendre-Jacobi

normal form F

(@, k)) only.

F

(@, k)

is a

special

function defined as

~

~~~ ~~ ~

~/(l ~~~l

k~

t~) i~ ~

where y = sin @. We assume that the variable

k,

known as the

modulus,

is real and lies in the interval

lo, I]

and that the variable @, known as the

amplitude,

is a

complex

number.

Reducing hyperelliptic integrals

is made

possible by

the

mapping (3).

In order to reduce

integrals (I)

with

R(r)

in form

(6),

we consider three

complex integrals

~°~°'~~~°~°'°~~~ wo~/r8-

(A+B)r6+ (2+AB)r4- (A+B)r2+1

~~~~

~~

'~ °~ two~/r~-(A+B)r~+(2+AB)r4- (A+B)r~+1

~~~~ ~~~~~~

~ ~

~o

N/r~ (A

+

B) r~

+

~~~B)

r4- (A

+

B) r~

+

~~~~

which

give

X*(")~1~0~~2

y* (w )

= I

(r~

+

r~) (8)

z*(w

= 2

ri

so that

(x,

y,

z)

=

rite (x*),

Re

~y* ),

Re

(z*)]

holds.

The

mapping

r'

(see

Tab.

II)

reduces

ro

and

r~

so that

(8) gives

~ ~ ~

wi

dt

~

~°'~

~

~°'°~

~ ~~

2

~, ~/(t

+

2) (t

A

) (t

B

)

~

~*~~°

"

~*~"°~

~

) w~

~/(t 2) (/~

A

) (t

B

~~~~

with

w]

and w' defined in table II and

-2<A,

B<2 with A~B. The

mapping

r"

(see

Tab.

II)

reduces

rj

with the result

(9)

916 JOURNAL DE

PHYSIQUE

I N° 4

Table II. Reduction

of pseudo-hyperelliptic integrals

to

elliptic integrals.

Mapping Inverse Differential Fixed limit

mapping

~ ~'

~

~~~~2 $~~()+)j ~~~~~ ~,~W~+I

r +2 r' -2 W( ~2

~

~~V~

~~

+

~ ~~

(l

+~r"~

fi~~

+

~~

~ ~

~ ~ 2

where

"

~2+B ~ ~2+A ~~~/(2

+A)(2 +B)

with a

~

p

and the limits

wl'

and w" are

given

in table II.

We see that the

integrals

in

(I)

which describes OCLP

family

can be reduced to

elliptic integrals.

All that remains to be done is to express the results in terms of

Legendre-Jacobi

forms of the

incomplete elliptic integrals

of the first kind. We

integrate

from wo =

0,

and

by employing

the

procedure

described elsewhere

[18]

evaluate

integrals

in

(9) using integral

tables in

Byrd

and Friedman

[24].

The Cartesian coordinates x, y and z of a

specific

OCLP saddle surface in the Cartesian coordinate system shown in

figure-2

are

given by

the

parametric equations

x(r,

w = Kg~ Re

[F (arcsin P~ (w ), k~)]

2

y

(r,

q~

)

= Kg~ Re

iF (arcsil~ P~ (w ),

k~ )1

(10)

z(r,

w

= zo Kg~ Re

[F (arctan P~(w ), k~)]

where

zo =

z(o)

= Kg~ F

arctan

,

/~

k~

Re stands for the real part of the

complex Legendre-Jacobi

function

F(@,k)

and

w is

complex

w

= rexp

(I,

w

),

with

(w

« I. For any

particular

values of the two free

parameters

A and B the

multiplication

factors g~, g~ and g~, and the moduli k~, k~ and k~, as well as zo are real constants, while

P~(w ), P~(w )

and

P~(w )

are

complex

functions.

Thus,

all

components

of

equations (lo) depend

on the value of the same two free real parameter and apart from the normalization factor K, this

dependence

is described in

table II.

Since we have

gz =

)gxgy kj=

I

-kjkj

and the

multiplication

factors and the moduli are related

(see

Tab.

IV),

of the six constants

(10)

z

y

b

a

Fig.

2. The Cartesian coordinate system anached to the OCLP saddle surface described by

equations

(10).

Table III.

Multiplication factors

g~, moduli

k;

and

complex functions P, (w )

which appear in the

parametric equations for

the orthorhombic nvo-parameter OCLP

family of triply

periodic

embedded minimal

su~fiaces.

A and B are

free

parameters with

-2<A,

B < 2 and A

~

B,

while

w is

complex

with w « 1.

X y Z

2 2 2

~

fi fi~ N/(2+A)(2-B)

~ ~~~ ~-~ (2~~~)(/~B)

~

l 2w 2iw

1-w~

'~°'~ gxl+w~ gyl-w2 il+w2

(11)

918 JOURNAL DE

PHYSIQUE

I N° 4

Table IV.

Relationships

benveen

multiplication factors

g; and moduli

k; appearing

in the

expressions for

the

parametric equations for

the orthorhombic nvo-parameter OCLP

family of triply periodic

embedded minimal

su~fiaces.

X y Z

/I-kjkj

~/I-kj(

I

I-kjk~

~'

l

k(

I

kj

~

~/(l k()(I ()

( g]

i

~

g(

i

~ g] g] g(

+

g(

9y

9x

(g~, g~,

g~, k~, k~ and k~) which describe a

specific

OCLP surface and appear in

( lo) only

two are

independent.

There are several reasons

why equations (10)

are

preferable

to the

Enneper-Weierstrass representation

in the

computation

of

specific

OCLP surface. It has been shown that the

integrals

in the

Enneper-Weierstrass representation

of OCLP

family

allow

analytical

evaluation

(resulting

in

parametrization ( lo)).

There is therefore no need to evaluate them

numerically.

Equations (10)

are

analytical expressions,

and the function

F(@,k)

has well-known

properties. Further, equations (10) require

the evaluation of

F(@, k)

which is much more

straightforward

than numerical

integration. Finally,

in view of the fact that numerical estimation of

integrals

fails close to the

singularities, equations (10)

are

superior,

since the function

F(@, k)

is finite in the entire

complex plane [25],

even at

singular points

of the Weierstrass function defined

by (5). Thus, equations (10) completely

obviate the need for

using

the

Enneper-Weierstrass representation,

I.e. avoid

integration

of the Weierstrass function in the

computation

of

specific

OCLP surfaces.

However,

this is not to say that the use of the Weierstrass

function,

necessary for the calculation of the Gaussian curvature, metric and

topology,

can be avoided.

However, computation using (10)

does not

by

itself solve the

practical problem

of

computing

a OCLP surface for a

given edge-to-length

ratio of the

bounding

unit.

Computation

of OCLP surfaceso

A OCLP saddle surface is bounded

by

a

right tetragonal prism

with

edges

a, b and

c. For any

pair

of values of free

parameters (

2 ~

A,

B

< 2 with A

~

B),

the

equations ( lo) give

x(bi )

= a/2

y(bi )

=

b/2

z(bi )

= qj

(I la) x(b5)

=

a/2

y(b5)

= b/2

z(b5)

= q~

where

bi

and

b5

are branch

points

defined in

(5),

and

[qi[

+

[q~[

= c.

Further,

it is not difficult to show that

Re

iF(arcsin P~(bi), k~)i

=

K(k~)

Re

[F (arcsin P~(b5), k~)]

=

K(k~) (I16)

(12)

and

c = Kg~ Re

[F (arctan P~(I ), k~)]

= Kg~

K(k~) (llc)

where K stands for the

complete elliptic integral

of the first

kind, K(k

= F

(ar/2,

k

).

From

(10)

and

(11)

we obtain the normalization factor K

~

g~

I(k~ )

g~

~(k~

)

g~

I(k~

~

~~'

~ ~~~~

which is a real and

positive

function of the free

parameters. Using (12)

and table

III,

K can be

easily analytically expressed

in terms of these parameters, so that an

expression

for

K = K

(A,

B

)

is

readily

available.

Equations (12)

also define six

possible edge-to-length ratios,

of which

only

two are

independent.

Table III

gives readily

available

analytical expressions

for the

edge-to-length ratios, involving

the free parameters A and B.

They

are

independent

of the normalization factor K, and

only depend (in

a continuous

manner)

on the free parameters on

the one-to-one basis.

The constant zo in

(lo)

is so chosen that the

parametric equations

describe an OCLP saddle surface in the coordinate system with the

largest

absolute value of the Gaussian curvature at the

origin (see Fig. 2).

It was shown earlier

[20]

that in case of CLP surfaces this

point

halves the

height

of

right tetragonal prism (I.e.

the

edge

c is devided in the I : I ratio and zo =

c/2). However,

for OCLP

surfaces,

the

edge

c is divided in the ratio

(see Fig. 3)

~

d~ K(k~)

~~~~

~~ F

(arcsin

,

~)

gx

where

d,

=

[q;[

and q; is

given

in

(lla). Analysis

of

(13)

reveals that D

= I for

A + B

= 0

(I.e.

CLP

surfaces)

and D @ I for A + B W 0.

Parametric

equations (lo)

and

expressions

for the normalization factor

(12) give

x(r,

q~

=

£ /

Re

iF (arcsil~ P~(w ),

k~ )1 2

K(k~ )

y(r,

w

)

=

] j

Re

IF (arcsin Py(w ), ky)1 (14)

( y)

z

(r,

q~

= zo

/

Re

iF (arctal~ P~(w ),

k~

)1

thus

providing

the solution of a

problem

which can be formulated as follows : « find the coordinates of the OCLP saddle surface which is bounded

by

the

given right tetragonal prism

with

edges

a, b and c". This means that for any

specific

values of the

length

of

edges

a, b and c there is

always exactly

one OCLP saddle surface

completely

described

by (12)

and

(14)

where k~, k~, k~,

P~(w ), P~(w )

and

P~(w )

all

depend

on the values of the two free

parameters, have the same

meaning

as in

(lo),

while w

=

rexp(iw

with 0 « r « I and 0 < w « 2 ar.

With B

= A

=

fi

where 0

< A

< 2

(-

2

< A

< 2

),

the

two-parameter

OCLP

family

with orthorombic symmetry is reduced to the one-parameter CLP

family

with

tetragonal

symmetry and

equations (10)

and

(14)

became

equations

of CLP surfaces in full agreement with results in

[20].

In

practice,

we need to find the values of the free parameters A and B for

given

(13)

920 JOURNAL DE

PHYSIQUE

I N" 4

a)

b)

Fig.

3. Four OCLP saddle surfaces

corresponding

to four different

bounding

units. The surfaces are calculated

using equations (12)

and (14), and the parameters used in the

computation

are

given

in table V.

(14)

Cl

di

Fig.

3

(continued).

(15)

922 jOURNAL DE

PHYSIQUE

I N° 4

a, b and c, I.e. to solve a system of two transcendental

equations

with two unknowns in

(12)

and

apply (14)

and calculate the coordinates for these calues of the free parameter. This

procedure

allows us to model the

given

structural data

belonging

to orthorombic symmetry and confined to the volume of a

right tetragonal prism by

a

specific

OCLP surface. Since

(12)

and

(14)

contain no

adjustable

parameters, « yes-or-no »

modelling

is

possible.

In other

words,

we can

always

decide whether or not a

given

data set matches a

specific

OCLP surface to a

prescribed degree

of accuracy.

We cannot recommend a numerical method of

calculating

the free parameters A and

B

corresponding

t

given

values of a, b and c, because of the absence of reliable

general

methods for

solving systems

of two and more nonlinear

equations [29b].

In

particular, considering

the very

complicated expression

for the

edge-to-length

ratios defined

by (12),

it

seems that

employing

of multidimensional

Newton-Raphson

method

involving

derivatives is

not

promising

even if

approximations

for the derivatives are used. This

problem

deserves additional

analysis,

but in most

applications

it is sufficient to use the iterative two-dimensional

fixed-point

successive substitution

»)

method

[30]

Uk "

d~l(Uk-l'~k-I)

Vk

"

d~2(Uk-I, Vk-I)

where k

=

1, 2,

3, is the number of iteration steps and uo, vo are the initial guesses for the

roots. The

advantage

of this method is its

simplicity

and

flexibility

in

choosing

of

fixed-point

equations

u

= Ah

(u, v)

and v

=

4l~(u, v) corresponding

to a guven system of

equations fi (u,

v

=

0

f2(u,

v

)

= 0.

The

disadvantage is, however,

that iteration does not

always

converge ; when it

does,

the convergence is slow.

The evaluation of functions F

(@, k)

is

computationally straightforward,

and

appropriate

programs are

easily

available either as user-callable routines in

general

purpose subroutine libraries or built-in functions in various software

packages.

Carlson's and Bulirisch's

algorithms,

based on Carlson's method and the

arithmetic-geometric

mean method, are the most

satisfactory.

Almost all mathematical subroutine libraries

(such

as the NAG FORTRAN

routine

S21BBF(X,

Y,

Z, WAIL),

where WAIL is a

machine-dependent constant)

use

Carlson's

algorithm

which calculates

R~(x,

y,

z),

the

incomplete elliptic integral

of the first kind in Carlson's canonical form. The source code of its FORTRAN

implementation

can

be,

for

instance,

found in reference

[29a].

This

callable,

robust and

highly portable

routine rf

(x,

y, z

)

enables the

computation

of F

(@, k)

with

F

(@, k)

= sin rf

(cos~ @,

I K~

sin~

@, I

).

Similarly,

the

computation

of

F(@, k) using

Bulirisch's

algorithm (the

source code is available in reference

[29b]

as routine e12

(x, k~,

a,

b))

can be

performed

with

F

(@, k)

= e12

(tan @,

I K~,

l, 1).

It should be noted that in both routines

changes

have to be made

regarding

the

complex

aritlimetic. We use a

simple

and very fast

algorithm

on the

arithmetic-geometric

mean

method,

because its use for the evaluation of F

(@, k)

for

complex

values of the

amplitude

is well

documented. Its

only

known

unsatisfactory

behaviour is for k

~ l and

~

ar/2,

but these

cases do not arise here. The software for mathematical

applications (Mathematica, MathLab,

Maple)

contains

elliptic integrals

as built-in functions. For

instance,

Mathematica has

elliptic integrals

and all related functions

(theta functions,

Jacobi and Weierstrass

elliptic functions), probably

based on the

arithmetic-geometric

mean method

(note

that

F(@,k)=

Elliptic

F

[@, k~]).

(16)

There is no

published computation

of OCLP surfaces. In order to

compute

four OCLP saddle surfaces

(Fig. 3) corresponding

to different

lengths

a, b and c of the

bounding unit,

we use

equations (12)

and

(14)

and

procedures

described above for

root-finding

in a two-dimensional

non-linear system and

computing

the function F

(@, k).

The

length

of

edge

a is assumed to be

unity,

and all

quantaties required

in the calculation are

given

in table V.

Table V. Constants used in

computation of

the various OCLP saddle minimal

su~fiaces

shown in

figure

3.

Figure

A B K

Edges

of

bounding

unit

a =

3 a 1.34188481 1.34188481 0.55126521 b

= I

c = I

a =

3 b 1.96999281 1.96999281 0.63302609 b

= I

c =

2

a =

3 c 0.65299525 1.93971240 0.36523922 b

= 3/4

c = I

a =

3 d 1.97469804 0.29508854 0.51759396 b

= 5/4

c = 3/2

Acknowledglnent.

We are

grateful

to Shell

Research, Amsterdam,

for

support.

References

[1] SCHWARz H. A., Gesammelte Mathematische

Abhandlungen (Verlag

Julius

Springer,

vol. I, Berlin, 1890).

[2] SCHOEN A. H., Infinite Periodic Minimal Surfaces Without Self-intersections, NASA Technical report No. TN D-05541 (1970).

[3] KARCHER H., Manuscr. Math. 64 (1989) 291-337.

[4]

(al FISCHER W. and KOCH E., Z. Krist. 179

(1987)

31-52 ; (b) KOCH E. and FISCHER W., Z. Krist, 183 (1988) 129-152 ;

(c) FISCHER W. and KOCH E., Acta

Cryst.

A 45 (1989) 166-169 ; A 45 485-490 A 45 558-563 ; A 45 726-732 ;

(d) KOCH E. and FISCHER W., Acta

Cryst.

A 45 (1989) 169-174 AM (1990) 33-40 ; (e) FISCHER W. and KOCH E., in Ref. [7], p. 131-147.

[5] NITSCHE J. C. C., Lectures on Minimal Surfaces, vol. I

(Cambridge University

Press, 1989).

[6] ANDERSSON S., HYDE S. T., LARSSON K. and LIDIN S., Chem. Rev. 88 (1988) 221-242 and references therein.

(17)

924 JOURNAL DE PHYSIQUE I N° 4

[7] DUBOIS-VIOLETTE E. and PANSU B. Eds., Intemational

Workshop

on

Geometry

and Interfaces, J.

Phys. Colloq.

France 51(1990) C7.

[8] SCRrVEN L. E., Nature 266 (1976) 123-125.

[9] MACKAY A. L., Nature 314 (1985) 604-606.

[10] MACKAY A. L.,

Physica

131B (1985) 300-305.

[I I] HYDE S. T. and ANDERSSON S., Z.

Kristallogr.

168 (1984) 221-254 and 170 (1985) 225-239.

[12] MACKAY A. and KLINOWSKI J.,

Computers

and Mathematics with

Applications,

12B (1986) 803- 824.

[13] SADOC J. F. and CHARVOLIN J., J.

Physique

France 47

(1986)

683-691.

[14] LIDIN S. and HYDE S. T., J.

Phys.

France 48 (1987) 1585-1590.

[15] FOGDEN A., in Ref. [7], p. 149-156.

[16] FOGDEN A., Ph. D. Thesis,

Department

of

Applied

Mathematics, ANU, Canberra

(1991).

[17] FOGDEN A. and HYDE S. T., Acta

Cryst.

A 48 (1992) 442-451 and A 48 (1992) 575-591.

[18] CVUOVIt D. and KLINOWSKI J., J.

Phys.

I France 2

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137-147.

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[20] CvIJovIt D. and KLINOWSKI J., J.

Phys.

I France 2 (1992) 2207-2220.

[21] CVIJOVIt D. and KLINOWSKI J. (in

preparation).

[23] DAVIS P. J. and RABINOWITz P., Methods of Numerical

Integration

(2nd Edition, Academic Press, New York, 1984).

[24] BYRD P. F. and FRIEDMAN M. D., Handbook of

Elliptic Integrals

for

Engineers

and Scientists (2nd Edition,

Springer-Verlag, Berlin-Heidelberg-New

York, 1971).

[25] MILNE-THOMPSON L. M., in M. Abramowitz and I. A.

Stegun

Eds., Handbook of Mathematical Functions (Dover Publications Inc., New York, ch. 17, 1980).

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(b) CARLSON B. C., Math.

Comput.

49 (1987) 595 and 51(1988) 267.

128] BULIRSCH R., Numer. Math. 7

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78-90 7 (1965) 353 13 (1969) 305 [29] (al PRESS W. H. and TEUKOLSKY S. A., Comput. Phys. (1990) 82-86

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Recepies

the Art of Scientific

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[30]

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Equations

in Several Variables

(Academic

Press, New York, 1970).

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