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membranes
W. Cai, T. Lubensky, P. Nelson, T. Powers
To cite this version:
W. Cai, T. Lubensky, P. Nelson, T. Powers. Measure factors, tension, and correlations of fluid membranes. Journal de Physique II, EDP Sciences, 1994, 4 (6), pp.931-949. �10.1051/jp2:1994175�.
�jpa-00248017�
Classification Physics Abstracts
87.10 II-Ii 68.15 87.20
Measure factors, tension, and correlations of fluid membranes
W.
Cai,
T-C-Lubensky,
P. Nelson and T. PowersPhysics Department, University of Pennsylvania, Philadelphia, PA 19104 U-S-A-
(Received
18 January1994, accepted 10 March1994)
Abstract We study two geometrical factors needed for the correct construction of statistical ensembles of surfaces. Such ensembles appear in the study of fluid bilayer membranes, though
our results are more generally applicable. The naive functional measure over height fluctuations must be corrected by these factors in order to give correct, self-consistent formulas for the free energy and correlation functions of the height. While one of these corrections the Faddeev,
Popov determinant has been studied extensively, our derivation proceeds from very simple geometrical ideas, which we hope removes some of its mystery. The other factor is similar to the Liouville correction in string theory. Since our formulas differ from those of previous authors,
we include some explicit calculations of the effective frame tension and two-point function to show that our version indeed secures coordinate-invariance and consistency to lowest nontrivial order in a temperature expansion.
1. Introduction and summary.
Amphiphilic
molecules in water tend to aggregate into thin flexiblebilayers,
which in turn forma wide
variety
ofnearly
two-dimensional structures with characteristic size of order microns[I].
The
study
of these structures may becomesignificant
forbiology; they
arecertainly
importanttechnologically
as theunderlying
elements of microemulsions and othercomplex
fluids.To understand the static and
dynamic properties
ofbilayer membranes,
and the transitions between differentmorphologjes,
we must first understand the role of thermal fluctuations intwo-dimensional
surfaces,
a subtleproblem
in statistical mechanics. Thermal fluctuations are important becauseregardless
how still a membrane maybe,
verylong-wavelength
undulations in itsshape
arealways allowed;
onlong enough length
scales any membrane will appear flexibleand will undulate
significantly,
aphenomenon
first observed in the cell walls of red blood cells in the 19th century[2](~).
(~) Strictly speaking we are here talking about "fluid membranes", those with no internal structure
or order within the surface. In this paper
we discuss only fluid membranes, but
our measure factors
can be used in more complicated situations too [3].
Since the
length
scales we wish tostudy
are muchlarger
than the size of the constituentmolecules,
we expect that a membrane will be characterizedby just
a few effective parameters,summarizing
the effects of thecomplicated
molecular forces.Indeed,
the famous Canham- Helfrich model [4] describes theequilibrium
statistical mechanics of membranes in terms ofjust
two parameters: a chemical
potential
for the addition of surfactantmolecules,
which we will call po, and abending
energycoefficient,
the stiffness ~o.(Another
parameter, the Gaussianstiffness Ku,
only
enters when we considertopology change.)
The bare coefficients po, ~o are notdirectly observable,
but from them we can derive some more relevantphenomenologjcal
parameters. We willmainly study
the "frame tension" T, which is the free energy per unit frame area of thefluctuating membrane,
and thetwo-point
correlation(h(u)h(0))
of theheight h(u)
of the membrane from its averageplane,
which we fixby fixing
theedges
of the membrane to lie on a square frame. Theleading
behavior of thistwo-point
function at small wavenumberdefines another
phenomenological
parameter, the "q~ coefficient" r via(hlq)hl-q))
=~~~
()~~~
,
(l.1)
where AB is the area of the
frame,
T is the temperature(we
set Boltzmann's constant kBequal
to
one),
and q is a wavenumber. Another reason to introduce r is that indynamics problems
we can still calculate correlation functions like
(I.I ),
while there is noanalog
of the free energy from which to compute T. Two of usstudy
thedynamical problem
in [5].in this paper we will
explore
the relation between the various coefficients po, ~o, T, and r.More
generally,
onlong length
scales theprecise
size of the constituent molecules is immaterial:we can get the same answers
using
molecules of size a with coefficients po, ~o or with rescaledmolecules of size
b~~a,
b < I, and effective coefficientspe~(b), ~e~(b).
The scaledependence
of ~e~ is well-known[6-11],
but various answers for pe~ have beengiven (for example,
see [8, 9,11-15]).
In part the differences reflectconvention,
but there is akey physics point
whichwe will address: to get correct answers we must define our functional measure
properly.
Two of us havealready
discussed such matters in [3], but here we will add a number ofpoints,
asfollows.
We first introduce the effective action
r[h]
of thefluctuating
membrane and recall the argument of [3] that its form is constrainedby
the coordinate invariance of theunderlying theory.
Inparticular
we show in section 2 that the coefficients r and T defined above must beequal.
We then set up a naive,uncorrected,
calculational scheme whichyields (consistent
withJ51)
~ ~° ~
/~ ~~(2
~°~~~°~~
~ ~°~~~
~~~
' ~~'~~
where A
=
27rla
and a is the linear size of the constituent molecules.Following
Morse and MiIner we have introduced the thermal deBroglie wavelength
I =
h/$4
,
(1.3)
where m is the mass of a surfactant molecule [16]. The same calculational scheme however
yields
a very different formula for r. In fact(1.2)
is our finalresult,
butclearly
we need towork a bit harder to understand r.
The first correction factor, the
"Faddeev-Popov" factor,
is well known. In [3] we gave aformula for this factor which differs from the one
given by
David [14]; here in section 3 wegive
a
simple geometrical
motivation followedby
a derivation of our formula which issimpler
than the one in [3]. Whileunimportant
in the calculation of T, this factor doesmodify
the naivecalculation of r
(and higher
correlation functionstoo), yielding
an rfp which stilldisagrees
With T.
Next in section 4, we argue that another correction factor is needed.
Physically
our mem-brane consists of constituent molecules each
occupying
a fixed area a2 inphysical 3,space.
As the surface bows outward away from its flatequilibrium configuration
its area increases and additional molecules must bebrought
in fromsolution, effectively increasing
the number ofdegrees
of freedom in the membraneproblem.
A statistical measure with variable number ofdegrees
offreedom, depending
on theconfiguration itself,
is rathercomplicated.
We wouldprefer
a measure with fixed number ofdegrees
offreedom,
as indeed we usedimplicitly
in the naive derivation of rFP. Sincechanging
the number ofdegrees
offreedom,
orequivalently
the ultraviolet
cutoff,
can becompensated by renormalizing
the bare energy, we expect that a countertenn correction will need to be added to the naive derivation.We fix this counterterm
by requiring consistency
between two differentMonge-gauge
cal- culations of the free energy(in
theAppendix
wegive
a differentstrategy).
In this way we discover that~ ~ ~~~ ~
d
~~Al
~~,~
' ~~'~~
where we introduced an anisotropic wavenumber cutoff
(Al, A2).
Infact, substituting
ourformulas for T and rFP into lA shows that
they
indeedobey (lA).
Therequired
countertermturns out to make a contribution
precisely changing
the q~ coefficient from rFP to r = T.The introduction of our second correction factor may seem like ad hoc
wish-fulfillment,
but in the
Appendix
wegive
some detailed calculationsshoring
how it and the Faddeev-Popov
factortogether
are crucial to obtain consistent answers; inparticular
we show that thespecific
coefficient of the countertermimplied by consistency
is theright
one to get r = T.Furthermore,
ananalogous
correction is well-known in thestring theory literature,
where it is called the "Liouville factor"[li,
18]. This factor sometimes appears in theprevious
membraneliterature
(e.g. [19]),
but one gets theimpression
that it mattersonly
in the low-stiffnessregime beyond
thepersistence length; again,
we will see that it is needed to get the correct correlation functions even in the morephysical
stiffregime.
Our correction differs in detail from the Liouville factor because the latter isappropriate
for conformal gauge, but in each case the motivation is the same. We will also argue that the usualinterpretation
of the Liouvillefactor as a Jacobian is
misleading; really
asargued
above it reflects renormalization.Again
our counterterm isimportant
because withoutit, ordinary diagrammatic perturbation theory gives
incorrect results due to thesubtlety
in the statistical measure discussed above.Finally
we conclude in section 5.2. General
arguments.
We will consider fluid
membranes,
those with no internal order or structure. Real membranesare
typically
fluid at temperatureshigh enough
todestroy in-plane
order, but in any case such order caneasily
beincorporated
into the argument below [3]. The constituents of a membrane have apreferred spacing,
with ahigh
energy cost for local deviations from thatdensity. Thus,
in this
regime
the free energy cost of a membraneconfiguration depends only
on itsshape.
As mentioned in the
Introduction,
we can thus capture thephysics
oflength
scales muchlonger
than the constituent molecule sizeby regarding
the surface as continuous andusing
the Canham-Helfrich free energy [4]7i=po /dS+) /dS(
+
~ (2.I)
1 2
Here dS is the element of surface area,
f
dS is the total area of thesurface,
andRi,
R2 are theprincipal
radii of curvature of the surface. The two coefficients po, ~o arerespectively
thearea cost and
bending rigidity.
The form of
(2.I)
isseverely
constrainedby
therequirement
that the free energydepend only
on the membrane's
shape,
and not on how one chooses to labelpoints
on the surface. While this property is manifest in(2.I),
to do calculations a moreexplicit
version of thisequation
proves necessary, in which we do choose coordinates u
=
(u~, u~)
to labelpoints R(u)
of the surface. Asusual,
we then get tangent vectors e~ =d~R
edR/du~
at u and a metric tensorg~b " ea eb at each
point.
The unit normal is then n=
(ei
xe2)/(ei
xe2(,
and the curvature tensor isKab
" nV~dbR,
where V~ is the covariant derivative associated to the metric g~b.Letting
g + det [g~b), [g~~) = [gab)~~,
andK]
%g~~Kab, equation (2.I)
becomes7i = po
/ d~u/j
+
) / d~u/j (K])~ (2.2)
If we
change
the coordinates from u~ to fi~=
fi~(u)
wejust
relabelpoints
in theplane.
Foran infinitesimal
change
fi~= u~ + e~
iv)
we get a newk(fi)
=
R(u) describing
the same surface:kin)
=
Rju) e~ju)ea(u) (2.3)
The
change
of R is atangential motion; conversely, tangential changes
of R are notphysical cllanges
to theshape
of the surface andought
not to be countedseparately
in the statisticalsum. We thus need to
supplement (2.2) by choosing
aprotocol
forassigning
asingle
coordinate system to eachshape,
and a procedure fordiscarding
every surfaceR(u)
notparameterized
in this way.Any
such choice is called a"gauge,fixing" procedure.
A
popular
class ofgauge-fixing procedures
are the so-called "normalgauges." Suppose
we have
arranged
thatconfigurations
very close to one reference surface will dominate the statistical sum(by stretching
the membrane across a fixedframe,
forinstance).
We chooseonce and for all a
parameterization
Itoiv)
for this reference surface and compute its unit normalno(u).
Then othernearby
surfaces can be written asR(u)
=Ruin)
+hju)noiu) j2.4)
where the
height
field h at anypoint
isuniquely
defined as the normal distance from thatpoint
to the reference surface. We thus describe each distinct surface once when we sum over all functionsh(u).
Of course thepoint
of this paper is that the correct definition of this sum is atricky
business, but let usproceed formally
to obtain somegeneral properties constraining
the correct
prescription;
Let us consider a membrane confined to span a square, flat frame of area
AB.
We suppose surfactant molecules canjoin
or leave the membrane with a fixed cost in free energy of po per added area(one
caneasily
pass to an ensemble with a fixed number of moleculesby
aLegendre transformation).
The full partition function of our systemZ(AB)
thendepends
on the base area, andimplicitly
on po, the stiffness ~oappearing
in(2.I)
the size a a 27rIA
of theconstituent
molecules,
and the temperature T.Since our frame is
flat,
theequilibrium (zero-temperature)
surface will be flat too, and so it is convenient to work inMonge
gauge, a normal gauge with RoIv)
the flat surfacespanned by
theframe,
with Cartesian coordinates u~running
from zero to/G.
In addition toZ(AB)
wewill find it convenient to introduce the "effective action"
r[h].
To definer[h]
we introduce aforcing
term into7i, 7ij
= 7if hj,
andadjust j
to ensure that(h(u))
is the desired functionh(~). Computing
thepartition
functionZ[AB, ii
=/[Dh]e~~/T~(i/T) f
hj '(2.5)
we then let
r[h]
+ -Tlog Z[AB, j]
+hj (2.6)
The frame tension is the free energy per area of the unforced
membrane,
so we haveT =
-) log Z(AB)
"
~ r[h
= o] «
r~°) (2.7)
B B
AB
Physically
there isnothing special
aboutMonge
gauge. Even if we agree to work inMonge
gauge there is
nothing special
about a reference surfaceIto(u) coinciding
with theplane
of theframe;
a tilted reference surface mustgive
the same free energy. All that matters is thephysical
area of the frame. Thus the terms ofr[h] involving
at most first derivatives ofh (higher
derivatives are insensitive totilting)
must enter in the combinationf
d~u/J,
wherejab " bab +
dahdbh
is the induced metric and g = det g~b as usual. In other
words,
rjhj
= T/ d2u
(1 +
)(oh)2
+ + ,(2.8)
where the first
ellipsis
involvesO(h~)
while the second involves more derivatives thanl's.
Wegave a more detailed argument for this conclusion in [3].
Whatever the
precise
form of the measure[Dh] appearing
in(2.5),
it does notdepend
onj,
and so the first moment.6)
nding
(h)j
=h,
we
&r
~i
&j(u')6z j
j(u')-
Differentiating again
andusing (h)j=o
" 0, we see thatjh(u)hju'))~=o
=
z-iT2
~~
/))~~,~
~
=
z-iT ~
~
(zh(u'))
&h(u')
&j(vi
~~~
&2r ~~ ~~'~~~
~
bi(Ul
o
~
bh(U')
o
bh(U)bh(U')
o
(~) This is
a formal trick to obtain correlations of height; we do not imagine j as coming from any physical force. Mathematically j = j12d~u is
a density on parameter space, so that 616
j(u)
is a scalar.For more details see [3].
Thus the inverse of the
two-point
function isjust
thequadratic
part of the effective action.We have
repeated
the above well-known argument to make a point: it in no waydepended
upon the niceties of the measure
[Dh]. Any
exoticgauge-fixing
orcutoff-stretching
factor whichwe may
eventually
fold into[Dh]
will not alter the aboveconclusion, though they
can and will affect the relation of thequadratic
part to the constant partr(°) Combining (2.ll)
with(2.8), (1.I)
at once shows that the q~ coefficient requals
the frame tension T.Let us make a first attempt at
calculating
r and T. If the temperature T is small we canexpand everything
around theequilibrium configuration
h = 0. The energy functional(2.2)
then becomes
ill]
7i = po
/ d~u (I
+
jfidh)~ ((dh)~)
+
i / d~u [(d~h)~ (dh)~(d~h)~ 2(d~h)d~hdbhd~dbh)
+O(h6)
~~ ~~~
2 2
In this formula d~
=
d/du~,
d~= b~~d~db is the flat
Laplacian,
and all indices are contracted with the Kroneckersymbol.
Thus allh-dependence
isexplicitly
in view in(2.12).
To calculateZ(AB)
we need aproposal
for[Dh].
Thesimplest
choice is to choose a mesh ofgrid
points(u~j)
on u space,spaced by
a, and let[Dh]~a;ve
=fl(dh(ujj)/1) (2.13)
iJ
We introduced the thermal
wavelength
I here to render the measureproperly dimensionless(3 ).
We will argue later that
[Dh]~a;ve
is wrong, but for now we take it as ourstarting point.
For low temperature we
approximate Z(AB)
ase~~°~B/~
times a Gaussianintegral.
Col-lecting
thequadratic
terms of(2.12)
andwriting f
d~u= a~
£~~
we findT
~
~~~~~~~ (p~q~
+oQ~)j
r(o)
~ -Tlog Z(AB)
"P°~B
~i
2~~Now the sum is over the
points
q ofreciprocal
space. The upper limit of this sum is related to the constituent size a; forexample,
if in(2.13)
we choose points on a squaregrid,
then ourBrillouin zone is a square of
length
27rla.
Thus we recover the announced formula(1.2).
Next we turn to the
two-point function,
which weprovisionally
define asjhju)h(0))na;ve
=Z~~ /jDhjna;vee~~/~hju)hj0) j2.14)
This time however the constant term of
(2.12) drops
out, thequadratic
termgives
theleading
contribution
(h(q)h(-q))o
=j~~~
~, and the
quartic
termsyield
the desired thermalPOQ + ~oQ
correction to
(hh)o
via Wick's theorem. To shorten theformulas,
in the rest of thisparagraph
(~) In [15] and [3] this scale was taken to be the molecule size a or a constant multiple of it. This is legitimate when we do not care about the bare chemical potential, for example when we just want
to dial ~o to zero physical tension. But ~0 does have physical meaning, and MiIner and Morse have argued that the factor in
(2.13)
is the correct choice [16].we will
drop
all factors ofAB,
or setAB
= I.Retaining only
those termscontributing
to r we get(~iU)~(°))na>ve
"i~(U)h(0))0
+
~4 / d~U'(h(U)dahlU')lolh10)dahlU')loldbh(U')0bhlU'))o
+ 8
/ d~U' ~(U)°ahiU'))01~i°)°bh(U'))0(°ahiU')°bh(U'))01
+
j
2/ d~U' (h(U)0ah(U'))0(h(0)bah(U'))0(b~hjU')b~h(U'))0
+
j
2/ d~U'(hjU)bahjU'))01hj0)bbhjU'))0i0a0bhjU')b~hjU'))0
,
or
into) hi -Q)ma>ve
=~~q4
~~q~
+ ~~q4
~~q~ / I ll))l~ill))l~
= T
P°Q~
~i~ /1 3
~~iq,iil'liq,~~
+°iQ~)l~
~~
T
/~
d~Q3
P°Q~(2.15)
~"~'~~ " ~°
§ @
~uq4 +poq2
Equation (2.15)
isessentially
the result of Meunier [13]. Itcertainly
does notequal (1.2), notwithstanding
our formalargument
that r = T.3.
Gauge fixing.
Apparently
our troubles stern from(2.13).
How should we sum over allconfigurations?
We will return in the next section to thequestion
of thespacing
ofgrid
points, but even with this choice madecorrectly, equation (2.13)
is not correct. Consider the two surfacesR,
R + dR infigure
I.
According
to(2.4),
we describe thedisplacement
from R to R + dRby
an incrementbh(u)
in
h(u).
But thisdisplacement
isonly partly physical,
I-e-,only partly
normal toR,
since it isalong no(u),
which is notequal
to the normaln(u)
atR(u),
The actual normaldisplacement
from R to R + dR issimply n(u)
no(u)dh(u)
[22], and we need toreplace [Dh]na;ve
in(2.13) by it
[hi[Dh]na;ve
whereLlhl
+fl(n(u,j) no(u,j)) (3.i)
,j
The Jacobian
it
[hi is the first correction factor(the "Faddeev-Popov
determinant" mentioned in the Introduction.Our derivation of
(3.I)
was heuristic. Nevertheless the result agrees with a more formal derivation which we will give in a moment, and the heuristic discussionfives it[h]
a verysimple geometric meaning.
The formula(3.I)
also agrees with theapproach
based on metricson field space [3]. For
example, taking Ito(u)
to beflat
we have n no=
g~~/~,
andit
is theR+dR
-, ' '
''
'~h
n '' ''
'
.,oooo,o2~o.o..
'
.,o..,
o o"'' ', '"..
, ,o.""" ". ~ ,." """". ',
, ."' °. ." ~ '~ /"°o, '
, ~o"' "o:.."' '".~ ,
'.°' '"°...~
h
no
R~
Fig. I. Two surfaces R, R + dR described in the normal gauge associated to Ro.
Monge
gauge factor found in [3]. It is not unity, contrary to reference [14]; while it does not affect theone-loop
renormalization of ~o, it will be crucial for r, as shown below and in [3].Our second derivation of
(3.I)
is couched inlanguage
familiar from gauge theories [20]. It ismore
precise
than the motivationjust given
for equation(3.I),
andagain reproduces
the answergiven
in [3]. We think that each derivation shedslight
on(and
increases our confidencein)
the final answer. In order to form a statistical sum over distinct surfaces weimagine integrating
over all
parameterized surfaces,
with a correction factor to eliminateovercounting. Thus,
wewrite the
partition
function asZ =
/[DR] lj) e~~/~ (3.2)
V°
Here
[DR] just
describes thepossible displacement
of the individualmass-points
on the surface andvol[R]
is a factor to be discussed below. All we will need to know for the moment is thatthe measure
[DR]
must becoordinate-invariant,
since nopreferred
coordinate system isgiven
on a fluid membrane;
[DR]
must also be invariant underspatial
translations and rotations.To finish
specifying (3.2)
we need tospecify
the extra volume factorvol[R] appearing
there.Starting
from any surfaceR(u)
andapplying
allpossible reparameterizations
we sweep out asubspace
of allparameterized
surfaces. The volumevol[R]
of this "orbit" may welldepend
on which surface we startwith,
but it cannotdepend
on howR(u)
isparameterized.
Since it proves inconvenient to include
vol[R] explicitly
in(3.2),
we now fix a coordinate choiceby introducing
two constraints onR(u)
at everypoint
u:ia(Rju))
= 0 a = 1,2
For
example,
in normal gauge werequire
falRlU))
+l~~ea,olU) (R(U) Ro(u))
= o
(3.3)
We have introduced a factor of l~~
(see 11.3))
to makef~
dimensionless.Any length
scale will do here since our answers will bealtogether independent
of our choice off~.
We now define theFaddeev-Popov
determinantAi[R]
viae
a~jRj l'jDkj &ji~jk)j j3.4)
The
integral
isonly
over the space ofk's
whichare
repararneterizations
ofR;
hence we also have,
vol[R]
=
[DR] (3.5)
To
keep vol[R],
and hence(3.2),
dimensionless we include two factors of l~~ at everypoint
in
(3.5).
Since everykin)
=
R(fl(u))
is related to Rby
a reparameterization, u~ -+fl~(u),
we can also write
f'[Dk]
as
f[Dfl]D[fl,R],
whereformally D[fl, R]
= detd(R(fl))/dfl
is a Jacobian factor related to thechange
of variables. Let us now insert(3A)
into(3.I)
to getZ
"
/lDRl ~~~~j e~~~~~~AflRl /lDflllllfl, RldlfalRlfl))I
Since a
reparameterization
fl hasmeaning independent
of the surface R weapply
it to, we cando the fl
integral
last.Letting k
=
R(fl),
we use the fact that[DR], 7i, vol[R]
andAi
arereparameterization
invariant to rewrite Z asZ =
/[Dfl] /[Dk] lfi) e~~l~l/~'Ai[k]d[f~(k)]D[fl, R]
vol[R]
Also,
the fact that[DR]
is coordinate-invariant means that smalldisplacements
of fl sweep outequal
volumes no matter where on-agiven
orbitthey
act, I-e-D[fl,R]
=
D[fl, R]. Renaming k
as R andusing (3.5)
we thus getZ =
/[DR]e~~l~l/~'Ai (Rid( f~(R)] (3.6)
The
only configurations entering (3.6)
are thoseobeying
the gaugecondition,
asdesired,
butnow we must compute
hi [R]
from the definition(3.4).
While
(3.6)
isquite general,
we will nowspecialize
to the normal gauge(2.4)
associated to asurface
Ito.
The functional delta-function in(3.6)
tells us we needonly
to examinehi [R]
for Robeying
thenormal-gauge condition;
the delta-function in(3.4)
then tells us we needonly study k infinitesimally
close to R. Thus we writek
in the form(2.3), kin)
=
R(u) e~(u)e~(u).
A reasonable
choice(~)
for[Dk]
near agiven
R is thenlDkl
%flld~klU,j)/>~) 13.7)
In
(3.7)
weimagine
that whatever coordinate system wechoose,
agrid
has been laid down with eachpoint carrying
constant mass. Since each constituent moleculeoccupies
a fixedphysical
area, we can
equivalently specify
that eachgrid
cell of size(Au~, Au~)
occupyequal
areas in 3-space.(This,
in turn,typically
means that the Au~ themselves are not all the same. With thisunderstanding [Dk]
is indeed coordinate-invariant-Submitting
R to an infinitesimal coordinate transformation u~ -+ u~ +e~(u),
we see that at each u,jR(u,j)
moves in the tangentplane;
the measured3k(uq)/13
in(3.7),
restricted to thisplane,
becomesl~~jei
x
e2(d~e(uq)
=
l~~fid~e(u,j) (3.8)
We can now evaluate
(3.4):
AflRl~~
"/fll>~~vld~flU~j))d~~~lfalRlUlj
+f~lUij))))
~
=
/ fl(l~~/jd~e(uq))det ~~[J~b(uq)]d(~)(e~(u~))
,
~
(~) The nonlinear measure correction to be discussed in the next section will not affect our answer;
see the Appendix.
where
J~b(u)
=
df~(R(u
+e))/de~
=
l~~e~,o
eb in normal gaugeusing (3.3).
Thushi [R]
=fl
~~~~~ ~~(3.9)
~~
To finish our
job
ofgetting
anexplicit
expression for thepartition function,
we now express[DR]d[f~(R)] appearing
in(3.6)
in terms of the nonredundantheight
variableh(u) appearing
in
(2.4).
We canconveniently
express anarbitrary
R in terms of aheight change plus
the rest:Rju)
=Roju)
+h(u)noiu)
+ea,oiu)v~ju) j3.10)
The calculation is not
quite
the same as the oneleading
to(3.8);
instead of infinitesimalreparameterizations
e~ from anarbitrary normal-gauge
surfaceR,
now we havedisplacements
from the
fixed
reference surface Ito.Accordingly,
instead of(3.8)
we findd~R(u)
=
fi$d~vdh (3.ll)
Next, (2A)
with(3.lo) gives f~(R)
=l~~e~,o.eb,ov~,
or with(3.lo) d(~)(f~(R))
= l~det~~(e~,o.
eb,o) d(~l(v~).
We can now do the v~integrals
to get from(3.6)
toZ =
/ lfl l~~dh(u~ iie~~/~'
,
(3.12)
iJ
Wlle~~
~
det(ea,o eb)
~
fl
~ ~~(u~~13.13)
~
i~
vlW
iJ
It is understood that 7i and
it
are evaluated on the surface
given
in terms ofh(u) by (2.4).
The last step follows because det
(e~,o eb)
"(ei,o
x e2,o(ei
xe2)
=/fino vln.
Note that each factor in(3.12)
isexplicitly coordinate-invariant,
in contrast with theanalogous
formula in[14j.
We see that
(3.13)
indeed does agree with our heuristic formula(3.I). Specializing
toMonge
gauge, no " I, we recover the result of [3],
it
= ~j~~~
g~l/2
An alternate form for
it
can be obtained
using
eb " dbR
= eb,o +
db(hno
" eb,o
he(Kbc,0
+ dbhno,
(3.14)
where Kbc,0 is the curvature tensor of the
background
surface. From this we find~
~~ ~~)
~(_ dahdah
+O(h ))
' ~~ ~~~
£
=
§
~~~~~~$
jf
~ ~~~~j
~
which
again
differsslightly
from the formula in [14]. We see thatgetting
the correct/j
factors in the denominator is crucial to avoid aspurious
term linear in h.Returning
to theunhappy ending
of section 3, we now see that theMonge-gauge
Faddeev-Popov
factorit
= exp
~j
~log(1
+(0h)~)
= exp
~j
~(dh)~
+(h~)1(3.16)
~
"
~ ~
"
~
effectively
contributes a new term to(2.12),
one which isalready
of order T.Following
the stepsleading
to(2.15),
we get the corrected version~~~ ~°
/~ ~~(2 ~ oo~i~ioo~
~~ ~~~On the other hand
it
cannot contribute toour calculation of T since
being already
of order Twe
simply
evaluate it at h= o, where it
equals
one. We still have theproblem
that rFP#
T.4. Nonlinear measure.
To see where we have erred, let us first
give
another derivation that r= r. Note that there
are many different
Monge
gaugescorresponding
toprojections
to various referenceplanes (~).
So far we have used a reference
plane coinciding
with theplane
of the frameholding
themembrane,
so theequilibrium configuration
is h= o, but we could instead choose
It~
tiltedby
a small
angle
~b. We willalways
work to lowest nontrivial order in ~b. In the new coordinate system the sameequilibrium
surface is now describedby h'iv)
= ~bu~
(Fig. 2);
furthermore theprojected
area has been foreshortened in onedirection, giving A)
= AB cos ~b =
AB(I
~~b~).2 Since the two calculations compute the same
quantity
we must have thatrjA~;
h= oj a TA~
"
~[~B ji~~~Bl h'(U)
" i~U~)(4.1)
~~~
~ ~~~~
~~ ~~~~
In the last step we wrote the
O(h'~)
term of r in terms ofr(0h')~
= r~b~. Thus we
again
concluder = T, contrary to our still
incomplete
calculation.v ~
A'~
Fig. 2. Tilting the reference surface foreshortens both the base
area and the coordinate cutoff.
What have we done
wrong? Throughout
our discussion of theprevious
section we assumedthat the measure
[DR],
and its reduction[Dh],
were invariant underchanges
of parameteriza-tion of the surface. But the choice made in
(2.13)
does not have this property. We chose the(~) Recall that a Monge gauge is a normal gauge where the reference surface Ro in figure I is flat.
Alternatively we could imagine two different physical surfaces related by a rotation, both viewed in the same Monge gauge.
grid points (u~ ) evenly spaced
in the coordinates u~, which has differentmeaning
for different coordinate systems. Inparticular
for our seconddescription
we have a total ofA[ la~ degrees
of
freedom,
which is different from the true numberABla~
of masspoints!
Moreformally, equation (3.7)
tells us to usegrid
cells of constant metric area Au~Au~=
a~llj,
while(2.13) specifies
constant coordinate area Au~Au~= a~. We can
easily
show that this error accounts for theremaining discrepancy
between T and rFP,equations (1.2)
and(3.17).
Let us denote
by
rfp [AB, A~, A~;hi
the effective action calculated with the correct Faddeev-Popov
factorit
but stillusing
the naive(coordinate-dependent)
measure(2.13).
We momentar-ily
allow ananisotropic
cutoff(A~, A~),
which we writeexplicitly;
at the end of the discussionwe will set A~
= A~
=
27rla.
Theforegoing
discussionimplies
that we may use rFP if we remember to foreshorten the spacing of constituents(increase
Al as well as the baseplane (Fig. 2),
so(4.I)
becomesrfp
[AB, ~~, ~~,
h=
0j
=TAB
~ ~
~ ~
(4.2)
= rfp
[AB -ifi~AB, (I
+-il~)~, ~; h'(u)
=
ilu~j
or
since rFP is the q~ coefficient we calculated with the naive measure. Thus we find
~ ~~~ ~
l~)A~
' ~~'~~
which
really
isobeyed by
our calculatedexpressions (1.2, 3.17).
We have thus identified the
problem:
the naive measurespreads
masspoints evenly
in coordinate space, not in real space. For flatequilibrium
surfaces(h
linear inu~),
theright prescription
was easy to find: wekeep
thegrid points
uniform butchange
theirdensity
toget the RHS of
(4.2). Clearly
for nonflath(u)
we will have to be moreclever,
since here the cutoff is nonuniform and indeedfield-dependent:
the desired measure[Dh]
is nonlinear in h.Incidentally,
the sameproblem
we face here arisesagain
in thedynamics
context [5], where anaive calculation
fives
thetwo-point
function controlledby
our rFP.We hinted at the answer in the Introduction: a
change
in thecutoff,
even aspatially-varying cllange,
amounts to a localchange
in the number ofdegrees
of freedom. We canimagine passing
from the desired nonlinear
[Dh]
to the convenient[Dh]na;ve by
a sort of decimationprocedure,
where weintegrate e~~/~
over the
discrepant degrees
of freedom to obtaine~~eff/~
Thedifference d7i
= 7ie~ 7i is
simply
a counterterm; while ingeneral
it is a nonlocal functional ofh,
still when we asklong-scale
questions it may bereplaced by
a renormalizable truncation,just
as we did for 7i itself.We therefore seek a correction factor d7i with the property that
"
[Dh]
=e~~~l~l/~[Dh]na;ve
"(4.5)
This
equation
is in quotes because as it stands it makes no sense: we cannot equate twomeasures with different numbers of