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Shear Viscosity

Shear viscosity is the cleanest transport coefficient in AdS/CFT. It measures how efficiently transverse momentum gradients are damped. In a strongly coupled plasma with an Einstein-gravity dual, it is computed by a transverse graviton falling into the black-brane horizon.

The famous result is

ηs=14π\boxed{ \frac{\eta}{s}=\frac{1}{4\pi} }

in units =kB=1\hbar=k_B=1.

This page derives the result in the form most useful for AdS/CFT calculations. The derivation also explains why the number is universal in two-derivative Einstein gravity and why it is not a theorem about all quantum field theories.

The logic is:

metric source hxy(0)GRTxyTxyηηs=14π.\text{metric source }h^{(0)}_{xy} \quad\longrightarrow\quad G_R^{T^{xy}T^{xy}} \quad\longrightarrow\quad \eta \quad\longrightarrow\quad \frac{\eta}{s}=\frac{1}{4\pi}.

In a relativistic QFT, the stress tensor responds to a small metric perturbation. Turn on an off-diagonal boundary metric source

g(0)xy(t)=hxy(0)(t).g_{(0)xy}(t)=h^{(0)}_{xy}(t).

The corresponding operator is TxyT^{xy}. Linear response gives

δTxy(ω)=12GRxy,xy(ω,0)hxy(0)(ω),\delta\langle T^{xy}(\omega)\rangle = -\frac12 G_R^{xy,xy}(\omega,\mathbf{0})h^{(0)}_{xy}(\omega),

up to sign conventions for how the source is inserted. The retarded correlator is

GRxy,xy(t,x)=iθ(t)[Txy(t,x),Txy(0,0)].G_R^{xy,xy}(t,\mathbf{x}) = -i\theta(t)\langle[T^{xy}(t,\mathbf{x}),T^{xy}(0,\mathbf{0})]\rangle .

For an isotropic fluid, the shear viscosity is determined by the low-frequency spectral weight:

η=limω01ωImGRxy,xy(ω,0).\boxed{ \eta = -\lim_{\omega\to0} \frac{1}{\omega} \operatorname{Im}G_R^{xy,xy}(\omega,\mathbf{0}) . }

This is the shear Kubo formula. The real part of GRG_R contains contact and scheme-dependent terms. The transport coefficient is obtained from the dissipative imaginary part.

Use the planar AdSd+1_{d+1} black brane

ds2=L2z2[f(z)dt2+dx2+dz2f(z)],f(z)=1(zzh)d,ds^2 = \frac{L^2}{z^2} \left[ -f(z)dt^2+d\mathbf{x}^2+\frac{dz^2}{f(z)} \right], \qquad f(z)=1-\left(\frac{z}{z_h}\right)^d,

with

T=d4πzh.T=\frac{d}{4\pi z_h}.

Consider a transverse traceless metric perturbation at zero spatial momentum:

gxygxy+δgxy,δg yx(t,z)=ϕ(z)eiωt.g_{xy}\to g_{xy}+\delta g_{xy}, \qquad \delta g^x_{\ y}(t,z)=\phi(z)e^{-i\omega t}.

The boundary value ϕ(0)\phi_{(0)} sources TxyT^{xy}:

ϕ(z0)=ϕ(0)+.\phi(z\to0)=\phi_{(0)}+\cdots .

For two-derivative Einstein gravity, this transverse graviton obeys the same radial equation as a minimally coupled massless scalar:

1gz(ggzzzϕ)+gttω2ϕ=0.\frac{1}{\sqrt{-g}}\partial_z \left(\sqrt{-g}g^{zz}\partial_z\phi\right) + g^{tt}\omega^2\phi=0 .

This simplification is the heart of the universality argument.

Shear viscosity from the transverse graviton

The shear viscosity computation. The boundary metric source hxy(0)h^{(0)}_{xy} launches a transverse graviton ϕ=h yx\phi=h^x_{\ y} into the black-brane geometry. Infalling horizon behavior selects the retarded correlator. In the low-frequency limit, the dissipative flux is fixed by the horizon area density, giving η=s/(4π)\eta=s/(4\pi) for two-derivative Einstein gravity.

The quadratic action and canonical momentum

Section titled “The quadratic action and canonical momentum”

Expand the Einstein-Hilbert action to quadratic order in the transverse graviton. For the shear mode, the relevant part can be written as

S(2)=132πGd+1dd+1xggMNMϕNϕ+boundary terms.S^{(2)} = -\frac{1}{32\pi G_{d+1}} \int d^{d+1}x\sqrt{-g}\, g^{MN}\partial_M\phi\partial_N\phi + \text{boundary terms}.

The radial canonical momentum is therefore

Π(z,ω)=116πGd+1ggzzzϕ(z,ω),\Pi(z,\omega) = -\frac{1}{16\pi G_{d+1}} \sqrt{-g}\,g^{zz}\partial_z\phi(z,\omega),

where the precise factor follows from varying the quadratic action and using the standard normalization of h yxh^x_{\ y}. After adding counterterms, the retarded correlator is schematically

GRxy,xy(ω,0)=limz0Πren(z,ω)ϕ(z,ω).G_R^{xy,xy}(\omega,\mathbf{0}) = \lim_{z\to0}\frac{\Pi_{\rm ren}(z,\omega)}{\phi(z, \omega)} .

For the viscosity, only the term linear in iωi\omega matters. Local counterterms are analytic and real at this order for the zero-momentum shear channel, so they do not change η\eta.

Near the horizon,

f(z)4πT(zhz),f(z)\simeq 4\pi T(z_h-z),

and the scalar equation has two local behaviors:

ϕ(z)(1zzh)iω/(4πT)or(1zzh)+iω/(4πT).\phi(z) \sim \left(1-\frac{z}{z_h}\right)^{-i\omega/(4\pi T)} \quad\text{or}\quad \left(1-\frac{z}{z_h}\right)^{+i\omega/(4\pi T)}.

The retarded Green function uses the infalling branch:

ϕin(z)(1zzh)iω/(4πT).\phi_{\rm in}(z) \sim \left(1-\frac{z}{z_h}\right)^{-i\omega/(4\pi T)}.

Expanding at small ω\omega,

zϕiniω4πT1zhzϕin.\partial_z\phi_{\rm in} \simeq \frac{i\omega}{4\pi T}\frac{1}{z_h-z}\phi_{\rm in}.

Because gzzf(z)g^{zz}\propto f(z) vanishes linearly at the horizon, the product gzzzϕg^{zz}\partial_z\phi has a finite limit. This is the cancellation that makes the horizon calculation simple.

Evaluating the low-frequency response at the horizon

Section titled “Evaluating the low-frequency response at the horizon”

At low frequency and zero spatial momentum, the ratio

Π(z,ω)iωϕ(z,ω)\frac{\Pi(z,\omega)}{i\omega\phi(z,\omega)}

is radially conserved at leading order in ω\omega. Therefore it may be evaluated at the horizon instead of at the boundary.

Using the infalling solution, one finds

Π(zh,ω)=iω116πGd+1(Lzh)d1ϕ(zh,ω)+O(ω2).\Pi(z_h,\omega) = -i\omega\frac{1}{16\pi G_{d+1}} \left(\frac{L}{z_h}\right)^{d-1} \phi(z_h, \omega) + O(\omega^2).

Since the zero-frequency solution is constant in zz,

ϕ(zh,ω)=ϕ(0)(ω)+O(ω).\phi(z_h,\omega)=\phi_{(0)}(\omega)+O(\omega).

Thus

GRxy,xy(ω,0)=iω116πGd+1(Lzh)d1+O(ω2)+real contact terms.G_R^{xy,xy}(\omega,\mathbf{0}) = -i\omega \frac{1}{16\pi G_{d+1}} \left(\frac{L}{z_h}\right)^{d-1} + O(\omega^2) + \text{real contact terms}.

The Kubo formula gives

η=116πGd+1(Lzh)d1.\boxed{ \eta = \frac{1}{16\pi G_{d+1}} \left(\frac{L}{z_h}\right)^{d-1}. }

The Bekenstein–Hawking entropy density of the planar horizon is

s=14Gd+1(Lzh)d1.s = \frac{1}{4G_{d+1}} \left(\frac{L}{z_h}\right)^{d-1}.

Comparing this with the viscosity gives

η=s4π.\eta = \frac{s}{4\pi}.

Therefore

ηs=14π.\boxed{ \frac{\eta}{s}=\frac{1}{4\pi}.}

This is independent of zhz_h, TT, and the number of degrees of freedom. Those quantities appear in both η\eta and ss and cancel in the ratio.

For N=4\mathcal N=4 SYM at large NN and large λ\lambda,

s=π22N2T3,η=π8N2T3,s=\frac{\pi^2}{2}N^2T^3, \qquad \eta=\frac{\pi}{8}N^2T^3,

so again

ηs=14π.\frac{\eta}{s}=\frac{1}{4\pi}.

The previous page derived the shear diffusion pole

ω=iDηk2+O(k4),Dη=ηϵ+p.\omega=-iD_\eta k^2+ O(k^4), \qquad D_\eta=\frac{\eta}{\epsilon+p}.

At zero chemical potential,

ϵ+p=sT.\epsilon+p=sT.

Using η/s=1/(4π)\eta/s=1/(4\pi) gives

Dη=14πT.\boxed{ D_\eta=\frac{1}{4\pi T}. }

The same number can be obtained from the lowest shear-channel quasinormal mode. Thus the Kubo computation and the hydrodynamic-pole computation agree.

Why the result is universal in Einstein gravity

Section titled “Why the result is universal in Einstein gravity”

The universality follows from three ingredients.

First, h yxh^x_{\ y} is a transverse graviton mode. In an isotropic two-derivative Einstein background, it behaves like a minimally coupled scalar at zero momentum.

Second, the low-frequency response is controlled by the future horizon. The horizon is where dissipation enters.

Third, both η\eta and ss are determined by the same horizon area density:

ηhorizon area density16πGd+1,s=horizon area density4Gd+1.\eta \sim \frac{\text{horizon area density}}{16\pi G_{d+1}}, \qquad s = \frac{\text{horizon area density}}{4G_{d+1}}.

The ratio is therefore fixed:

ηs=14π.\frac{\eta}{s}=\frac{1}{4\pi}.

This is sometimes called the membrane-paradigm explanation of the result.

The value 1/(4π)1/(4\pi) is not an exact law of nature. It is a robust result for a class of holographic theories whose low-energy bulk dynamics is governed by two-derivative Einstein gravity.

Corrections can come from several sources.

In AdS5_5/CFT4_4, finite ‘t Hooft coupling produces higher-derivative terms in the type IIB effective action. The leading correction behaves schematically as

ηs=14π[1+O(λ3/2)].\frac{\eta}{s} = \frac{1}{4\pi} \left[ 1+O(\lambda^{-3/2}) \right].

For maximally supersymmetric Yang–Mills theory, the leading correction is positive in the standard normalization.

Finite NN produces bulk loop corrections. These are suppressed by powers of 1/N1/N in theories with a weakly coupled bulk dual.

If the bulk action contains curvature-squared or higher-curvature terms not removable by field redefinitions, the transverse graviton can acquire an effective coupling different from the Einstein value. Then

ηarea density16πGd+1,\eta \neq \frac{\text{area density}}{16\pi G_{d+1}},

and η/s\eta/s can differ from 1/(4π)1/(4\pi).

In Gauss–Bonnet gravity, for example, one obtains a shifted value of the schematic form

ηs=14π(14λGB)\frac{\eta}{s} = \frac{1}{4\pi}(1-4\lambda_{\rm GB})

with conventions in which λGB\lambda_{\rm GB} is the Gauss–Bonnet coupling. Consistency constraints such as causality and positivity restrict the allowed range of such couplings, but the original universal value is no longer automatic.

If translations are broken, momentum is no longer conserved and the shear channel need not contain an ordinary diffusion pole. If rotational symmetry is broken, different shear components can have different viscosities.

The lesson is: η/s=1/(4π)\eta/s=1/(4\pi) is universal for a clean universality class, not for every holographic model one can write down.

A small shear perturbation changes the boundary geometry by stretching one spatial direction into another. In the bulk, this is a transverse graviton.

The imaginary part of the retarded correlator measures absorption. At small frequency, the absorption of the transverse graviton by the horizon is governed by the horizon area. Since the same area computes entropy, viscosity and entropy are locked together.

This is why the result is so elegant:

dissipationhorizon absorption,\text{dissipation} \quad\leftrightarrow\quad \text{horizon absorption},

and

entropyhorizon area.\text{entropy} \quad\leftrightarrow\quad \text{horizon area}.

In Einstein gravity, both are controlled by the same geometric object.

Boundary quantityBulk computation
metric source hxy(0)h^{(0)}_{xy}boundary value of transverse graviton h yxh^x_{\ y}
GRxy,xyG_R^{xy,xy}response/source ratio for infalling graviton
shear viscosity η\etalow-frequency absorptive part of graviton correlator
entropy density sshorizon area density divided by 4Gd+14G_{d+1}
η/s=1/(4π)\eta/s=1/(4\pi)universality of two-derivative Einstein graviton coupling
corrections to η/s\eta/shigher-derivative, stringy, quantum, anisotropic, or translation-breaking effects

“Small viscosity means no interactions.”

Section titled ““Small viscosity means no interactions.””

No. In weakly coupled kinetic theory, viscosity is often large because quasiparticles travel far before exchanging momentum. Strongly coupled holographic plasmas have no long-lived quasiparticles and can have very small η/s\eta/s.

“The Kubo formula uses Euclidean correlators.”

Section titled ““The Kubo formula uses Euclidean correlators.””

The viscosity is defined by a retarded correlator. Euclidean correlators can sometimes be analytically continued, but the holographic calculation must impose the Lorentzian infalling condition to obtain the retarded answer.

“The ratio 1/(4π)1/(4\pi) is a proven lower bound.”

Section titled ““The ratio 1/(4π)1/(4\pi)1/(4π) is a proven lower bound.””

It was historically conjectured as a bound for a broad class of systems, but higher-derivative holographic models show that the value can be modified. A safer statement is that 1/(4π)1/(4\pi) is the universal answer for isotropic two-derivative Einstein gravity duals.

“The calculation only works for N=4\mathcal N=4 SYM.”

Section titled ““The calculation only works for N=4\mathcal N=4N=4 SYM.””

The original explicit computation was done in the canonical D3-brane example, but the universality argument applies much more broadly to theories whose relevant bulk shear mode is governed by two-derivative Einstein gravity.

Local counterterms can change analytic real contact terms in GRG_R. The shear viscosity depends on the coefficient of iω-i\omega in the retarded correlator at zero momentum, which is fixed by horizon absorption in the Einstein-gravity calculation.

Exercise 1: Extract η\eta from a retarded correlator

Section titled “Exercise 1: Extract η\etaη from a retarded correlator”

Suppose the small-frequency retarded correlator in the shear channel is

GRxy,xy(ω,0)=PiωA+O(ω2),G_R^{xy,xy}(\omega,\mathbf{0}) = P-i\omega A+O(\omega^2),

where PP and AA are real constants. Use the Kubo formula to find η\eta.

Solution

The Kubo formula is

η=limω01ωImGRxy,xy(ω,0).\eta = -\lim_{\omega\to0}\frac{1}{\omega}\operatorname{Im}G_R^{xy,xy}(\omega,\mathbf{0}).

The imaginary part is

ImGRxy,xy=ωA+O(ω2).\operatorname{Im}G_R^{xy,xy}=-\omega A+O(\omega^2).

Therefore

η=limω0ωAω=A.\eta = -\lim_{\omega\to0}\frac{-\omega A}{\omega}=A.

The real contact term PP does not affect the viscosity.

Exercise 2: Derive η/s\eta/s from horizon area density

Section titled “Exercise 2: Derive η/s\eta/sη/s from horizon area density”

Assume that a two-derivative Einstein-gravity black brane gives

η=ah16πGd+1,s=ah4Gd+1,\eta=\frac{a_h}{16\pi G_{d+1}}, \qquad s=\frac{a_h}{4G_{d+1}},

where aha_h is the horizon area density. Show that η/s=1/(4π)\eta/s=1/(4\pi).

Solution

Divide the two expressions:

ηs=ah/(16πGd+1)ah/(4Gd+1).\frac{\eta}{s} = \frac{a_h/(16\pi G_{d+1})}{a_h/(4G_{d+1})}.

The area density and Newton constant cancel:

ηs=416π=14π.\frac{\eta}{s} = \frac{4}{16\pi} = \frac{1}{4\pi}.

Exercise 3: Check the N=4\mathcal N=4 SYM numbers

Section titled “Exercise 3: Check the N=4\mathcal N=4N=4 SYM numbers”

Using

s=π22N2T3,ηs=14π,s=\frac{\pi^2}{2}N^2T^3, \qquad \frac{\eta}{s}=\frac{1}{4\pi},

compute η\eta.

Solution

Multiply the entropy density by 1/(4π)1/(4\pi):

η=s4π=14ππ22N2T3.\eta = \frac{s}{4\pi} = \frac{1}{4\pi}\frac{\pi^2}{2}N^2T^3.

Therefore

η=π8N2T3.\eta = \frac{\pi}{8}N^2T^3.

Show that the shear diffusion constant of a zero-density holographic conformal plasma is

Dη=14πTD_\eta=\frac{1}{4\pi T}

if η/s=1/(4π)\eta/s=1/(4\pi).

Solution

The shear diffusion constant is

Dη=ηϵ+p.D_\eta=\frac{\eta}{\epsilon+p}.

At zero chemical potential,

ϵ+p=sT.\epsilon+p=sT.

Thus

Dη=ηsT=1Tηs=14πT.D_\eta=\frac{\eta}{sT} =\frac{1}{T}\frac{\eta}{s} =\frac{1}{4\pi T}.

Exercise 5: Why can higher-derivative terms change η/s\eta/s?

Section titled “Exercise 5: Why can higher-derivative terms change η/s\eta/sη/s?”

Explain qualitatively why a higher-curvature term in the bulk action can modify the shear-viscosity ratio.

Solution

In two-derivative Einstein gravity, the transverse graviton has a universal kinetic coupling fixed by Newton’s constant. The same Newton constant controls the Bekenstein–Hawking entropy, so η\eta and ss are tied to the same horizon area density.

Higher-curvature terms can change the effective kinetic coupling of the transverse graviton. They can also change the entropy formula from the simple area law to the Wald entropy. Since the two quantities need not be modified in the same way, the ratio η/s\eta/s can differ from 1/(4π)1/(4\pi).