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Epsilon Expansion and One-Loop Scaling

The previous page found the upper critical dimension of the Ising universality class. In the continuum scalar theory

S[ϕ]=∫dDx [12(∂ϕ)2+12rϕ2+λ4!ϕ4+⋯ ],S[\phi] = \int d^D x\, \left[ {1\over2}(\partial\phi)^2 +{1\over2}r\phi^2 +{\lambda\over4!}\phi^4 +\cdots \right],

the quartic coupling has engineering dimension

[λ]=4−D.[\lambda]=4-D.

For D>4D>4, the quartic perturbation is irrelevant at the Gaussian fixed point, and mean-field theory is asymptotically correct. For D<4D<4, it is relevant, so the Gaussian fixed point cannot describe the true long-distance critical theory. The borderline case D=4D=4 is special: the coupling is classically marginal, and loop integrals generate logarithms.

The epsilon expansion turns this borderline into a controlled calculation. Write

D=4−ϵ,0<ϵ≪1.D=4-\epsilon, \qquad 0<\epsilon\ll1.

Then the quartic coupling is weakly relevant. Classical scaling makes it grow at long distances, but one-loop fluctuations reduce it. The two effects balance at an interacting infrared fixed point, the Wilson–Fisher fixed point. Since the fixed-point coupling is proportional to ϵ\epsilon, perturbation theory becomes an expansion around an interacting, non-Gaussian theory.

Required background. Critical propagators and the upper critical dimension supplies the continuum propagator, self-energy power counting, and the identification Dc=4D_c=4 for ϕ4\phi^4 theory.

Helpful background. Hubbard–Stratonovich fields and the continuum limit explains how the Ising order parameter becomes a scalar field and why its mass is a temperature-like coupling.

The one-loop correction to the quartic vertex contains the massless bubble integral, evaluated at nonzero Euclidean external momentum pp,

BD(p)=∫q1q2(q+p)2,∫q≡∫dDq(2π)D,B_D(p)=\int_q {1\over q^2(q+p)^2}, \qquad \int_q\equiv\int {d^Dq\over(2\pi)^D},

where pp is a characteristic external momentum. By power counting,

BD(p)∼pD−4.B_D(p)\sim p^{D-4}.

Equivalently, with a UV cutoff Λ\Lambda, the ultraviolet part behaves as

BD(p)∼∫Λdq qD−1q4=∫Λdq qD−5.B_D(p)\sim \int^{\Lambda}dq\,{q^{D-1}\over q^4} =\int^{\Lambda}dq\,q^{D-5}.

Thus D=4D=4 is logarithmic:

B4(p)∼K4log⁡Λp+finite,K4=18π2B_4(p)\sim K_4\log{\Lambda\over p}+\text{finite}, \qquad K_4={1\over8\pi^2}

for a spherical momentum shell. The finite part depends on the scheme and on the external momentum configuration. The logarithm does not. It is the signal that a coupling measured at one scale differs from the coupling measured at another scale.

For the interaction λϕ4/4!\lambda\phi^4/4!, the local one-loop correction to the four-point vertex is

δλloop=−32λ2∫shelldDq(2π)D1(q2+r)2+higher-derivative terms.\delta\lambda_{\rm loop} =-{3\over2}\lambda^2 \int_{\rm shell}{d^Dq\over(2\pi)^D}{1\over(q^2+r)^2}+\text{higher-derivative terms}.

The factor 33 counts the ss, tt, and uu channels. The factor 1/21/2 is the bubble symmetry factor in this normalization. At criticality and in four dimensions,

δλloop=−3λ216π2dℓ.\delta\lambda_{\rm loop} =-{3\lambda^2\over16\pi^2}d\ell.

Tree-level quartic vertex and one-loop bubble correction

The one-loop correction to the four-point vertex is the bubble diagram in the three channels. Its logarithm at D=4D=4 becomes the beta function near D=4−ϵD=4-\epsilon.

The same logarithm appears in dimensional regularization as a pole. Introduce a reference scale μ\mu and define

BD(p;μ)=μ4−D∫dDq(2π)D1q2(q+p)2,B_D(p;\mu) =\mu^{4-D}\int {d^Dq\over(2\pi)^D}{1\over q^2(q+p)^2},

so that the regulated integral is dimensionless, as it is at D=4D=4. A standard Feynman-parameter evaluation gives

BD(p;μ)=μ4−D1(4π)D/2Γ(2−D/2)Γ(D/2−1)2Γ(D−2)(p2)D/2−2.B_D(p;\mu) = \mu^{4-D} {1\over(4\pi)^{D/2}} {\Gamma(2-D/2)\Gamma(D/2-1)^2\over\Gamma(D-2)} (p^2)^{D/2-2}.

Near D=4−ϵD=4-\epsilon,

B4−ϵ(p;μ)=116π2[2ϵ−log⁡p2μ2+scheme-dependent constant+O(ϵ)].B_{4-\epsilon}(p;\mu) = {1\over16\pi^2} \left[ {2\over\epsilon}-\log {p^2\over\mu^2} +\text{scheme-dependent constant}+O(\epsilon) \right].

The pole and the logarithm are two representations of the same marginal short-distance sensitivity.

The Wilsonian RG makes the logarithm into a differential equation. Split the field into slow and fast Fourier modes,

ϕ(x)=ϕ<(x)+ϕ>(x),\phi(x)=\phi_<(x)+\phi_>(x),

where

∣q∣<Λ/bfor ϕ<,Λ/b<∣q∣<Λfor ϕ>,|q|<\Lambda/b \quad\text{for }\phi_<, \qquad \Lambda/b<|q|<\Lambda \quad\text{for }\phi_>,

with b=edℓb=e^{d\ell}. Define the slow-field effective action by

e−Seff[ϕ<]=∫Dϕ> e−S[ϕ<+ϕ>].e^{-S_{\rm eff}[\phi_<]} = \int D\phi_>\,e^{-S[\phi_<+\phi_>]}.

After integrating over the thin shell, rescale momenta, coordinates, and fields to restore the cutoff:

q′=bq,x′=x/b,ϕ′(x′)=b(D−2)/2ϕ<(x).q'=bq, \qquad x'=x/b, \qquad \phi'(x')=b^{(D-2)/2}\phi_<(x).

The field rescaling keeps the Gaussian kinetic term normalized.

Momentum shell integration and rescaling in Wilsonian RG

A Wilsonian step integrates out fast modes in the shell Λ/b<∣q∣<Λ\Lambda/b<|q|<\Lambda, then rescales lengths and fields to restore the cutoff. Repeating this operation turns couplings into functions of the observation scale.

For the shell calculation, introduce the cutoff-scaled coupling

λˉ=λΛ−ϵ.\bar\lambda=\lambda\Lambda^{-\epsilon}.

Its classical flow follows from [λ]=ϵ[\lambda]=\epsilon:

λˉ↦bϵλˉ,dλˉdℓ∣tree=ϵλˉ.\bar\lambda\mapsto b^\epsilon\bar\lambda, \qquad \left.{d\bar\lambda\over d\ell}\right|_{\rm tree} =\epsilon\bar\lambda.

The loop correction at criticality uses

∫shelldDq(2π)D1q4=KD∫Λ/bΛdq qD−5,\int_{\rm shell}{d^Dq\over(2\pi)^D}{1\over q^4} =K_D\int_{\Lambda/b}^{\Lambda}dq\,q^{D-5},

where

KD=SD−1(2π)D,SD−1=2πD/2Γ(D/2).K_D={S_{D-1}\over(2\pi)^D}, \qquad S_{D-1}={2\pi^{D/2}\over\Gamma(D/2)}.

In D=4−ϵD=4-\epsilon, the shell integral is

KDΛ−ϵdℓ+O(dℓ2).K_D\Lambda^{-\epsilon}d\ell+O(d\ell^2).

Therefore, near four dimensions,

dλˉdℓ=ϵλˉ−3λˉ216π2+O(λˉ3,ϵλˉ2),{d\bar\lambda\over d\ell} = \epsilon\bar\lambda -{3\bar\lambda^2\over16\pi^2} +O(\bar\lambda^3,\epsilon\bar\lambda^2),

where KDK_D has been expanded about K4=1/(8π2)K_4=1/(8\pi^2). In terms of

g=3λˉ16π2,g={3\bar\lambda\over16\pi^2},

the sharp-shell flow before expanding the angular factor is

dgdℓ=ϵg−KDK4g2+O(g3).{dg\over d\ell}=\epsilon g-{K_D\over K_4}g^2+O(g^3).

Since KD/K4=1+O(ϵ)K_D/K_4=1+O(\epsilon), its leading form is

dgdℓ=ϵg−g2+O(g3,ϵg2).\boxed{ {dg\over d\ell}=\epsilon g-g^2+O(g^3,\epsilon g^2). }

Near the interacting fixed point, g=O(ϵ)g=O(\epsilon), so both omitted terms are of order ϵ3\epsilon^3. This accuracy determines the leading fixed point and exponents. The balance between weak relevance and a quadratic loop correction is the mechanism in Wilson and Fisher 1972, p. 241, Eqs. (8)–(12), PDF; their block-spin coupling has a different normalization from gg.

The fixed points of

βR(g)=dgdℓ=ϵg−g2\beta_R(g)={dg\over d\ell}=\epsilon g-g^2

are

g=0,g∗=ϵ.g=0, \qquad g_*=\epsilon.

The Gaussian point is unstable below four dimensions, because

βR′(0)=ϵ>0.\beta_R'(0)=\epsilon>0.

A small positive quartic coupling grows as the system is viewed at longer distances. The interacting fixed point is stable in the quartic direction, because

βR′(g∗)=ϵ−2g∗=−ϵ.\beta_R'(g_*)= \epsilon-2g_*=-\epsilon.

Thus, if g(ℓ)=g∗+δg(ℓ)g(\ell)=g_*+\delta g(\ell), then

dδgdℓ=−ϵδg+O(δg2,ϵ2δg),{d\delta g\over d\ell}=-\epsilon\delta g+O(\delta g^2,\epsilon^2\delta g),

so

δg(ℓ)∼e−ϵℓ.\delta g(\ell)\sim e^{-\epsilon\ell}.

The corresponding correction-to-scaling exponent is

ω=ϵ+O(ϵ2).\omega=\epsilon+O(\epsilon^2).

In terms of the cutoff-scaled quartic coupling,

λˉ∗=16π23ϵ+O(ϵ2).\bar\lambda_* ={16\pi^2\over3}\epsilon+O(\epsilon^2).

The corresponding dimensionful coupling is λ∗=λˉ∗Λϵ\lambda_*=\bar\lambda_*\Lambda^\epsilon in this cutoff convention; it is not itself a universal fixed-point coordinate. The dimensionless value is small when ϵ\epsilon is small, which is what makes the expansion controlled.

One-loop beta function with Gaussian and Wilson–Fisher fixed points

For the length-scale flow dg/dℓ=ϵg−g2dg/d\ell=\epsilon g-g^2, the Gaussian fixed point becomes unstable for D<4D<4, while the Wilson–Fisher fixed point g∗=ϵg_*=\epsilon is stable in the quartic-coupling direction.

The one-loop flow equation is exactly solvable:

dgdℓ=g(ϵ−g).{dg\over d\ell}=g(\epsilon-g).

For initial value g(0)=g0>0g(0)=g_0>0,

g(ℓ)=ϵ1+(ϵg0−1)e−ϵℓ.\boxed{ g(\ell)= {\epsilon\over1+\left({\epsilon\over g_0}-1\right)e^{-\epsilon\ell}}. }

For 0<g0<ϵ0<g_0<\epsilon, the coupling grows toward ϵ\epsilon. For g0>ϵg_0>\epsilon, it decreases toward ϵ\epsilon; g0=ϵg_0=\epsilon is stationary. These statements hold for every positive initial value in the truncated differential equation. Its perturbative application requires small ϵ\epsilon and a trajectory at weak coupling. Within that regime, attraction toward a common fixed point explains universality.

At ϵ=0\epsilon=0, the same equation becomes

dgdℓ=−g2,{dg\over d\ell}=-g^2,

so

g(ℓ)=g01+g0ℓ.g(\ell)={g_0\over1+g_0\ell}.

Since ℓ∼log⁡(R/a)\ell\sim\log(R/a), the four-dimensional coupling vanishes only as 1/log⁡R1/\log R. This is why four-dimensional mean-field behavior is modified by logarithms rather than by new leading power laws.

The Wilson–Fisher fixed point is not stable in every direction. The mass or temperature perturbation must still be tuned. Write the temperature-like scaling field as tt, proportional to T−TcT-T_c after a nonuniversal normalization. Under RG,

dtdℓ=ytt+nonlinear terms.{dt\over d\ell}=y_t t+\text{nonlinear terms}.

At the Gaussian fixed point, yt=2y_t=2. Interactions renormalize the composite operator ϕ2\phi^2. The tadpole shell displays both the additive and multiplicative effects:

λ2∫shelldDq(2π)D1q2+r=λ2∫shelldDq(2π)D(1q2−rq4+⋯ ).{\lambda\over2} \int_{\rm shell}{d^Dq\over(2\pi)^D}{1\over q^2+r} = {\lambda\over2} \int_{\rm shell}{d^Dq\over(2\pi)^D} \left({1\over q^2}-{r\over q^4}+\cdots\right).

The first term moves the critical surface to rc(λ)r_c(\lambda). After subtracting that additive shift, the term linear in the scaling field t=r−rct=r-r_c combines with the tree-level rescaling. In the normalization above, the one-loop flow is

dtdℓ=(2−g3+O(g2,ϵg))t.{dt\over d\ell} = \left(2-{g\over3}+O(g^2,\epsilon g)\right)t.

The unexpanded shell coefficient is (KD/K4)g/3(K_D/K_4)g/3; replacing KDK_D by K4K_4 accounts for the O(ϵg)O(\epsilon g) remainder. Evaluating at the Wilson–Fisher fixed point gives

yt=2−ϵ3+O(ϵ2).\boxed{ y_t=2-{\epsilon\over3}+O(\epsilon^2). }

The correlation length exponent is the inverse of this relevant eigenvalue:

ν=1yt.\nu={1\over y_t}.

Therefore

ν=12+ϵ12+O(ϵ2).\boxed{ \nu={1\over2}+{\epsilon\over12}+O(\epsilon^2). }

This is the first non-mean-field exponent produced by the epsilon expansion. The Gaussian answer ν=1/2\nu=1/2 is shifted because the energy operator, represented in the continuum by ϕ2\phi^2, has an anomalous scaling dimension at the interacting fixed point.

Critical surface and relevant mass direction near the Wilson–Fisher fixed point

The Wilson–Fisher fixed point is stable along the quartic-coupling direction but unstable along the temperature direction. Criticality is reached by tuning onto the critical surface r=rc(g)r=r_c(g).

The anomalous dimension η\eta is defined by the critical two-point function

⟨ϕ(x)ϕ(0)⟩∼1∣x∣D−2+η,\langle\phi(x)\phi(0)\rangle \sim {1\over |x|^{D-2+\eta}},

or, equivalently,

G(k)∼1k2−η.G(k)\sim {1\over k^{2-\eta}}.

At one loop in ϕ4\phi^4 theory, the self-energy is the tadpole

Σ1(k)=λ2∫q1q2+r.\Sigma_1(k)={\lambda\over2}\int_q {1\over q^2+r}.

This integral is independent of the external momentum kk. It shifts the mass and therefore the location of the critical surface, but it does not renormalize the coefficient of k2k^2 in the inverse propagator. Hence

η=0+O(ϵ2).\boxed{ \eta=0+O(\epsilon^2). }

The first momentum-dependent self-energy correction is the two-loop sunset diagram:

Σ2(k)∼λ2∫dDp dDqp2q2(p+q+k)2.\Sigma_2(k) \sim \lambda^2 \int {d^Dp\,d^Dq\over p^2q^2(p+q+k)^2}.

For 3<D<43<D<4, use the same rotationally symmetric ultraviolet regulator in both terms and subtract the mass term before removing the cutoff. The remaining momentum-dependent part has scaling

Σ2(k)−Σ2(0)∼λ2k2D−6.\Sigma_2(k)-\Sigma_2(0) \sim \lambda^2 k^{2D-6}.

At D=4D=4, a local k2k^2 counterterm is also required. After renormalization, the nonlocal dependence is proportional to λ2k2log⁡(k/μ)\lambda^2 k^2\log(k/\mu). Power counting here determines the momentum power and loop order, not the coefficient or sign of that logarithm. Since g∗∼ϵg_*\sim\epsilon, the field anomalous dimension begins at order ϵ2\epsilon^2.

The tadpole only shifts the mass; momentum dependence first appears in the sunset and changes field scaling at two loops.

The tadpole is independent of external momentum. For 3<D<43<D<4, the sunset difference is defined with a common symmetric regulator and mass subtraction before removing it. At D=4D=4, a local kinetic counterterm is also required; the displayed renormalized nonlocal dependence omits its coefficient and sign. This schematic explains the loop order η=O(ϵ2)\eta=O(\epsilon^2), not the numerical value of η\eta.

For the one-component Ising theory,

η=ϵ254+O(ϵ3),\eta={\epsilon^2\over54}+O(\epsilon^3),

This two-loop coefficient is reported in Wilson and Fisher 1972, p. 243, PDF; deriving its value is beyond the one-loop calculation here.

At a fixed point, the scaling dimension of the spin field is

Δϕ=D−2+η2.\Delta_\phi={D-2+\eta\over2}.

The two-point function at criticality is therefore

⟨ϕ(x)ϕ(0)⟩∼1∣x∣2Δϕ=1∣x∣D−2+η.\langle\phi(x)\phi(0)\rangle \sim {1\over |x|^{2\Delta_\phi}} ={1\over |x|^{D-2+\eta}}.

Away from criticality, the correlation length is set by the relevant temperature perturbation:

ξ∼∣t∣−1/yt=∣t∣−ν.\xi\sim |t|^{-1/y_t}=|t|^{-\nu}.

The susceptibility is the integral of the connected two-point function up to distances of order ξ\xi:

χ∼∫ξdDx 1∣x∣D−2+η∼ξ2−η.\chi \sim \int^{\xi}d^Dx\,{1\over |x|^{D-2+\eta}} \sim \xi^{2-\eta}.

Thus

γ=ν(2−η).\gamma=\nu(2-\eta).

Using η=0+O(ϵ2)\eta=0+O(\epsilon^2) and ν=1/2+ϵ/12+O(ϵ2)\nu=1/2+\epsilon/12+O(\epsilon^2) gives

γ=1+ϵ6+O(ϵ2).\boxed{ \gamma=1+{\epsilon\over6}+O(\epsilon^2). }

Other exponents follow from scaling relations. To first order,

η=0+O(ϵ2),ν=12+ϵ12+O(ϵ2),γ=1+ϵ6+O(ϵ2),βmag=12−ϵ6+O(ϵ2),δ=3+ϵ+O(ϵ2),α=ϵ6+O(ϵ2).\begin{aligned} \eta&=0+O(\epsilon^2),\\ \nu&={1\over2}+{\epsilon\over12}+O(\epsilon^2),\\ \gamma&=1+{\epsilon\over6}+O(\epsilon^2),\\ \beta_{\rm mag}&={1\over2}-{\epsilon\over6}+O(\epsilon^2),\\ \delta&=3+\epsilon+O(\epsilon^2),\\ \alpha&={\epsilon\over6}+O(\epsilon^2). \end{aligned}

Here βmag\beta_{\rm mag} is the magnetization exponent, not inverse temperature and not an RG beta function. The notation is old and unfortunate, so context has to do the work.

Setting ϵ=1\epsilon=1 gives rough three-dimensional Ising estimates such as

ν≈0.583,γ≈1.167.\nu\approx0.583, \qquad \gamma\approx1.167.

These are not precision values. The achievement of the one-loop epsilon expansion is structural: it explains why a non-Gaussian universal fixed point exists and why its exponents can be computed systematically.

The same dimensional reasoning appears in gauge theory. In the convention F=dA+[A,A]F=dA+[A,A], where the coupling multiplies the whole action, a DD-dimensional Euclidean Yang–Mills action is

SYM=14gD2∫dDx FμνaFμνa.S_{\rm YM}={1\over4g_D^2}\int d^D x\,F_{\mu\nu}^aF_{\mu\nu}^a.

The gauge coupling has engineering dimension

[gD2]=4−D.[g_D^2]=4-D.

Thus four dimensions are also the dimension where Yang–Mills coupling is classically marginal. At D=4D=4, loops generate logarithmic running. In D=3D=3, the coupling g32g_3^2 has dimension of mass, so the natural dimensionless coupling at momentum scale qq is

geff2(q)∼g32q.g_{\rm eff}^2(q)\sim {g_3^2\over q}.

It grows in the infrared already by dimensional analysis. This does not make scalar criticality and gauge dynamics identical, but it highlights a shared lesson: the physical strength of an interaction is the dimensionless coupling at the scale being probed, not the bare constant by itself.

At D=4D=4, the Ising quartic coupling is classically marginal and the one-loop four-point diagram produces logarithms. Slightly below four dimensions, these logarithms combine with classical scaling to produce the beta function

dgdℓ=ϵg−g2+O(g3,ϵg2),ϵ=4−D.{dg\over d\ell}=\epsilon g-g^2+O(g^3,\epsilon g^2), \qquad \epsilon=4-D.

There are two nearby fixed points:

g=0,g∗=ϵ+O(ϵ2).g=0, \qquad g_*=\epsilon+O(\epsilon^2).

The Gaussian point is unstable for D<4D<4. The Wilson–Fisher point is stable in the quartic direction and controls the ordinary Ising critical point. The mass direction remains relevant, with eigenvalue

yt=2−ϵ3+O(ϵ2).y_t=2-{\epsilon\over3}+O(\epsilon^2).

Therefore

ν=12+ϵ12+O(ϵ2).\nu={1\over2}+{\epsilon\over12}+O(\epsilon^2).

The one-loop self-energy is momentum independent, so

η=0+O(ϵ2).\eta=0+O(\epsilon^2).

The susceptibility exponent follows from scaling:

γ=1+ϵ6+O(ϵ2).\gamma=1+{\epsilon\over6}+O(\epsilon^2).

The epsilon expansion is not a perturbation of the lattice coupling. It is an expansion in the fixed-point value of a dimensionless long-distance coupling, which is small when DD is close to four.

Confusing the critical mass with the bare mass. The critical condition is not the naive bare equation r=0r=0. Tadpoles shift the critical surface, so one must tune the physical inverse correlation length to zero.

Forgetting the RG-time convention. With increasing momentum scale μ\mu, the beta function is μ dg/dμ=−ϵg+g2+⋯\mu\,dg/d\mu=-\epsilon g+g^2+\cdots. With increasing length scale ℓ\ell, its sign is reversed. The fixed points agree, but the flow arrows do not.

Treating η=0\eta=0 at one loop as exact. The one-loop tadpole is momentum independent. Wavefunction renormalization starts with the two-loop sunset, giving η=O(ϵ2)\eta=O(\epsilon^2).

Using ϵ=1\epsilon=1 as precision perturbation theory. The expansion is controlled near four dimensions. First-order three-dimensional estimates are structural guides, not precision values.

Equating irrelevant with disposable. Above four dimensions the quartic coupling is dangerously irrelevant: it does not change the leading Gaussian critical two-point function, but it stabilizes the ordered phase and causes violations of naive hyperscaling.

Show that the bubble integral

BD(p)=∫dDq(2π)D1q2(q+p)2B_D(p)=\int {d^Dq\over(2\pi)^D}{1\over q^2(q+p)^2}

has scaling dimension D−4D-4.

Solution

Rescale q=pQq=pQ, where pp denotes the magnitude of the external momentum. Then

dDq=pDdDQ,q2=p2Q2,(q+p)2=p2(Q+p^)2.d^Dq=p^D d^DQ, \qquad q^2=p^2Q^2, \qquad (q+p)^2=p^2(Q+\hat p)^2.

Therefore

BD(p)=pD−4∫dDQ(2π)D1Q2(Q+p^)2.B_D(p) =p^{D-4} \int {d^DQ\over(2\pi)^D}{1\over Q^2(Q+\hat p)^2}.

The remaining integral is dimensionless after regularization. Hence

BD(p)∼pD−4.B_D(p)\sim p^{D-4}.

At D=4D=4, the power vanishes and the dimensionless integral becomes logarithmic.

Exercise 2: Fixed points and their stability

Section titled “Exercise 2: Fixed points and their stability”

For the one-loop length-scale beta function

dgdℓ=ϵg−g2,{dg\over d\ell}=\epsilon g-g^2,

find the fixed points and determine their stability for ϵ>0\epsilon>0.

Solution

Set the beta function to zero:

0=g(ϵ−g).0=g(\epsilon-g).

Thus

g=0,g∗=ϵ.g=0, \qquad g_*=\epsilon.

The derivative is

βR′(g)=ϵ−2g.\beta_R'(g)=\epsilon-2g.

At g=0g=0,

βR′(0)=ϵ>0,\beta_R'(0)=\epsilon>0,

so a small positive coupling grows as ℓ\ell increases. The Gaussian fixed point is infrared-unstable. At g∗=ϵg_*=\epsilon,

βR′(g∗)=−ϵ<0,\beta_R'(g_*)=-\epsilon<0,

so deviations decay as e−ϵℓe^{-\epsilon\ell}. The Wilson–Fisher fixed point is infrared-stable in the quartic direction.

Solve

dgdℓ=g(ϵ−g){dg\over d\ell}=g(\epsilon-g)

with g(0)=g0>0g(0)=g_0>0 and ϵ>0\epsilon>0.

Solution

For g0=ϵg_0=\epsilon, the stationary solution is g(ℓ)=ϵg(\ell)=\epsilon. For g0≠ϵg_0\ne\epsilon, separate variables:

dgg(ϵ−g)=dℓ.{dg\over g(\epsilon-g)}=d\ell.

Since

1g(ϵ−g)=1ϵ(1g+1ϵ−g),{1\over g(\epsilon-g)}={1\over\epsilon}\left({1\over g}+{1\over\epsilon-g}\right),

integration gives

1ϵlog⁡∣gϵ−g∣=ℓ+C.{1\over\epsilon}\log\left\lvert{g\over\epsilon-g}\right\rvert=\ell+C.

Using g(0)=g0g(0)=g_0 and solving for g(ℓ)g(\ell),

g(ℓ)=ϵ1+(ϵg0−1)e−ϵℓ.\boxed{ g(\ell)= {\epsilon\over1+\left({\epsilon\over g_0}-1\right)e^{-\epsilon\ell}}. }

The absolute value keeps the integration real on either side of g=ϵg=\epsilon. The final expression includes the stationary solution by continuity. For ℓ≥0\ell\ge0, it approaches ϵ\epsilon for every positive initial value of the truncated equation; interpreting the trajectory perturbatively requires weak coupling.

Exercise 4: The correlation-length exponent

Section titled “Exercise 4: The correlation-length exponent”

Using

yt=2−ϵ3+O(ϵ2),y_t=2-{\epsilon\over3}+O(\epsilon^2),

derive

ν=12+ϵ12+O(ϵ2).\nu={1\over2}+{\epsilon\over12}+O(\epsilon^2).
Solution

By definition,

ν=1yt.\nu={1\over y_t}.

Write

yt=2(1−ϵ6+O(ϵ2)).y_t=2\left(1-{\epsilon\over6}+O(\epsilon^2)\right).

Then

ν=12(1−ϵ6+O(ϵ2))−1.\nu={1\over2}\left(1-{\epsilon\over6}+O(\epsilon^2)\right)^{-1}.

Using (1−x)−1=1+x+O(x2)(1-x)^{-1}=1+x+O(x^2) gives

ν=12(1+ϵ6+O(ϵ2))=12+ϵ12+O(ϵ2).\nu={1\over2}\left(1+{\epsilon\over6}+O(\epsilon^2)\right) ={1\over2}+{\epsilon\over12}+O(\epsilon^2).

Exercise 5: Momentum dependence of the sunset

Section titled “Exercise 5: Momentum dependence of the sunset”

Estimate the momentum dependence of the two-loop sunset self-energy at criticality:

Σ2(k)∼λ2∫dDp dDqp2q2(p+q+k)2.\Sigma_2(k) \sim \lambda^2\int {d^Dp\,d^Dq\over p^2q^2(p+q+k)^2}.
Solution

The two loop measures contribute dimension 2D2D. The three propagators contribute dimension −6-6. For 3<D<43<D<4, subtract the mass term using the same rotationally symmetric ultraviolet regulator in both integrals, then remove the cutoff. The remaining momentum dependence has scale kk. Therefore

Σ2(k)−Σ2(0)∼λ2k2D−6,\Sigma_2(k)-\Sigma_2(0) \sim \lambda^2 k^{2D-6},

At D=4D=4, one must also subtract a local kinetic term; the remaining nonlocal dependence is proportional to λ2k2log⁡(k/μ)\lambda^2k^2\log(k/\mu). The mass subtraction alone does not renormalize the four-dimensional integral. This is why wavefunction renormalization, and hence η\eta, begins at order λ2\lambda^2 or ϵ2\epsilon^2.

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