The Power Wall Steve Fulling and Jef Wagner Quantum Vacuum Workshop, TAMU, July 2010 1 Motivation • Physical understanding requires hT µν (r)i. • Perfectly reflecting wall ⇒ divergence. • Ultraviolet cutoff ⇒ pressure paradox: ∂E 6= − ∂h ∂E =+ ∂x Z p Z p. Sh in dimension 2, intersecting planes. Sx 2 ∂E = +2 ∂h Z p in dimension 3 Sh (for both intersecting planes and sphere). • This shouldn’t happen in an internally consistent dynamical theory. • A steeply rising smooth potential ∗ mocks up a reflecting wall. ∗ should define a nonsingular, internally consistent theory. • In principle this can be done for a spherical boundary, etc., but for now we do only a plane one. 3 Renormalization Cylinder kernel divergences ⇐⇒ heat kernel. In dimension 3, hT 00 i should contain • universal t−4 divergence • t−2 term ∝ V (r) • ln t terms ∝ V 2 and ∇2 V . After removing these we should be able to set t = 0. Only the first occurs where V = 0. Elsewhere hT µν i should include V ϕ2 interaction term. 4 The model v(x, y, z) = 0, z<0 λz α , z > 0. (1 ≤ α ∈ R) α z . Get dimensions right: v = λ0 z0 1 α α+2 −1 z0 α+2 = . Only one length scale: ẑ = λ λ0 For any α, v(z0 ) = λ0 ; increasingly steep as α → ∞. 5 . .. . .. .. . . .. . . ... ...... .. . . . . . . . ..... ...... .. . . . . . . ..... ...... .. . . . . . . ..... .. .......... . . ..... .. .......... . . ..... ........... . . .... ............ . . . . ........... ............. . . . . ... ... ...... ....... ................ α=2 α=1 λ0 • z0 6 0 ϕ(r, x ) = X n ∂2 ∂t2 0 0 1 √ an φn (r)e−iωn x + a†n φn (r)eiωn x ]. 2ω n 2 ∂ T 1 00 , etc. T = lim − t→0 2 ∂t2 X φ (r)φ (r′ ) n n ′ T (t, r, r ) = e−ωn t . −ω n n +∇2 − v(z) T (t, x, y, z, z ′ ) = 2δ(t)δ(x)δ(y)δ(z−z ′ ). 7 Eigenfunctions φn (r) = eik⊥ ·r⊥ φp (z) (r⊥ , k⊥ ∈ R2 , z ∈ R, p ∈ (0, ∞).) 2 ∂ − 2 + v(z) − p2 φp (z) = 0. ∂z r 2 sin[pz − δ(p)] when z < 0. φp (z) = π 8 When z > 0, 2 − φp (z) = C(p)Pα z ẑ d α + z − E Pα (z, E) = 0, 2 dz , (ẑp) 2 , Pα (+∞, E) = 0. √ P2 (z, E) ∝ D 21 (E−1) ( 2 z). √ For hard wall at z0 , P∞ (z, E) ∝ sin[ E(z − z0 )]. √ (Henceforth usually ẑ = 1, E = p (z0 = 1 = λ0 ).) P1 (z, E) ∝ Ai(z − E), 9 The solutions must match at z = 0: Pα (0, p2 ) . tan δ(p) = −p ′ 2 Pα (0, p ) C(p)2 = 1 2 . 2 2 2 2 −2 ′ π Pα (0, p ) + p Pα (0, p ) Even for P = Ai, these formulas are unpleasant. 10 Small p When p = 0 the solution is known: α+2 2 1/2 1 z 2 . Pα (z, 0) = z K α+2 α+2 Perturbation expansion: Pα (z, E) = Pα (z, 0) + EPα(1) (z) + · · · . −1 2 α+2 α+1 α+3 Γ + O(p3 ). Γ δ(p) = p α + 2 α+2 α+2 11 Large p (WKB) φp (z) ∼ [p2 − v(z)] − 41 cos Z a z p π , p2 − v(z̃) dz̃ − 4 turning point a = p2/α . Z ap π 2 p − v(z) dz + δ(p) = mod π 4 0 3 1 1 1+2/α π B , = p + . α 2 α 4 12 α = 1 (Airy function): 2/3 4 2 p 3 Γ( 3 )/Γ( 3 ), p → 0, δ(p) ∼ 2p3 π + , p → ∞. 3 4 α = 2 (parabolic cylinder function): 5 3 2p Γ( 4 )/Γ( 4 ), p → 0, δ(p) ∼ πp2 π + , p → ∞. 4 4 13 Cylinder kernel calculations Recall X φ (r)φ (r′ ) n n T (t, r, r′ ) = e−ωn t . −ω n n ∂2 (2) 2 ′ ′ +∇ − v(z) T (t, r , z, z ) = 2δ(t)δ (r )δ(z − z ). ⊥ ⊥ ∂t2 φp (z ′ ) −2 . T̂ (ω, k⊥ , p) = 2 2 2 3/2 ω + k⊥ + p (2π) 14 Cartesian calculations 1 ′ T (t, r⊥ , z, z ) = − 2π Z ∞ 0 dp Y (s, p)φp (z)φp (z ′ ), p e−sp Y (s, p) ≡ , s ≡ t2 + |r⊥ |2 . s In potential-free region, z < 0, Z ∞ 1 ′ dp Y (s, p) sin pz − δ(p) sin pz − δ(p) . T =− 2 π 0 15 1 1 2π 2 t2 + r⊥2 + (z − z ′ )2 Z ∞ 1 ′ dp Y (s, p) cos p(z + z ) − 2δ(p) + 2 2π 0 T =− ≡ T free + T ren . Hard wall: δ(p) = z0 p ⇒ (correctly) T ren 1 1 = . 2π 2 t2 + r⊥2 + (z + z ′ − 2z0 )2 16 The bad news: ∞ e−sp ′ cos p(z + z ) − 2δ(p) dp T ren s 0 √ is poorly convergent when s ≡ t2 + r⊥2 is small, which is precisely where we want it. In fact, we should be able to take s = 0 and get a finite answer when z + z ′ > 0, but the integrand is pointwise infinite there! There is a genuine divergence for δ(p) = Ap + B unless B = 0. Asymptotics for small p as well as large is critical. Presumably large k⊥ is at fault, so . . . 1 = 2π 2 Z 17 Polar calculations Do the integral in polar coordinates in the Fourier space: (Z ≡ z + z ′ , s = (t, r⊥ ), v = (ω, k⊥ )) T ren ∞ 1 eiv·s = 4 dv 2 cos pZ − 2δ(p) dp 2 4π 0 v +p R3 Z ∞ Z 1 p 1 −1 = 3 dρ du s sin(sρ 1 − u2 ) π 0 0 × cos Zρu − 2δ(ρu) . Z Z 18 With s = 0 and z = z ′ , Z ∞ Z 1 p 1 T ren (0, 0, z, z) = 3 dρ du ρ 1 − u2 π 0 0 × cos 2zρu − 2δ(ρu) . Integration by parts (appealing to δ(0) = 0 !) improves the convergence but worsens the algebra: # " √ Z ∞ Z 1 1 d 1 − u2 T ren (0, 0, z, z) = − 3 dρ du 2π 0 du z − δ ′ (ρu) 0 × sin 2zρu − 2δ(ρu) . 19 Numerics (barely started) • Padé interpolation between small and large p asymptotics works fairly well. • The oscillatory integrals appear intractable so far, even with Riesz–Cesàro averaging. 20