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[4], [3], [2], adiance) cse.Det hs esn hscsshave physicists reasons these to Due ocesses. aino h akrudmti,wihi a is which metric, background the on iation oso htqatzdaosi perturbations acoustic quantized that show to , aiya h oi oio.Ti sacceptable is This horizon. sonic the at ravity in o yEnti’ qain tmymimic may it equation, Einstein’s by not tion, cladqatmgaiainlrgms have regimes, gravitational quantum and ical y, fc hr h nadnra eoiyo the of velocity normal inward the where rface bet ii rvttoa ytmi its in system gravitational a mimic to able ern dao nlgmdl ae nfluid on based models analog of idea neering coaeBcgon eprtr.S the So temperature. Background icrowave rmabakhl oio i Hawking via horizon hole black a from s eninrdi re omiti the maintain to order in ignored been s h o sirttoa,teeuto of equation the irrotational, is flow the h atcul fyas oseveral to years, of couple last the † all a.Tems eakbefact remarkable most The ial. cutcdsubne within disturbances acoustic Lorentzian (1) in proposals for the experimental verification of acoustic . The Hawking temperature for typical acoustic analogues has been estimated to be in the nano-Kelvin range; with improved experimental techniques and equipment, this is not outside the realm of realistic possibilities in the near future. One slightly unsavory feature of the Unruh approach has to do with the necessity of quantizing linearized acoustic disturbances and the manner in which they are quantized. In a classical fluid, there is no compelling physical reason to quantize acoustic disturbances. So quantizing acoustic perturbations just to demonstrate Hawking radiation from the horizon of acoustic black holes appears somewhat artificial. In a quantum fluid like superfluid on the other hand, there are phonon excitations of the fluid background itself. On top of this one may have acoustic perturbations which are quantized in terms of phonons. However, in that case, the division between the background and linear acoustic fluctuations tends to get a bit hazy. There is however an alternative phenomenon which does not necessitate quantization of acoustic disturbances for it to occur, although a full quantum description is possible in principle. This is the phenomenon called Superresonance by us [7] which occurs in a curved Lorentzian acoustic geometry if the acoustic spacetime is that of a rotating . Recall that such a black hole spacetime admits a region - the ergoregion - containing the event horizon, where the time translation Killing vector turns spacelike. The existence of this region is crucial for the Penrose process of energy extraction from the black hole, at the cost of its rotational energy. Superresonance is simply an acoustic wave version of the Penrose process, wherein a plane wave solution of a massless scalar field in the black hole background is scattered from the ergoregion with an amplification of its amplitude. The energy gained by the wave is at the cost of the rotational energy of the black hole. In the earlier paper [7], superresonance has been shown to occur in a certain class of analogue 2+1 dimensional rotating black holes. Linear acoustic perturbations in such a background are shown to scatter from the ergoregion with an enhancement in amplitude, for a restricted range of frequencies of the incoming wave. However, while the plausibility of superresonance was established in that earlier work through the analysis of the Wronskian of the radial equation of the acoustic perturbations, the actual frequency dependence of the amplification factor was not worked out. In this paper this gap is filled. We present a more detailed quantitative analysis of this phenomenon, as also a somewhat different way of arriving at the results of the previous paper. An explicit expression is derived for the reflection coefficient as a function of the frequency of the incoming wave for a certain low frequency regime. This expression is expected to be useful for possible future experimental endeavors to observe superresonance. The plan of the paper is as follows: in section II, certain aspects of the acoustic black hole analogue we work with are reviewed. The demonstration of superresonance is repeated with a choice of coordinates different from those used in the earlier work [7]. In section III, detailed quantitative analysis of the reflection coefficient is presented, explicitly exhibiting its frequency dependence, albeit within a certain restricted low frequency regime. We conclude in section IV with a sketch of the outlook on this class of problems.

II. DRAINING VORTEX FLOW AND SUPERRESONANCE

In order to demonstrate superresonance, a certain choice is to be made of the velocity potential of the fluid, which functions as a suitable acoustic analogue of a Kerr black hole. In other words, the flow must have a well-defined (ergo)region of transonic flow containing a sonic horizon as discussed in the Introduction. In 2+1 dimensions, a velocity profile with these properties is the ‘draining vortex’ flow with a sink at the origin, given by [8]

A B v = rˆ + φˆ , (2) −→ − r r where A, B are real and positive and (r, φ) are plane polar coordinates. The metric corresponding to this effective geometry is ,

2 2 2 2 ρ0 2 A + B 2 2 A 2 2 2 ds = c dt + dr dt 2B dφ dt + dr + r dφ (3) c − − r2 r −       A A two surface, at r = c , in this flow, on which the fluid velocity is everywhere inward pointing and the radial component of the fluid velocity exceeds the local sound velocity everywhere, behaves as an outer trapped surface in this acoustic geometry. This surface can be identified with the future event horizon of the black hole. Since the fluid velocity (2) is always inward pointing the linearized fluctuations originating in the region bounded by the sonic horizon cannot cross this boundary. As for the Kerr black hole in , the radius of the boundary of 2 2 the ergosphere of the acoustic black hole is given by vanishing of g00 , i.e, re = √A + B /c. If we assume that the background density of the fluid is constant, it automatically implies that background pressure and the local speed of

2 sound are also constant. Thus we can ignore the position independent pre-factor in the metric because it will not effect the equation of motion of fluctuations of the velocity potential. From the components of the draining vortex metric it is clear that the (2+1)-dimensional curved spacetime possesses isometries that correspond to time translations and rotations on the plane. The solution of the massless Klein Gordon equation can therefore be written as,

Ψ(t, r, φ)= R(r) e−i ω t eimφ (4) where ω and m are real and positive. In order to make Ψ(t, r, φ) single valued , m should take integer values. Then the radial function R(r) satisfies

d2R(r) dR(r) + P1(r) + Q1(r) R(r)=0 , (5) dr2 dr where,

A2 + r2 c2 +2 i A (B m r2 ω) P1(r)= − r (r2 c2 A2) − and 2 iABm B2m2 + c2m2 r2 +2 Bmωr2 r4 ω2 Q1(r)= − − . r2 (r2 c2 A2) − Observe that the equ.(5) is different from that used in [7] (equ. 8), since the diffeomorphisms given in equ. (5) of [7] have not been effected in the present case. Now we introduce tortoise coordinate r∗ through the equation,

d A2 d = 1 (6) dr∗ − r2 c2 dr   which implies that,

A r c A r∗ = r + log − (7) 2 c r c + A

A This tortoise coordinate spans the entire real line as opposed to r which spans only the half-line.The horizon at r = c maps to r∗ , while r corresponds to r∗ + . Let us now define a new radial function G(r) as, → −∞ → ∞ → ∞ H(r) i ω A r2 c2 m B A2 R(r)= exp log 1 log 1 (8) √r 2 c2 A2 − − A − r2 c2       Substituting this in equation (5) we observe that G(r) satisfies the differential equation

2 2 2 2 2 A d A d 1 B m A 1 2 1 5 A 1 1 H(r)+ ω 1 m + H(r)=0 − r2 c2 dr − r2 c2 dr c2 − r2 − − r2 c2 r2 − 4 r4c2      "        # (9)

Now in terms of tortoise coordinate one obtains the modified differential equation as,

2 d2H(r∗) 1 B m A2 1 1 5 A2 + ω 1 m2 + H(r∗)=0 (10) dr∗2 c2 − r2 − − r2 c2 r2 − 4 r4 c2 "        # We analyze this differential equation in two distinct radial regions, viz., near the sonic horizon, i.e., at r∗ and at asymptopia, i.e., at r∗ + . In the asymptotic region, the above differential equation can be→ written −∞ approximately as, → ∞

d2H(r∗) ω2 + H(r∗)=0 (11) dr∗2 c2

3 This can be solved trivially,

∗ ω ∗ ω ∗ H(r )= Rωm exp i r + exp i r (12) c − c     The first term in the above equation corresponds to reflected wave and the second term to the incident wave, so that R is the reflection coefficient in the sense of potential scattering. Similarly , near the horizon the above differential equation can be written approximately as,

2 ∗ 2 d H(r ) (ω m ΩH ) + − H(r∗)=0 (13) dr∗2 c2 where ΩH is the angular velocity of the sonic horizon. We impose the physical boundary condition that of the two solutions of this equation, only the ingoing one is physical, so that one has,

∗ (ω m ΩH ) ∗ H(r )= Tωm exp i − r (14) − c   Now using these approximate solutions of the above differential equation together with their complex conjugates and recalling the fact two linearly independent solutions of this differential equation (10) must lead to a constant Wronskian, it is easy to show that,

2 m ΩH 2 1 Rωm = 1 Tωm (15) − | | − ω | |  

Here Rωm and Tωm are amplitudes of the reflection and transmission coefficient of the scattered wave respectively. It is obvious from the above equation that, for frequencies in the range 0 <ω

III. THE REFLECTION COEFFICIENT

We begin with defining a new function L(r) through the relation

r c i ω A r2 c2 m B A2 R(r)= exp log 1 log 1 L(r) . (16) A 2 c2 A2 − − A − r2 c2       2 2 r c We next introduce a new variable x 2 1 . Then L(x) satisfies the differential equation , ≡ A − d2L(x) 1 1 dL(x) Q2 1 ω2 A2 L(x) + + + + + (1 S2)+ x = 0 (17) dx2 x x +1 dx x x +1 − c4 4x(x + 1)     where,

2 ω A B m Q2 = c2 − A   2 Bmω 2 ω2 A2 S2 = m2 + c2 − c4 In order to find a solution of this differential equation, we adapt a matching procedure employed by Starobinsky [3]; for the region

4 ω A ω A x m , 1 c2 ≪ c2 ≪   the above differential equation can be approximately written as,

d2L(x) 1 1 dL(x) Q2 1 L(x) + + + + + (1 S2) =0 . (18) dx2 x x +1 dx x x +1 − 4x(x + 1)     This is the standard Riemann-Papparitz equation with regular singular points at 0, 1, and at . We can convert this differential equation into the Hypergeometric form by the following substitution,− ∞

′ ′ L(x)= xα (x + 1)β G(x) (19) such that G(x) satisfies the Hypergeometric differential equation given by

d2G(x) dG(x) x(1 x) + [ γ (α + β + 1)x ] αβG(x)=0 (20) − dx2 − dx − where

′ Q ′ 1 α = i , β = − 2 −2 S Q S Q α = i , β = i , γ =1 i Q − 2 − 2 2 − 2 −

x = x − The most general solution of this differential equation is ,

1−γ G(x)= C1 2F1(α, β; γ; x)+ C2 x 2F1(α +1 γ,β +1 γ;2 γ; x) (21) − − − where C1 and C2 are arbitrary constants to be determined. Near the horizon, x 0 ∼ ′ ′ α −α G(x) C1 x + C2 x . (22) −→ 1−γ Here we have absorbed ( 1) in C2 . The first term represents ingoing wave and the second term represents outgoing wave near the horizon.− Since nothing can come out of the horizon, the boundary condition at the horizon implies that C2 = 0. Therefore the solution of equ.(18) reduces to

′ ′ α β L(x)= C1 x (x + 1) 2F1(α, β; γ; x) (23) − To use the matching procedure we need to know the behavior of this solution in the asymptotic region, i.e, at x . This can be obtained by the transformation (x 1/x) for the Hypergeometric function in above equation.−→ ∞ Using this rule we obtain, →

′ ′ α β Γ(γ) Γ(β α) −α ( 1) L(x)= C1x (x + 1) − x 2F1 α , α +1 γ ; α +1 β ; − Γ(β) Γ(γ α) − − x  −   − β Γ(γ) Γ(α β) ( 1) +x − 2F1 β, β +1 γ ; β +1 α ; − (24) Γ(α) Γ(γ β) − − x −   So in the region x Max( m2,Q2 ), we have ≫ ′ ′ α β Γ(γ) Γ(β α) −α Γ(γ) Γ(α β) −β L(x) C1 x (x + 1) − x + − x (25) −→ Γ(β) Γ(γ α) Γ(α) Γ(γ β)  − −  Hence the approximate form of L(x) in the region,

ω A Max( m2,Q2 ) x m ≪ ≪ c2 .   5 is given by

C1 Γ(γ) Γ(β α) S Γ(γ) Γ(α β) S L(x)= − x 2 + − x− 2 √ x Γ(β) Γ(γ α) Γ(α) Γ(γ β)  − − 

1 S − S = D1 x 2 + D2 x 2 (26) √ x h i where,

Γ(γ) Γ(β α) D1 = − C1 Γ(β) Γ(γ α) − Γ(γ) Γ(α β) D2 = − C1 Γ(α) Γ(γ β) − The solution (26) is in a form where it is not obvious which combinations of the complex coefficients D1,D2 corre- spond to the ingoing and outgoing modes, This information can be retrieved from the energy flux per unit time radially 2 2 ω A across an arbitrarily chosen surface at a constant radial coordinate r in the region Max( m ,Q ) x m 2 . ≪ ≪ c This is obtained by the surface integral .  2 π µ ν FL = Tµν l k √ g dφ − 0 − Z ∗ ∗ = iπSω D1 D2 D1 D2 − πωS  2  2 = D1 + i D2 D1 i D2 (27) 2 | | − | − |   µ µ where Tµν is the energy momentum tensor for Ψ, l is the normal to a constant r surface , k is the time translational killing vector and g is the determinant of the . Given that the outgoing mode of the wave corresponds to a positive value of radial component of the flux, and the ingoing mode just the opposite, one concludes that the amplitudes of the incident and reflected wave are proportional to (D1 i D2) and (D1 + i D2) respectively. One can− now write down an explicit expression for the amplification factor(AF); this is given by,

2 2 D1 + iD2 AF 1 Rωm =1 ≡ − | | − D1 iD2 − ∗ ∗ 2 i (D1 D2 D1 D2) = − 2 D1 i D2 | − | 2 2 2 Q C1 2 ω A C1 m ΩH = | | 2 = 2 | | 2 1 (28) S D1 i D2 S c D1 i D2 − ω | − | | − |   It follows from this that the reflection coefficient exceeds unity in the frequency range 0 < ω

2 2 2 ω A C1 Tωm = 2 | | 2 (29) | | S c D1 i D2 | − | Equations (28-29) exhibit the frequency dependence of both the reflection and transmission coefficients and hence of the amplification factor in the low frequency regime. If vortex motion with a sink is realized in the laboratory, our result can be used to provide an order of magnitude estimate for the amplification factor. According to our assumption ω A these relations are valid in the frequency range where c2 1 , i.e, when wave length of the sound wave is much larger than the radius of the horizon. Clearly, this frequency≪ range does not cover the entire superresonant range 0 to m ΩH . It is interesting and of importance to find the behavior of the reflection coefficient near the critical point around ω = m ΩH where the reflection coefficient is expected to cross unity. We hope to report on this in the near future.

6 IV. OUTLOOK

The link with possible experimental observation of superresonance is yet incomplete, despite the explicit expres- sions we have derived for the reflection and transmission coefficients. One needs to input into these results typical characteristics of draining vortex flows in fluids like superfluid helium which obey our assumptions of barotropicity, irrotationality and zero viscosity. These characteristics are to be derived from the macroscopic quantum mechanics of superfluid helium, and novel features like flux quantization are expected to play a non-trivial role. In particular, flux quantization may well lead to the phenomenon of discrete amplification discussed in [7], which would perhaps facilitate observation. We should mention that ergoregions in superfluid helium have been considered in ref. [9], [10], although from a somewhat different standpoint. These authors do not consider vortex flows with a drain, and as such, their acoustic spacetime does not share all characteristics of black holes, like an outer trapped surface. Another feature which we have ignored in the foregoing analysis is the existence of shock fronts at the interface of normal and transonic flows. Indeed, in astrophysical black holes, analysis of these shock fronts constitutes an important component of models used in observational work on these objects. The existence of these shock fronts are in part responsible for the non-observation of superradiant scattering in such black holes. The issue of shocks in acoustic black hole analogues thus assumes special significance for future work on this topic. One of us (PM) thanks J. Bhattacharjee, G. Bhattacharya and A. Chatterjee for helpful discussions.

[1] S. W. Hawking, Comm. Math. Phys., (1975) [2] Y. Zeldovich, JETP Lett. 14, 180 (1971); Sov. Phys. JETP 35, 1085 (1972) [3] A. Starobinski, Sov. Phys. JETP 37, 28 (1973). [4] B. DeWitt, Phys. Rep. 6, 295 (1975). [5] R. Wald, General Relativity, (University of Chicago, Chicago, 1984). [6] W. Unruh, Phys. Rev. Lett. 46, 1351 (1981); Phys. Rev. D 27, 2827 (1995). [7] S. Basak, P. Majumdar, arXiv gr-qc/0203059. [8] For a comprehensive and pedagogical review, see M. Visser, Class. Quant. Grav. 15, 1767 (1998) and references therein. [9] G. Volovik, Phys. Rep. 351, Issue 4, 195 (2001). [10] U. Fischer and G. Volovik, Int. Jou. Mod. Phys. 10, 57 (2001).

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