Axion Bosenova Hirotaka Yoshino Hideo Kodama (KEK) Prog. Thoer. - - PowerPoint PPT Presentation

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Axion Bosenova Hirotaka Yoshino Hideo Kodama (KEK) Prog. Thoer. - - PowerPoint PPT Presentation

Axion Bosenova Hirotaka Yoshino Hideo Kodama (KEK) Prog. Thoer. Phys. 128, 153-190 (2012), arXiv:1203.5070[gr-qc] JGRG22 @ RESCEU University of Tokyo ( November 14, 2012 ) Contents Introduction Simulation Discussion Summary Introduction


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SLIDE 1

Axion Bosenova

Hirotaka Yoshino

JGRG22 @ RESCEU University of Tokyo (November 14, 2012)

Hideo Kodama (KEK)

  • Prog. Thoer. Phys. 128, 153-190 (2012),

arXiv:1203.5070[gr-qc]

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SLIDE 2

Contents

Introduction Simulation Summary Discussion

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SLIDE 3

Introduction

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SLIDE 4

CMB Polarization

10-33 4 10-28

Axion Mass in eV

108

Inflated Away

Decays

3 10-10

QCD axion

2 10-20 3 10-18

Anthropically Constrained Matter Power Spectrum Black Hole Super-radiance

Axiverse

QCD axion String axions

QCD axion was introduced to solve the Strong CP problem. It is one of the candidates of dark matter.

Arvanitaki, Dimopoulos, Dubvosky, Kaloper, March-Russel, PRD81 (2010), 123530.

String theory predicts the existence of 10-100 axion-like massive scalar fields. There are various expected phenomena of string axions.

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SLIDE 5

Axion field around a rotating black hole

Axion field forms a cloud around a rotating BH and extract energy of the BH by “superradiant instability”.

Arvanitaki, Dimopoulos, Dubvosky, Kaloper, March-Russel, PRD81 (2010), 123530. Arvanitaki and Dubovsky, PRD83 (2011), 044026.

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SLIDE 6

Superradiance

R = u √ r2 + a2 d2u dr2

+

  • ω2 − V (ω)
  • u = 0

ω < ΩHm

Superradiant condition:

Φ = Re[e−iωtR(r)S(θ)eimφ]

u ∼ e−i(ω−mΩH)r∗

∇2Φ =0

Massless Klein-Gordon field

  • 1 − mΩH

ω

  • |T|2 = 1 − |R|2

u ∼ Aouteiωr∗ + Aine−iωr∗

A 1

horizon

in

Aout

Zeľdovich (1971)

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SLIDE 7

Bound state

Zouros and Eardley, Ann. Phys. 118 (1979), 139. ω < ΩHm

Superradiant condition:

0.14 0.15 0.16 0.17 0.18 0.19 0.2 0.21 0.22

  • 100
  • 50

50 100 V r*/M !2 V

I II III IV

u ∼ e−i(ω−mΩH)r∗

distant region

u ∼ e−√

µ2−ω2r∗

Massive Klein-Gordon field

∇2Φ − µ2Φ =0

Detweiler, PRD22 (1980), 2323. near horizon

Typical time scale ∼ 107M

  • 50 s

(M = 10M⊙) 1.6 year (M = 106M⊙)

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SLIDE 8

Accretion Rotating Black Hole Super-Radiant Modes Decaying Modes Gravitons

BH-axion system

Superradiant instability

Emission of gravitational waves (Level transition, Pair annihilation of axions)

Effects of nonlinear self-interaction

Bosenova Mode mixing Arvanitaki and Dubovsky, PRD83 (2011), 044026.

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SLIDE 9

Nonlinear effect

c.f., QCD axion Typically, the potential of axion field becomes periodic U(1)PQ symmetry

PQ phase transition

V = f 2

aµ2[1 − cos(Φ/fa)]

ϕ ≡ Φ fa

∇2ϕ − µ2 sin ϕ = 0

QCD phase transition

Z(N) symmetry

Potential becomes like a wine bottle

⇒ ⇒

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SLIDE 10

Accretion Rotating Black Hole Super-Radiant Modes Decaying Modes Gravitons

BH-axion system

Superradiant instability Effects of nonlinear self-interaction

Bosenova Mode mixing Arvanitaki and Dubovsky, PRD83 (2011), 044026. Emission of gravitational waves (Level transition, Pair annihilation of axions)

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SLIDE 11

Bosenova in condensed matter physics

http://spot.colorado.edu/~cwieman/Bosenova.html BEC state of Rb85(interaction can be controlled) Switch from repulsive interaction to attractive interaction Wieman et al., Nature 412 (2001), 295

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SLIDE 12

What we would like to do

W e would like to study the phenomena caused by axion cloud generated by the superradiant instability around a rotating black hole. In particular, we study numerically whether “Bosenova” happens when the nonlinear interaction becomes important. W e adopt the background spacetime as the Kerr spacetime, and solve the axion field as a test field.

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SLIDE 13

Simulations

Typical two simulations Does the bosenova really happen?

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SLIDE 14

Setup

Numerical simulation

Sine-Gordon equation

∇2ϕ − µ2 sin ϕ = 0

a/M = 0.99, Mµ = 0.4

As the initial condition, we choose the bound state of the Klein-Gordon field of the mode.

l = m = 1

1 2 3 4 1 2 3 4 BH

40 20 20 40 40 20 20 40 r CosΦ r SinΦ

aM0.99, MΜ0.4

Initial peak value (A) 0.6 1370 (B) 0.7 1862 E/[(fa/Mp)2M]

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SLIDE 15

−200 ≤ r∗/M ≤ 200

(φ = 0)

Φ (θ = π/2)

ϕpeak(0) = 0.6

r cos φ

r sin φ

Axion field on the equatorial plane

Simulation (A)

(Equatorial plane)

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SLIDE 16

Simulation (A)

Peak value and peak location

5 10 15 20 200 400 600 800 1000 r*

(peak)

t/M (b)

0.5 1 1.5 2 200 400 600 800 1000 !peak t/M (a)

Fluxes toward the horizon Energy and angular momentum distribution

  • 0.01
  • 0.008
  • 0.006
  • 0.004
  • 0.002

0.002 200 400 600 800 1000 FE and FJ t/M FE FJ

  • 10

10 20 30 40 50 60 70

  • 200
  • 100

100 200 300 dE/dr* r*/M t = 0 t = 1000M

  • 0.5
0.5 1 50 100 150 200 t = 0 t = 1000M
  • 20

20 40 60 80 100 120 140 160 180

  • 200
  • 100

100 200 300 dJ/dr* r*/M t = 0 t = 1000M

  • 1
1 2 50 100 150 200 t = 0 t = 1000M
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SLIDE 17

−200 ≤ r∗/M ≤ 200

(φ = 0)

Φ (θ = π/2)

ϕpeak(0) = 0.7

r cos φ

r sin φ

Axion field on the equatorial plane

Simulation (B)

(Equatorial plane)

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SLIDE 18

1 2 3 4 200 400 600 800 1000 !peak t/M (a) 4 8 12 16 200 400 600 800 1000 r*

(peak)

t/M (b)

  • 1.6
  • 1.2
  • 0.8
  • 0.4

0.4 0.8 200 400 600 800 1000 FE and FJ t/M FE FJ

  • 20

20 40 60 80 100

  • 200
  • 100

100 200 300 dE/dr* r*/M t = 0 t = 750M t = 1500M

  • 0.1
0.1 0.2 0.3 0.4 0.5
  • 200 -150 -100
  • 50
t = 750M t = 1500M
  • 0.5
0.5 1 1.5 2 100 200 300 400 500 600 t = 0 t = 750M t = 1500M
  • 50

50 100 150 200 250 300

  • 200
  • 100

100 200 300 dJ/dr* r*/M t = 0 t = 750M t = 1500M

  • 1.5
  • 1
  • 0.5
0.5
  • 200 -150 -100
  • 50
t = 750M t = 1500M
  • 2
2 4 6 8 100 200 300 400 500 600 t = 0 t = 750M t = 1500M

Peak value and peak location Fluxes toward the horizon Energy and angular momentum distribution

Simulation (B)

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SLIDE 19
  • 20

20 40 60 80 100

  • 200
  • 100

100 200 300 dE/dr* r*/M t = 0 t = 750M t = 1500M

  • 0.1

0.1 0.2 0.3 0.4 0.5

  • 200 -150 -100
  • 50

t = 750M t = 1500M

  • 0.5

0.5 1 1.5 2 100 200 300 400 500 600 t = 0 t = 750M t = 1500M

Energy distribution

Simulation (B)

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SLIDE 20

Simulations

Typical two simulations Does the bosenova really happen?

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SLIDE 21

Does bosenova really happen?

time amplitude Bosenova??? (A) Saturation???

Additional simulation:

ϕ(0) = Cϕ(A)(1000M) ˙ ϕ(0) = C ˙ ϕ(A)(1000M)

C =    1.05 1.08 1.09

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SLIDE 22

Supplementary simulation

ϕ(0) = Cϕ(A)(1000M) ˙ ϕ(0) = C ˙ ϕ(A)(1000M)

Energy absorbed by the black hole

∆E := t FEdt

C1.05 1.08 1.09

2000 4000 6000 8000 10000 20 20 40 60 80

tM E

C =    1.05 1.08 1.09

The bosenova happens when E ≃ 1600 × (fa/Mp)2M

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SLIDE 23

Discussions

Effective theory Gravitational waves

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SLIDE 24

rp δr δν

Effective theory (1)

Action

ˆ S =

  • d4x√−g
  • −1

2(∇ϕ)2 − µ2 ϕ2 2 + ˆ UNL(ϕ)

  • ,

Non-relativistic approximation

ϕ = 1 √2µ

  • e−iµtψ + eiµtψ∗

ˆ SNR =

  • d4x

i 2

  • ψ∗ ˙

ψ − ψ ˙ ψ∗ − 1 2µ∂iψ∂iψ∗ + αg r ψ∗ψ − µ2 ˜ UNL(|ψ|2/µ)

˜ UNL(x) = −

  • n=2

(−1/2)n (n!)2 xn.

Approximate the axion cloud as a Gaussian wavepacket

ψ = A(t, r, ν)eiS(t,r,ν)+imφ

A(t, r, ν) ≈ A0 exp

  • −(r − rp)2

4δrr2

p

− (ν − νp)2 4δν

  • ,

S(t, r, ν) ≈ S0(t) + p(t)(r − rp) + P(t)(r − rp)2 + πν(t)(ν − νp)2 + · · · , (ν = cos θ)

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SLIDE 25

Effective Lagrangian:

rp δr δν

Effective theory (2)

L = T − V

T = 1 2A ˙ δ2

r + B ˙

δr ˙ rp + 1 2C ˙ r2

p + 1

2D ˙ δ2

ν,

V µα2

g

= 1 2(αgµrp)2(1 + δr)

  • 1 + δν + 1

4δr + 1 4δν

1 (αgµrp)(1 + δr)

−α−2

g ∞

  • n=2

(−1/2)n (n!)2n

  • N∗

√δrδν(αgµrp)3(1 + δr) n−1 .

Potential

αg = 0.1

N0.02 N0.08

0.0 0.5 1.0 1.5 2.0 2.5 10 5 5

ΑGΜrp VΜΑG

2

ΑG0.1

0.00 0.02 0.04 0.06 0.08 0.10 0.12 0.14 0.0 0.5 1.0 1.5 2.0 2.5 3.0

N ΑGΜrp ΑG0.1

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SLIDE 26

Small oscillations

Oscillation around a equilibrium point ∆qi = (∆δr, ∆δν, αgµ∆rp) Oscillation frequencies

ω2 = 1.141, 0.249, 0.0166,

δq =   0.110 −0.027 0.994   ,   0.075 0.724 0.686   ,   −0.378 −0.005 0.925   .

∆t ≈ 761M

ω2 = 14.06, 5.59, 0.175,

∆t ≈ 26M

∆q =   0.218 −0.030 0.975   ,   0.070 0.927 0.367   ,   −0.640 −0.085 0.763   .

αg = 0.4, N∗ = 1.1 αg = 0.4, N∗ = 1.3

d2(∆qi) dt2 = −

  • j

ωij∆qj

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SLIDE 27

Discussions

Axion cloud model Gravitational waves

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SLIDE 28

GWs emitted in the bosenova (rough estimate)

Assumption:

C1.05 1.08 1.09

2000 4000 6000 8000 10000 20 20 40 60 80

tM E

Qij ∼ r2

pE

Quadrupole approximation Amplitude of generated GWs

h ∼ ¨ Qij robs ∼ 10−7 M robs

Change in the quadrupole moment by the infall of energy in the bosenova

10M

E0 + 1 2(∆E)

  • cos
  • π t

∆t

  • − 1
  • 0.05E0

500M

10−3M

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SLIDE 29

Detectability

Supermassive BH of our galaxy(Sagittarius A*) Solar-mass BH (e.g., Cygnus X-1)

h ∼ ¨ Qij robs ∼ 10−7 M robs

Detectable by the eLISA

hrss ∼ 10−24(Hz)−1/2

below the sensitivity of the KAGRA, Advanced LIGO, Advanced Virgo, etc.

(10−4 Hz) (102 Hz)

Angular frequency

  • f GW

hrss :=

  • |h|2dt

1/2 ∼ 10−16(Hz)−1/2

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SLIDE 30

Summary

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SLIDE 31

Summary

W e developed a reliable code and numerically studied the behaviour of axion field around a rotating black hole. The nonlinear effect enhances the rate of superradiant instability when the amplitude is not very large. Calculation of the gravitational waves emitted in bosenova.

Ongoing studies

The case where axions couple to magnetic fields. The bosenova collapse would happen as a result of superradiant instability.

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SLIDE 32

Appendix

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SLIDE 33

Superradiant instability

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SLIDE 34

Massive scalar fields around a Kerr BH

Metric

ds2 = − ∆ − a2 sin2 θ Σ

  • dt2 − 2a sin2 θ(r2 + a2 − ∆)

Σ dtdφ + (r2 + a2)2 − ∆a2 sin2 θ Σ

  • sin2 θdφ2 + Σ

∆dr2 + Σdθ2

Σ = r2 + a2 cos2 θ,

∆ = r2 + a2 − 2Mr.

Massive scalar field

L = −√−g 1 2gab∇aΦ∇bΦ + U(Φ)

  • ,

∇2Φ − U ′(Φ) = 0

Lagrangian density Klein-Gordon equation

U(Φ) = 1 2µ2f 2

a sin2(Φ/fa)

≃ 1 2µ2Φ2

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SLIDE 35

Massive scalar field around a Kerr BH

Separation of variables Φ = e−iωtR(r)S(θ)eimφ

1 sin θ d dθ sin θdS dθ +

  • −k2a2 cos2 θ −

m2 sin2 θ + Elm

  • S = 0

d dr∆dR dr + K2 ∆ − λlm − µ2r2

  • R = 0

K = (r2 + a2)ω − am

k2 = µ2 − ω2 λlm = Elm + a2ω2 − 2amω

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SLIDE 36

(tortoise coordinate) :

Massive scalar field around a Kerr BH

d dr∆dR dr + K2 ∆ − λlm − µ2r2

  • R = 0

distant region near horizon

R ∼ e±iω∗r∗

  • utgoing

ingoing

r∗

dr∗ = r2 + a2 ∆ dr

ω∗ = ω − ΩHm

Energy flux

P µ = −T µ

νξν

−Pr∗ = ∇r∗Φ∇tΦ ∝ (ω − ΩHm)ω

If , negative energy falls into the black hole

ω < ΩHm

superradiance

R ∼ r−1± µ2−2ω2

k

exp(±kr)

k =

  • µ2 − ω2
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SLIDE 37

Bound state

Matching method WKB method Numerical analysis

Zouros and Eardley, Ann. Phys. 118 (1979), 139. Dolan, PRD76 (2007), 084001. Detweiler, PRD22 (1980), 2323.

Mµ ≃ Mω ≪ 1

Mµ ≫ 1

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SLIDE 38

Ergo-region Barrier region Potential Well Exponential growth region

Potential r*

Black Hole Horizon

“Mirror” at r~1/µ

Bound state

Zouros and Eardley, Ann. Phys. 118 (1979), 139.

r∗

1 r∗

2

r∗

3

ω2

R = u √ r2 + a2 d2u dr2

+

  • ω2 − V (ω)
  • u = 0

V (ω) = ∆µ2 r2 + a2 + 4Mamωr − a2m2 + ∆

  • Elm + (ω2 − µ2)a2

(r2 + a2)2 + ∆ (r2 + a2)3

  • 3r2 − 4Mr + a2 − 3∆r2

r2 + a2

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SLIDE 39

Qualitative discussion on “Bosenova”

Arvanitaki and Dubovsky, PRD83 (2011), 044026.

Nonrelativistic approximation

S =

  • d4x
  • iΨ∗∂tψ − 1

2µ∂iψ∂iψ − µVNψ∗ψ + 1 16f 2

a

(ψ∗ψ)2

  • V (r) ≈ N l(l + 1) + 1

2µr2 − NMµ r − N 2 32πf 2

ar3

Effective potential action

U(Φ) = 1 2µ2f 2

a sin2(Φ/fa)

S =

  • d4x√−g

1 2gab∇aΦ∇bΦ + U(Φ)

  • Φ =

1 √2µ

  • e−iµtψ + eiµtψ∗
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SLIDE 40

Code

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SLIDE 41

Stable simulation cannot be realized in Boyer- Lindquist coordinates.

First difficulty

  • 1
  • 0.5
0.5 1 1.5 2 2.5 3 3.5 4
  • 200
  • 150
  • 100
  • 50
50 100 150 200 ! r*
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SLIDE 42

Stable simulation cannot be realized in Boyer- Lindquist coordinates.

First difficulty

  • 1
  • 0.5
0.5 1 1.5 2 2.5 3 3.5 4
  • 200
  • 150
  • 100
  • 50
50 100 150 200 ! r*

W e use ZAMO coordinates.

˜ t = t, ˜ φ = φ − Ω(r, θ)t, ˜ r = r, ˜ θ = θ,

Ω = dφ dt = uφ ut = − gtφ gφφ = 2Mar (r2 + a2)2 − ∆a2 sin2 θ

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SLIDE 43

r∗ Φ

t/M = 0 ∼ 50

Numerical solution in the ZAMO coordinates

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SLIDE 44

ZAMO coordinates become more and more distorted in the time evolution

Second difficulty

6 4 2 2 4 6 6 4 2 2 4 6 r Cos r Sin t50
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SLIDE 45

ZAMO coordinates become more and more distorted in the time evolution

Second difficulty

W e “pull back” the coordinates

6 4 2 2 4 6 6 4 2 2 4 6 r Cos r Sin t50

t(n) = t, φ(n) = φ − Ω(r, θ)(t − nTP ), r(n) = r, θ(n) = θ.

nTP ≤ t ≤ (n + 1)TP :

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SLIDE 46

Pure ingoing BC at the inner boundary, Fixed BC at the outer boundary

Our 3D code

Space direction:6th-order finite discretization Time direction:4th-order Runge-Kutta Courant number: Pullback: 7th-order Lagrange interpolation

C = ∆t ∆r∗ = 1 20

Grid size:

∆r∗ = 0.5 (M = 1) ∆θ = ∆φ = π/30

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SLIDE 47

r∗ Φ

t/M = 0 ∼ 100

Code check (1)

Comparison with semianalytic solution of the Klein-Gordon case

ω(CF)

I

/µ = 3.31 × 10−7 ω(Numerical)

I

/µ = 3.26 × 10−7

Growth rate ωI = ˙ E 2E ≃ E(100M) − E(0) 200ME(0)

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SLIDE 48
  • 8
  • 7.5
  • 7
  • 6.5
  • 6
  • 5.5
  • 5
  • 4.5
  • 0.35 -0.3 -0.25 -0.2 -0.15 -0.1 -0.05

0.05 0.1 0.15 0.2 Log10(error) Log10!x

E/E0

J/J0

t/M

Code check (2)

Convergence Conserved quantities

(t = 12.5M)

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SLIDE 49

Comparison with BEC

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SLIDE 50

Action

BEC BH-axion

S = N¯ h

  • d3xdt
  • iψ∗ ˙

ψ + 1 2ψ∗∇2ψ − r2 2 ψ∗ψ − g 2(ψ∗ψ)2

  • i ˙

ψ = −1 2∇2ψ + r2 2 ψ + g|ψ|2ψ

Gross-Pitaevskii equation Action

ˆ S =

  • d4x√−g
  • −1

2(∇ϕ)2 − µ2 ϕ2 2 + ˆ UNL(ϕ)

  • ,

Non-relativistic approximation

˜ UNL(x) = −

  • n=2

(−1/2)n (n!)2 xn. ϕ = 1 √2µ

  • e−iµtψ + eiµtψ∗

+αg r ψ∗ψ − µ2 ˜ UNL(|ψ|2/µ)

  • ˆ

SNR =

  • d4x

i 2

  • ψ∗ ˙

ψ − ψ ˙ ψ∗ − 1 2µ∂iψ∂iψ∗

Saito and Ueda, PRA63 (2001), 043601 Action

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SLIDE 51

Effective theory

BEC BH-axion

ψ = A(x, y, z, t)eiφ(x,y,z,t)

A = exp

  • −(

x2 2d2

x(t) +

y2 2d2

y(t) +

z2 2d2

z(t))

  • π3/2dx(t)dy(t)dz(t)

φ = ˙ dx(t) 2dx(t)x2 + ˙ dy(t) 2dy(t)y2 + ˙ dz(t) 2dz(t)z2

dx = dy = dz = r(t)

Spherical case

S = N¯ h 4

  • dt
  • 3 ˙

r2 + 3 ˙ r − f(r)

  • 2

4 6 8 0.5 1 1.5 f!r" r rc

!=#.$!c !=!c !=%.%!c

ψ = A(t, r, ν)eiS(t,r,ν)+imφ

A(t, r, ν) ≈ A0 exp

  • −(r − rp)2

4δrr2

p

− (ν − νp)2 4δν

  • ,

S(t, r, ν) ≈ S0(t) + p(t)(r − rp) + P(t)(r − rp)2 + πν(t)(ν − νp)2 + · · · , N0.02 N0.08

0.0 0.5 1.0 1.5 2.0 2.5 10 5 5

ΑGΜrp VΜΑG

2

ΑG0.1

Saito and Ueda, PRA63 (2001), 043601

(ν = cos θ)

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SLIDE 52

Simulation results

BEC BH-axion

i ˙ ψ = −1 2∇2ψ + r2 2 ψ + g|ψ|2ψ

100 200 300 1 2 3 |!!r="#| t 2.5 2.6

1 2 3 4 200 400 600 800 1000 !peak t/M (a)

Saito and Ueda, PRA63 (2001), 043601 Our simulation results − i 2 L2 2 |ψ|2 + L3 6 |ψ|4

  • ψ
slide-53
SLIDE 53

Green’s function analysis

slide-54
SLIDE 54

m=-1 mode is generated!

Simulation (B)

  • 1
  • 0.5

0.5 1 r*/M ! t = 500M

  • 100
  • 50

50 100 1 2 3 4 5 6

  • 2
  • 1

1 2 3 4

  • 200 -150 -100 -50

50 100 150 200 ! r*/M t = 0 t = 350M t = 700M

Snapshots

MωKG = 0.39

M ˜ ωKG = −0.04 M ˜ ωNL = 0.87 MωNL = 0.35

(Near the horizon)

Φ ∼ e−iωte−i˜

ωr∗

˜ ω = ω − mΩH

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SLIDE 55

Green’s function

(∇2 − µ2)x′G(x, x′) = δ4(x, x′)

Equation

ϕ(x) = ϕ0(x) + ∆ϕ,

ϕ0 = 2Re

  • e(γ−iω0)tP(r)S1

1(cos θ)eiφ

,

Formal solution

BH i t=0 + t, r

r * u=const. =const. r =u *

( ) * i0 i-

Approximation

O(ϕ4

0) is ignored

Green’s function approach (1)

(∇2 − µ2)∆ϕ = J(ϕ0) := −µ2 6 ϕ3

∆ϕ(x) =

  • D′ d4x′

−g(x′)G(x, x′)J(ϕ0(x′))

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SLIDE 56

Green’s function approach (2)

Constructing the Green’s function

BH i t=0 + t, r

r * u=const. =const. r =u *

( ) * i0 i-

ℓm(r, r′) =

1 Wℓmω

  • θ(r − r′)R+

ℓmω(r)R− ℓmω(r′) + θ(r′ − r)R− ℓmω(r)R+ ℓmω(r′)

  • ,

G(x, x′) = 1 (2π)2

  • ℓ,m

−∞

dωGω

ℓm(r, r′)e−iω(t−t′)+im(φ−φ′)Sm ℓ (cos θ) ¯

Sm

ℓ (cos θ′),

Radial function

R+

ℓmω ≃

  • C+

ℓmωeikr/r,

r → ∞; A+

ℓmωei˜ ωr∗ + B+ ℓmωe−i˜ ωr∗,

r ≃ r+, R−

ℓmω ≃

  • A−

ℓmωe−ikr/r + B− ℓmωeikr/r,

r → ∞; C−

ℓmωe−i˜ ωr∗,

r ≃ r+, k =

  • ω2 − µ2, Im[k] ≥ 0

W(R−, R+) = 2i˜ ω(r2

+ + a2)C− ℓmωA+ ℓmω = 2ikC+ ℓmωA− ℓmω.

slide-57
SLIDE 57

! !! m"H

Green’s function approach (3)

Near-horizon solution ∆ϕ =

  • ℓ,m

eimφSm

ℓ (cos θ)

eimΩHr∗ 2i(r2

+ + a2)

×

  • e(3γ−imω0)uDℓm(u, r∗) −

−∞

dω e−iωu ˜ ωA+(ω)

ℓm [3γ + i(ω − mω0)]

E(ω)

ℓm (u, r∗)

  • ,

First term Second term

Pole

ω = mω0 + 3iγ

∼ e−i(mω0+3iγ)t

Pole A

+(ω(ℓmn)

BS

) ℓm

= 0

  • n

(· · ·)e−iω(ℓmn)

BS

t

ω(n)

BS ≃ ±µ ≃ ±ω0 Nonlinear term makes transfer from growing bound state to decaying bound state with negative frequency.

∼ e−i(mω0+3iγ)t