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S C O T T
PRATT
M I C H I G A NSTATE
U N I V E R S I Y
T S U N A M I
THE
B TPUZZLE
AND
T H E
R H I C
Scott Pratt The HBT Puzzle and the RHIC Tsunami The HBT Puzzle and the RHIC Tsunami Michigan State University
OUTLINE
• What does HBT Measure?• Models• HBT and the Equation of State
– Dynamical Signatures– Entropy
• Tsunamis, EoS & Viscosity
Scott Pratt The HBT Puzzle and the RHIC Tsunami The HBT Puzzle and the RHIC Tsunami Michigan State University
What does HBT measure?
Determines Shape of f(p,r,t)
Scott Pratt The HBT Puzzle and the RHIC Tsunami The HBT Puzzle and the RHIC Tsunami Michigan State University
HBT Basics
Rout ≈Rside + vΔτ
Rlong
Rside
Scott Pratt The HBT Puzzle and the RHIC Tsunami The HBT Puzzle and the RHIC Tsunami Michigan State University
Blast-Wave Models
Rvz=z/τ
Vx=V(r/R)
Parameters: T, R, V , τ, Δτ
Schnedermann, Sollfrank and HeinzTomasik, Broniowski,Lisa and Retiere,…
Scott Pratt The HBT Puzzle and the RHIC Tsunami The HBT Puzzle and the RHIC Tsunami Michigan State University
Blast Wave Fits
QuickTime™ and aTIFF (Uncompressed) decompressor
are needed to see this picture.
Lisa and Retiere, PRC 70:044907 (04)
QuickTime™ and aTIFF (Uncompressed) decompressor
are needed to see this picture.
TherminatorBroniowski et al., nucl-th/0212053
Scott Pratt The HBT Puzzle and the RHIC Tsunami The HBT Puzzle and the RHIC Tsunami Michigan State University
NA49 vs. Therminator
3-dimensional details of blast-wave confirmed
Scott Pratt The HBT Puzzle and the RHIC Tsunami The HBT Puzzle and the RHIC Tsunami Michigan State University
Blast-Wave and the HBT Puzzle
Parameters:T 110 MeVR 13 fmV 0.7c τ 10 fm/c Δτ 3 fm/c
Similar Conclusions:Blast Waves (Lisa-Retiere, Tomasik)TherminatorBuda Lund
Requires Kp spectra
Rapid expansionsudden disintegration
Scott Pratt The HBT Puzzle and the RHIC Tsunami The HBT Puzzle and the RHIC Tsunami Michigan State University
HYDRO
Overall sizes depend on EOS & breakup criteria
Scott Pratt The HBT Puzzle and the RHIC Tsunami The HBT Puzzle and the RHIC Tsunami Michigan State University
Cascade/Boltzmann
More resonances -> softer -> biggerStrings -> softer -> bigger
Scott Pratt The HBT Puzzle and the RHIC Tsunami The HBT Puzzle and the RHIC Tsunami Michigan State University
HBT and the EoS: Dynamical Signature
Leads to: Rout/Rside >> 1
Scott Pratt The HBT Puzzle and the RHIC Tsunami The HBT Puzzle and the RHIC Tsunami Michigan State University
HBT and EoS: Entropy
f (rp)≡
d3r[ f(rp,
rr )]2∫
d3r f(rp,
rr )∫
=π 3/2
(2S+1)dN / d3p
RoutRlongRside
Sizes and spectra give phase space density
Phase space density gives Entropy
dS
dy≅2π ptdpt E∫
dNd3p
52−32
ln(2)−ln[ f (pt)] ±123/2
f (pt)⎡⎣⎢
⎤⎦⎥
Scott Pratt The HBT Puzzle and the RHIC Tsunami The HBT Puzzle and the RHIC Tsunami Michigan State University
HBT and EoS:Entropy
• <f> increases with s1/2
• gives entropy for pions• Rinv and spectra for other species gives total S
Scott Pratt The HBT Puzzle and the RHIC Tsunami The HBT Puzzle and the RHIC Tsunami Michigan State University
Is Lattice Eq. of State excluded?
Range
Scott Pratt The HBT Puzzle and the RHIC Tsunami The HBT Puzzle and the RHIC Tsunami Michigan State University
Total Entropy and the lattice EOS
• Final S consistent with lattice EOS• CRUDE!• Entropy moved from pions to baryons
Scott Pratt The HBT Puzzle and the RHIC Tsunami The HBT Puzzle and the RHIC Tsunami Michigan State University
The HBT puzzle
• Models that fit overall volume (fit entropy)underpredict Rside
Scott Pratt The HBT Puzzle and the RHIC Tsunami The HBT Puzzle and the RHIC Tsunami Michigan State University
Explanations to the HBT Puzzle
• Refraction (Cramer-Miller, 2005)
- Requires extreme assumptions
• Surface Emission (Heiselberg, 2002)
- What happened to energy in center?
• Initial transverse velocity (Sinyukov, 2007)
- Source ???
Needed: Explanation with consistent dynamical model
Scott Pratt The HBT Puzzle and the RHIC Tsunami The HBT Puzzle and the RHIC Tsunami Michigan State University
Tsunamis at RHIC
vwave = gh
(Bauer and Bertsch, PRL '90)
Scott Pratt The HBT Puzzle and the RHIC Tsunami The HBT Puzzle and the RHIC Tsunami Michigan State University
Modeling Tsunamis at RHIC with Hydrodynamics
Pcs2 =dP
d
H
L
cs2 =0.3
cs2 =constant
Increasing L or decreasing c2mixed -> stronger
tsunami
Resonance Gas
Scott Pratt The HBT Puzzle and the RHIC Tsunami The HBT Puzzle and the RHIC Tsunami Michigan State University
HydrodynamicEvolution
L=2 GeV/fm3,c2
mixed=0.05
τ=1,3,5,7,9,11 fm/c
Scott Pratt The HBT Puzzle and the RHIC Tsunami The HBT Puzzle and the RHIC Tsunami Michigan State University
HBT Radii cmixed2 =0.05
cmixed2 =0.15
Large Rside
for L2 GeV/fm3
Scott Pratt The HBT Puzzle and the RHIC Tsunami The HBT Puzzle and the RHIC Tsunami Michigan State University
Viscosity and Tsunamis:
Txx =Tyy =Tzz =PPerfect Hydro:
Navier-Stokes: Tzz =P−η(2∂zvz−∂xvx−∂yvy)−B∇gv
Israel-Stewart: ∂tTij = −(1 / τ )(Tij −TijN .S .)
Scott Pratt The HBT Puzzle and the RHIC Tsunami The HBT Puzzle and the RHIC Tsunami Michigan State University
Initial-State Asymmetry of Tij
Relativistic Gas:
Classical Longitudinal Fields:
Txx =Tyy =Tzz = / 3
Txx =Tyy =Tzz =−
CGC (Krasnitz, Nara &Venugopalan) : Txx =Tyy ≈ / 2Tzz ≈0
For τ=0.5 fm/c -> Significant strengthening of tsunami
Scott Pratt The HBT Puzzle and the RHIC Tsunami The HBT Puzzle and the RHIC Tsunami Michigan State University
Non-Zero Shear
Even for η s/4π
-> significant strengthening of tsunami
Scott Pratt The HBT Puzzle and the RHIC Tsunami The HBT Puzzle and the RHIC Tsunami Michigan State University
Bulk Viscosity in Mixed RegionK.Paech and S.P., PRC 2006
P
P−B∇gv
-> Significant strengthening of tsunami
Scott Pratt The HBT Puzzle and the RHIC Tsunami The HBT Puzzle and the RHIC Tsunami Michigan State University
Summary
• HBT invaluable for investigating EoS:- HBT + spectra -> entropy
• Large experimental Rside might indicate tsunami- Driven by Softness in EoS and viscosity
• More serious analysis is needed
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