zimányi winter school, 2013/12/05 csörgő, t. 1 observables and initial conditions from exact...

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Zimányi Winter School, 2013/12/05 Csörgő, T. 1 Observables and initial conditions from exact rotational hydro solutions T. Csörgő 1 , I. Barna 1 and M.I. Nagy 1,3 1 MTA Wigner Research Center for Physics, RMKI 3 ELTE University, Budapest, Hungary Continuation: observables Two different family of equations of state Single particle spectra Elliptic and higher order flows Oscillations of HBT radii What have we learnt? Summary Manuscript in preparation arXiv:1309.4390v2

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Page 1: Zimányi Winter School, 2013/12/05 Csörgő, T. 1 Observables and initial conditions from exact rotational hydro solutions T. Csörgő 1, I. Barna 1 and M.I

                       

Zimányi Winter School, 2013/12/05 Csörgő, T.1

Observables and initial conditions from exact rotational hydro solutions

T. Csörgő 1 , I. Barna 1 and M.I. Nagy 1,3

1 MTA Wigner Research Center for Physics, RMKI3 ELTE University, Budapest, Hungary

Continuation: observablesTwo different family of equations of state

Single particle spectraElliptic and higher order flows

Oscillations of HBT radiiWhat have we learnt?

Summary

Manuscript in preparationarXiv:1309.4390v2

Page 2: Zimányi Winter School, 2013/12/05 Csörgő, T. 1 Observables and initial conditions from exact rotational hydro solutions T. Csörgő 1, I. Barna 1 and M.I

                       

Zimányi Winter School, 2013/12/05 Csörgő, T.2

Rotated Gaussian solutions

Note: (r’, k’) in fireball frame rotated wrt lab frame (r,k)

Note: in this talk, rotation in the (X,Z) impact parameter plane !

Page 3: Zimányi Winter School, 2013/12/05 Csörgő, T. 1 Observables and initial conditions from exact rotational hydro solutions T. Csörgő 1, I. Barna 1 and M.I

                       

Zimányi Winter School, 2013/12/05 Csörgő, T.3

Role of EoS on acceleration

Lattice QCD type Eos is explosive

Tilt angle q integrates rotation in (X,Z) plane: sensitive to EoS!

Page 4: Zimányi Winter School, 2013/12/05 Csörgő, T. 1 Observables and initial conditions from exact rotational hydro solutions T. Csörgő 1, I. Barna 1 and M.I

                       

Zimányi Winter School, 2013/12/05 Csörgő, T.4

Single particle spectra

In the rest frame of the fireball:

Rotation increases effective temperatures both in the

longitudinal and impact parameter direction

in addition to Hubble flows

Page 5: Zimányi Winter School, 2013/12/05 Csörgő, T. 1 Observables and initial conditions from exact rotational hydro solutions T. Csörgő 1, I. Barna 1 and M.I

                       

Zimányi Winter School, 2013/12/05 Csörgő, T.5

Directed, elliptic and other flows

Note: model is fully analytic

As of now, only X = Z = R(t)spheroidal solutions are found

→ vanishing odd order flows

See next talk for fluctuations

From the single particle spectra→ flow coefficents vn

Page 6: Zimányi Winter School, 2013/12/05 Csörgő, T. 1 Observables and initial conditions from exact rotational hydro solutions T. Csörgő 1, I. Barna 1 and M.I

                       

Zimányi Winter School, 2013/12/05 Csörgő, T.6

Reminder: Universal w scaling of v2

Notes: Rotation does not change thisJust modifiesRadial flow parameters

See +for more details

Page 7: Zimányi Winter School, 2013/12/05 Csörgő, T. 1 Observables and initial conditions from exact rotational hydro solutions T. Csörgő 1, I. Barna 1 and M.I

                       

Zimányi Winter School, 2013/12/05 Csörgő, T.7

HBT radii for rotating spheroids

New terms with blue → Rotation decreases HBT radii similarly to Hubble flow.

Diagonal Gaussians in natural frame

Page 8: Zimányi Winter School, 2013/12/05 Csörgő, T. 1 Observables and initial conditions from exact rotational hydro solutions T. Csörgő 1, I. Barna 1 and M.I

                       

Zimányi Winter School, 2013/12/05 Csörgő, T.8

HBT radii in the lab frame

HBT radii without flow

But spheriodal symmetry of the solutionMakes several cross terms vanish → need for ellipsoidal solutions

Page 9: Zimányi Winter School, 2013/12/05 Csörgő, T. 1 Observables and initial conditions from exact rotational hydro solutions T. Csörgő 1, I. Barna 1 and M.I

                       

Zimányi Winter School, 2013/12/05 Csörgő, T.9

HBT radii in the lab frame

HBT radii without flow

But spheriodal symmetry of the solutionMakes several cross terms vanish → need for ellipsoidal solutions

Page 10: Zimányi Winter School, 2013/12/05 Csörgő, T. 1 Observables and initial conditions from exact rotational hydro solutions T. Csörgő 1, I. Barna 1 and M.I

                       

Zimányi Winter School, 2013/12/05 Csörgő, T.10

Qualitatively rotation and flow similar

But need more time dependent calculations

and less academic studies(relativistic solutions)

Page 11: Zimányi Winter School, 2013/12/05 Csörgő, T. 1 Observables and initial conditions from exact rotational hydro solutions T. Csörgő 1, I. Barna 1 and M.I

                       

Zimányi Winter School, 2013/12/05 Csörgő, T.11

Summary

Observables calculated

Effects of rotation and flowCombine and have same mass dependence

Spectra: slope increasesv2: universal w scaling remains valid

HBT radii:Decrease with mass intensifies

Even for spherical expansions:v2 from rotation.

Picture: vulcanoHow to detect the rotation?

Next step: penetrating probes

Page 12: Zimányi Winter School, 2013/12/05 Csörgő, T. 1 Observables and initial conditions from exact rotational hydro solutions T. Csörgő 1, I. Barna 1 and M.I

                       

Zimányi Winter School, 2013/12/05 Csörgő, T.12

Summary

Observables calculated

Effects of rotation and flowCombine and have same mass dependence

Spectra: slope increasesv2: universal w scaling remains valid

HBT radii:Decrease with mass intensifies

Even for spherical expansions:v2 from rotation.

Picture: vulcanoHow to detect the rotation?

Next step: penetrating probes