Distinct-particle pair correlation
Subtracting multiplicity removes each particle paired with itself. The saved event flow vectors determine every plotted correlation.
FR06 · Conditional Bayesian inference
How much does a viscosity estimate depend on the initial state? A viscosity estimate depends on the initial geometry and on correlations that do not come from collective flow. The same saved synthetic events give different conditional posteriors when those assumptions change, so a narrow interval alone cannot establish an unconditional QGP viscosity.
Fit one fixed synthetic event sample under different initial geometries and pair backgrounds. Watch the viscosity posterior move and widen as the assumptions change.
Reading the fixed synthetic event sample.
Brighter areas show higher conditional probability; the dot marks the best fit and the lower strip shows its viscosity marginal.
Gold shows fixed synthetic means and statistical errors; teal shows the selected prediction, with model discrepancy treated in the likelihood.
4,500 synthetic events; 128 particles each; seed 602710. Four identical-angle doublets per event create a known pair background. The four-particle cumulants below use distinct particles and the saved flow vectors. Finite-sample fluctuations and flowing doublets remain.
Uniform priors: viscosity from 0.03 to 0.35; undamped response from 0.25 to 0.44. A 97 by 65 grid integrates both parameters. The data do not change when assumptions change.
Natural units are used. The Gaussian density has unit mean squared radius per axis before deformation. Its short-axis direction defines the elliptic emission plane. This is an assigned response calculation, with no transverse fluid solver.
The response coefficient and damping scale are illustrative. Higher harmonics and nonlinear mode coupling are omitted.
Gardim et al. (2012) · Bilandzic et al. (2011) · Bernhard et al. (2019)
Physics tutorial
BackgroundFit one fixed synthetic event sample under different initial geometries and pair backgrounds. Watch the viscosity posterior move and widen as the assumptions change.
Why it mattersA finite-lived cloud leaves particle directions behind. Inferring its viscosity requires a prediction of how its unknown initial shape becomes those directions.
Start with the essentials
Subtracting multiplicity removes each particle paired with itself. The saved event flow vectors determine every plotted correlation.
Four distinct particles contribute to each four-particle term. Cumulants suppress many pair backgrounds; finite samples and clusters that themselves flow still matter.
The residual compares the same six observed pair means with the selected model. Marginalizing the response amplitude gives the viscosity interval.
Typical misconceptionA narrow posterior fixes the viscosity of real QGP.
Better mental modelThe displayed interval conditions on the chosen response, geometry, priors, and error model. Real extractions also simulate the full collision and compare many observables.
Start with Planted assumptions, then download the event records.
What to observe: The benchmark holds 4,500 events. Its seed and generation parameters travel with the records.Choose Larger ellipticity and compare the shaded interval.
What to observe: The data points stay put. The model and conditional posterior move.Choose Ignore doublets, then Allow model error.
What to observe: A background change shifts the estimate; a larger discrepancy generally broadens the range compatible with the same sample.Heavy-ion matter and hydrodynamics · Reading path
Articles on this path that use this experiment, followed by the other experiments they suggest.