  The hadronic phase space distributions calculated with the transport model
RQMD for central S(200 AGeV) on S and Pb(160AGeV) on Pb collisions are analyzed
to study the deviations from ideal hydrodynamical evolution. After the
preequilibrium stage, which lasts for approximately 4 (2) fm/c in Pb+Pb (S+S)
the source stays in approximate kinetic equilibrium for about 2 fm/c at a
temperature close to 140 MeV. The interactions of mesons last until around 14
(5) fm/c during which time strong transverse flow is generated. The
interactions in the hadronic resonance gas are not sufficiently strong to
maintain ideal fluid expansion. While pions acquire average transverse fluid
velocities around 0.47-0.58 c, heavier particles like protons and kaons cannot
keep up with the pionic fluid, since their average velocities are smaller by
about 20 to 30 \%. Although kinetic equilibrium breaks down in the final dilute
stage of $AA$ collisions, the system resembles a thermal system at a
temperature of 130 MeV, if the free streaming of hadrons after freeze-out is
suppressed. This freeze-out temperature is consistent with estimates based on
mean free paths and expansion rates in a thermal fireball but lower than values
derived from fits to measured particle ratios and transverse momentum spectra.
The processes in RQMD to which the differences can be attributed to are the
non-ideal expansion of the hadronic matter and the absence of chemical
equilibrium at freeze-out.
