Abstract
The polymer brush bilayer under non-equilibrium shear inversion is studied by
means of MD simulations with Langevin and DPD thermostats. The temporal evo-
lution of the shear stress reveals that there is an overshoot during shear inversion only
with hydrodynamic interactions i.e. DPD. The overshoot in the shear stress takes
place moments after the chains stretch in the opposite shear direction and before the
new stationary shear is established. Nature suppresses this overshoot by an unknown
mechanism which is an open problem for the future researches.