EVOLUTION OF MICROSTRUCTURE DURING SHEAR ALIGNMENT IN A POLYSTYRENE-POLYISOPRENE LAMELLAR DIBLOCK COPOLYMER

The process of flow-induced alignment in a lamellar diblock copolymer melt is investigated using simultaneous measurements of shear stress and birefringence. Flow birefringence, in situ, during oscillatory shear clarifies how the orientation distribution evolves toward either ''parallel'' or ''perpendicular'' alignment, i.e., layers normal to either the velocity gradient or the vorticity axis, respectively. A nearly symmetric, polystyrene-polyisoprene diblock (ODT similar or equal to 164 degrees C) is studied at 120 degrees C (T/T-ODT similar or equal to 0.90). The critical frequency (omega(c)') associated with a crossover in the relaxation dynamics from being dominated by the macromolecular response to being dominated by the microstructural response is estimated to be omega(c)' approximate to 3-7 rad/sat 120 degrees C. At high frequencies (relative to omega(c)'), shearing induces parallel alignment, while shearing at lower frequencies leads to perpendicular alignment. In all cases, alignment proceeds through a ''fast'' process followed by a ''slow'' one. The fast process is dominated by depletion of the projection of the orientation distribution along either the perpendicular direction or the ''transverse'' direction (layers normal to the flow). The resulting biaxial distribution is transformed into a well-aligned uniaxial one during the slow process. Surprisingly, the projection along the perpendicular direction can disappear faster than the projection along the transverse direction. This occurs during the fast process en route to parallel alignment with sufficiently high frequencies. As the shearing frequency is lowered, the projection along transverse orientation decreases faster than that along the perpendicular direction.