Journal of Rheology · 1993 · 47 citations · 0 references
Natural SciencesMaterials EngineeringMaterials SciencePolymer ChemistryPolymer MaterialsRheologyPolymer CharacterizationPolymer MorphologyPolymer Physical ChemistryPolymer PhysicsPolymer RheologyPolymer ThermodynamicsGlass TransitionGlass Transition TemperatureLiquid Crystalline PolymersRheological BehaviorRheological CharacterizationRheometer MeasurementsSolution PolymerizationThermotropic Liquid Crystals
The transient rheological responses upon startup of shear flow were investigated for a well-characterized thermotropic liquid-crystalline polymer in the nematic region using a cone-and-plate rheometer. For the study, an aromatic polyester, poly[(phenyl sulfonyl)-p-phenylene 1,10-decamethylene-bis(4-oxybenzoate)] (PSHQ10), was synthesized via solution polymerization in our laboratory. The PSHQ10 was found via gel permeation chromatography to have the weight-average molecular weight of 45 000 relative to polystyrene standards and a polydisperity index of 2, and via differential scanning calorimetry to have (a) a glass transition temperature of 88 °C; (b) a melting point of 115 °C; and (c) a nematic–isotropic transition temperature (TNI) of 175 °C. The initial morphology (i.e., initial conditions) for the startup of shear flow of PSHQ10 in the nematic region was controlled by first heating a solvent-cast specimen to 190 °C (i.e., to the isotropic region), shearing at a rate of 0.085 s−1 for 5 min, and then cooling slowly down to a predetermined temperature in the nematic state (i.e., 130, 140, 150, or 160 °C). A fresh specimen was employed for each transient experiment, and the growths of shear stress σ+(t,γ̇) and first normal stress difference N1+(t,γ̇) were recorded as functions of time (t) for shear rates (γ̇) ranging from 0.107 to 1.07 s−1 and for temperatures ranging from 130 to 160 °C. It was found that thermal and deformation histories could be erased, and large overshoots in σ+(t,γ̇) and N1+(t,γ̇) were observed with only positive steady-state normal stress difference existing for all temperatures.