Pressure variation during the coextrusion of two low density polyethylene melts was investigated. Melt streams were delivered to ad ie from two separate extruders to converge in a 3088 geometry to form atwo layer extrudate. Melt flow in the confluent region and die land to the die exit was observed through side windows of av isualisation cell. Stream velocity ratio was varied by control of extruder screw speeds. Layer thickness ratios producing wave type interfacial instability were quantified for each melt coextruded on itself and for the combined melts. Stream pressures and screw speeds were monitored and analysed.W ave type interfacial instability was present during the processing of the melts at specific, repeatable, stream layer ratios. Increased melt elasticity appeared to promote this type of instability. Analysis of process data indicates little correlation between perturbations in extruder screw speeds and stream pressures. The analysis did however show covariance between the individual stream pressure perturbations. Interestingly there was significant correlation even when interfacial instability was not present. We conclude that naturally occurring variation in extruder screw speeds do not perturb stream pressures and, more importantly, natural perturbations in stream pressures do not promote interfacial instability.
1I ntroductionCoextruding stratified layers of polymer melts is ac omplex process. Indeed, in coextrusion flows melt streams are constrained not only by metal die walls but also at least one moving boundary in the form of stream interfaces, and the moving interface is often formed between melts with different thermal and strain history dependent viscoelastic properties. Streamline curvature also tends to vary in ac omplex manner throughout the flow at regions of confluence. It is not unusual for this type of flow to give rise to interfacial instability.Two distinct types of \ interfacial instability" are associated with the unsteady-state distortion of the interface of co-joining melt streams. These instabilities are covered in the seminal work of Ramanathan and Shrenk