EXPLORING MOLECULAR-ORIGINS OF SHARKSKIN, PARTIAL SLIP, AND SLOPE CHANGE IN FLOW CURVES OF LINEAR LOW-DENSITY POLYETHYLENE

Citation
Sq. Wang et al., EXPLORING MOLECULAR-ORIGINS OF SHARKSKIN, PARTIAL SLIP, AND SLOPE CHANGE IN FLOW CURVES OF LINEAR LOW-DENSITY POLYETHYLENE, Journal of rheology, 40(5), 1996, pp. 875-898
Citations number
45
Categorie Soggetti
Mechanics
Journal title
ISSN journal
01486055
Volume
40
Issue
5
Year of publication
1996
Pages
875 - 898
Database
ISI
SICI code
0148-6055(1996)40:5<875:EMOSPS>2.0.ZU;2-0
Abstract
This paper explores the molecular mechanism for sharkskin formation on extrudate of linear low density polyethylenes (LLDPE) and investigate s the rheological origin of a characteristic curvature (i.e., a slope change) in the flow curve of LLDPE. Rheological measurements, performe d at various temperatures from 160 to 240 degrees C with a controlled- pressure capillary rheometer and a variety of dies, suggest that the s lope change in the flow curve, interpreted by many as demonstrating wa ll slip in the die land, arises from a combination of interfacial slip and cohesive failure due to chain disentanglement, first initiated on the die wall in the exit region. Since the disentanglement state is u nstable for the adsorbed chains within a certain stress range below th e critical stress for the global stick-slip transition, a partial slip flow cannot sustain itself and occurs only periodically. This time-de pendent molecular entanglement-disentanglement fluctuation produces th e sharkskin like extrudate in the regime where the slope change takes place. Sharkskin dynamics are found to precisely correlate with chain relaxation processes. Specifically, the characteristic time scale tau( i.e., the sharkskin periodicity) is found to be of the same magnitude and have the same WLF (Williams-Landel-Ferry) temperature dependence a s that of the characteristic molecular relaxation time tau as determi ned by oscillatory shear measurements in a parallel-plate flow cell. T he LLDPE resins are also observed to undergo interfacial stick-slip tr ansitions as well as a rarely seen cohesive slip-slip transitions at v arious temperatures. (C) 1996 Society of Rheology.