Strong Extensional and Shearing Flows of a Branched Polyethylene

Simultaneous fits of the Kaye‐BKZ and Wagner equations to shear and uniaxial extensional flow data are not the most critical tests of these equations, because their memory functions depend on two strain invariants, and this dependence can be varied independently for shear and for uniaxial extension...

Full description

Saved in:
Bibliographic Details
Published inJournal of rheology (New York : 1978) Vol. 33; no. 4; pp. 559 - 578
Main Authors Samurkas, T., Dealy, J. M., Larson, R. G.
Format Journal Article
LanguageEnglish
Published Melville, NY Society of Rheology 01.05.1989
Subjects
Online AccessGet full text

Cover

Loading…
More Information
Summary:Simultaneous fits of the Kaye‐BKZ and Wagner equations to shear and uniaxial extensional flow data are not the most critical tests of these equations, because their memory functions depend on two strain invariants, and this dependence can be varied independently for shear and for uniaxial extension to obtain a fit for each. In planar deformations, however, the memory function depends on only one invariant; this dependence can be measured in single‐step shear experiments, as is reported here for a branched polyethylene, IUPAC X, using a sliding plate rheometer. Predictions are then made for three different planar deformation histories: start‐up of steady simple shear and steady planar extension, and exponentially growing shear, all tests in which the memory function depends on only one invariant. The predictions in steady shear and exponential shear are in rough agreement with the data. The theory for planar extension, however, greatly underpredicts the experimental strain hardening of IUPAC X, which has been reported to be similar to the strain hardening usually seen in uniaxial extension for LDPE. Thus, the Kaye‐BKZ and Wagner single‐integral equations cannot simultaneously describe both strain softening in shear and extreme strain hardening in planar extension using a damping function obtained from one of these flows.
ISSN:0148-6055
1520-8516
DOI:10.1122/1.550028