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Particle motion in the fountain flow region during filling of a tube with a viscoelastic fluid
Author(s) -
Kolli Venkata Giri,
Ogadhoh Shem O.,
Abel Steve M.,
GadalaMaria Francis,
Papathanasiou Thanasis D.
Publication year - 2002
Publication title -
polymer engineering and science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.503
H-Index - 111
eISSN - 1548-2634
pISSN - 0032-3888
DOI - 10.1002/pen.10958
Subject(s) - viscoelasticity , mechanics , particle (ecology) , fountain , free surface , materials science , magnetosphere particle motion , flow (mathematics) , newtonian fluid , tube (container) , classical mechanics , physics , composite material , geology , oceanography , archaeology , quantum mechanics , magnetic field , history
We present the results of an investigation of particle motion behind the advancing free surface during the filling of an initially empty tube with a viscoelastic fluid. Particle motion in the vicinity of an advancing free surface (the fountain flow region) is of significance in a number of processes used to form composite materials, notably injection and compression molding. This motion determines, to a large extent, the distribution of the reinforcing phase in the molded part. We show experimentally that an isolated spherical particle moves behind the interface in characteristic orbits, remaining in close proximity to the advancing free surface. This is in stark contrast to what happens in a Newtonian fluid. In that case, the particle is deposited on the tube walls by the fountain flow and never again reaches the faster moving free surface. The particle motion behind the interface is modeled with a combination of equations that describe the advection of the particle due to convective/fountain flow and its lateral migration due to viscoelasticity. This model neglects the finite size of the particle and is thus unable to capture the full details of the observed motion. However, the qualitative agreement between the experimental results and the modeling predictions suggests that the observed particle motion is the result of the combined effect of viscoelasticity and fountain flow.