Issue |
J. Phys. I France
Volume 6, Number 2, February 1996
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Page(s) | 237 - 244 | |
DOI | https://doi.org/10.1051/jp1:1996145 |
J. Phys. I France 6 (1996) 237-244
Multiphase Coexistence and Non-linear Rheology of Colloidal. Dispersions as Observed in a Model Capillary Viscosimeter
Thomas Palberg and Mathias WürthUniversity of Konstanz, Faculty of Physics, Postfach 5560 M675, 78434 Kontanz, Germany
(Received 13 July 1995, revised 26 October 1995, accepted 6 November 1995)
Abstract
Investigations of the flow properties of colloidal substances by viscometry and
rheometry are a
valuable tool in understanding many transport processes of importance in biology, medicine and
industrial treatment of materials. The streaming of cytoplasm, blood, micellar solutions or crude
oil emulsions are but some obvious examples. One of the most intriguing properties of colloidal
systems is their ability of thinning or thickening under shear. To characterise this non-Newtonian
flow behaviour different visco- and rheometric experiments have been devised, the capillary
viscometer being one of the classical instruments. The underlying physical mechanisms of non-linear
rheometry are the shear-induced formation and destruction of long range positional and
orientational order. Since only in rare cases comprehensive structure and velocity information is
accessible from inside a viscosimeter, generally, homogeneous samples are assumed. However, there
are indications of a geometry dependent evolution of inhomogeneous phase and flow behaviour from
recent experiments on colloidal model systems, in particular for denser systems of strongly
interacting particles. We here present investigations performed on a well characterised suspension
of spherical particles interacting via a screened electrostatic potential. We give a detailed
study of the local structures and shear rates in an optical model capillary viscosimeter. As a
function of the overall flux several different flow scenarios are observed within the viscosimeter
and the most striking feature is the simultaneous existence of up to four concentrically arranged
phases under conditions of stationary flow.
© Les Editions de Physique 1996