The non-monotonic shear-thinning flow of two strongly cohesive concentrated suspensions
Richard Buscall, Tiara E. Kusuma, Anthony D. Stickland, Sayuri, Rubasingha, Peter J. Scales, Hui-En Teo, Graham L. Worrall

TL;DR
This paper investigates the complex shear flow behavior of two highly cohesive mineral suspensions, revealing non-monotonic flow curves and strain-rate softening effects, with implications for understanding cohesive suspension rheology.
Contribution
It provides a detailed analysis of non-monotonic flow curves in cohesive suspensions, decomposing stress components and linking behavior to strain-rate softening, supported by experimental data.
Findings
Runaway flow occurs above a yield stress in controlled stress mode.
Flow curves exhibit triple-valued regions indicating non-monotonicity.
Solid-phase stress softening explains non-monotonic behavior.
Abstract
The behaviour in simple shear of two concentrated and strongly cohesive mineral suspensions showing highly non-monotonic flow curves is described. Two rheometric test modes were employed, controlled stress and controlled shear-rate. In controlled stress mode the materials showed runaway flow above a yield stress, which, for one of the suspensions, varied substantially in value and seemingly at random from one run to the next, such that the up flow-curve appeared to be quite irreproducible. The down-curve was not though, as neither was the curve obtained in controlled rate mode, which turned out to be triple-valued in the region where runaway flow was seen in controlled rising stress. For this first suspension, the total stress could be decomposed into three parts to a good approximation: a viscous component proportional to a plastic viscosity, a constant isostatic contribution, and a…
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