K
Kenneth Walters
Researcher at Aberystwyth University
Publications - 77
Citations - 3513
Kenneth Walters is an academic researcher from Aberystwyth University. The author has contributed to research in topics: Newtonian fluid & Rheometer. The author has an hindex of 31, co-authored 76 publications receiving 3347 citations.
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Elastico-viscous squeeze films: Part 2. superimposed rotation
TL;DR: In this paper, it is shown that the Part 1 concentration on the half-time t 1 2 sometimes hides interesting elastico-viscous effects, since these are most pronounced at short times after the load is applied.
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A critical re-appraisal of the jet-thrust technique for normal stresses, with particular reference to axial velocity and stress rearrangement at the exit plane
TL;DR: In this article, it was shown that the axial velocity and axial stress re-arrangement is the major cause of the reduction in measured thrust from the expected value of a jet on the tube from which it flows, and the corresponding die-swell ratio.
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Computations with viscoplastic and viscoelastoplastic fluids
TL;DR: In this article, the authors explored the viscoplastic regime with regularised Bingham-type and viscoelastoplastic fluids, performing simulations for 4:1:4 contraction-expansion flow with a hybrid finite element-finite volume subcell scheme.
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Interfacial effects in the flow of viscous and elasticoviscous liquids
TL;DR: In this paper, a technique of flow visualization by means of an expanded laser beam and trace amounts of particulate additives is used to study the behavior of newtonian and non-newtonian elastic liquids in complex geometries.
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The Stability of the Flow of an Elastico-Viscous Liquid in a Curved Channel
R. H. Thomas,Kenneth Walters +1 more
TL;DR: In this paper, the stability of the flow of an idealized elastico-viscous liquid in a narrow curved channel, the motion being due to a pressure gradient acting around the channel, was investigated and the main effect of the elasticity of the liquid is to lower the value of the critical Reynolds number at which instability occurs.