Abstract

Constant-flux gravity currents of viscoplastic fluid remain axisymmetric when extruded onto a dry horizontal plane. However, if the plane is coated with a shallow layer of water, the current suffers a dramatic non-axisymmetric instability in which localized $v$ -shaped cuts appear in the outer edge where the viscoplastic fluid is in contact with water. These ‘fractures’ lengthen and guide the subsequent radial outflow, leading to distinctive flower-like patterns. This pattern formation process is illustrated for two viscoplastic materials, an aqueous suspension of Carbopol, and a mixture of water and joint compound (a kaolin-based, commercially available product). The fracturing spreads over the entire upper surface of the current when deeper water baths are used, complicating the extrusion patterns. The instability can be removed entirely when the ambient water layer is replaced by an immiscible liquid of comparable viscosity, indicating that the presence of water at the surface is key to the pattern formation process. We conjecture that the underlying mechanism is the fracture under tension of the viscoplastic material, exacerbated by the ambient water.

Highlights

  • The viscous gravity current is a classical problem in fluid mechanics, with a number of important applications in the geosciences and engineering

  • For Carbopol extruded into a water layer, the extrusion pattern depends on the ambient water depth Hw, flux Q and rheology

  • Constant-flux gravity currents of viscoplastic fluid remain largely axisymmetric when extruded onto a dry, horizontal plane of Plexiglas

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Summary

Introduction

The viscous gravity current is a classical problem in fluid mechanics, with a number of important applications in the geosciences and engineering. Morris more freely over its base, promoting the extensional stresses (Luu & Forterre 2009; Pegler & Worster 2012; Luu & Forterre 2013; Sayag & Worster 2019a) This second scenario has applications to floating ice shelves or water-lubricated ice streams (MacAyeal & Barcilon 1988; MacAyeal 1989; Pegler, Lister & Worster 2012; Schoof & Hewitt 2013) and the deformation of the Earth’s crust (England & McKenzie 1982, 1983), both of which are more accurately modelled as shear-thinning generalized Newtonian fluids

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