Abstract

Rubber friction on ice is studied both experimentally and theoretically. The friction tests involve three different rubber tread compounds and four ice surfaces exhibiting different roughness characteristics. Tests are carried out at four different ambient air temperatures ranging from $$-5$$ to $$-13\,^{\circ }\hbox {C}$$ , under three different nominal pressures ranging from 0.15 to $$0.45\,\hbox {MPa}$$ , and at the sliding speed 0.65 m/s. The viscoelastic properties of all the rubber compounds are characterized using dynamic mechanical analysis. The surface topography of all ice surfaces is measured optically. This provides access to standard roughness quantities and to the surface roughness power spectra. As for modeling, we consider two important contributions to rubber friction on ice: (1) a contribution from the viscoelasticity of the rubber activated by ice asperities scratching the rubber surface and (2) an adhesive contribution from shearing the area of real contact between rubber and ice. At first, a macroscopic empirical formula for the friction coefficient is fitted to our test results, yielding a satisfactory correlation. In order to get insight into microscopic features of rubber friction on ice, we also apply the Persson rubber friction and contact mechanics theory. We discuss the role of temperature-dependent plastic smoothing of the ice surfaces and of frictional heating-induced formation of a meltwater film between rubber and ice. The elaborate model exhibits very satisfactory predictive capabilities. The study shows the importance of combining advanced testing and state-of-the-art modeling regarding rubber friction on ice.

Highlights

  • Friction on ice has been studied for many years [3, 4, 6, 14, 15, 28]

  • When a water film separates the sliding surfaces, the frictional shear stress is proportional to the small viscosity of water, such that the adhesive contribution to friction is in most cases negligible compared to the viscoelastic contribution

  • We have measured the friction force acting on rubber blocks sliding along ice surfaces at different background temperatures, different nominal contact pressures, and at a sliding speed which is representative for braking with an antilock braking system

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Summary

Introduction

Friction on ice has been studied for many years [3, 4, 6, 14, 15, 28]. We here focus on rubber friction on ice, a topic of great practical importance when it comes to grip of tires on icy road surfaces [9]. When a rubber block is sliding on an ice surface, friction will result largely from two processes, namely (1) from viscoelastic deformation of rubber activated by interactions with ice asperities [16, 23], referred to as viscoelastic contribution to friction, and (2) from shearing the area of real contact [4], referred to as adhesive contribution to friction. As for the latter contribution, it is important whether or not a thin meltwater film forms in the area of contact. If no meltwater film is produced, the frictional shear stress results from the adhesive interaction between the ice surface and the rubber molecules at the sliding interface [27, 30], and the adhesive ice-rubber interaction will give an important contribution to the friction force

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