Abstract

Conventionally discussed dynamic mechanisms of elastic strain energy redistribution in near-contact surface regions include P and S elastic wave pulses radiating from the contact surface. At the same time, the elastic strain energy can be transferred by localized vortex-like elastic waves (Rayleigh, Love, Stoneley wave, and so on). In the paper, we numerically studied the main features of the formation and propagation of localized vortex-like waves in the surface layers under the contact zone. The study was done using the numerical method of movable cellular automata. We showed that the initial phase of dynamic contact interaction with a nonzero tangential component of contact velocity is accompanied by the formation of a so-called elastic vortex. The elastic vortex is a fully dynamic object, which is characterized by shear stress concentration and propagates at the shear wave speed. We first revealed the ability of the elastic vortex to propagate toward the bulk of the material and transfer elastic strain energy deep into the surface layer in a localized manner. We analyzed the dependence of the direction of vortex propagation on the tangential contact velocity, contact pressure and Young’s modulus of the material. The results of the study are important for better understanding the dynamic mechanisms contributing to inelastic strain accumulation or gradual degradation of surface layers.

Highlights

  • The contact interaction of dry surface layers of solid bodies is a complex multiscale phenomenon, simultaneously taking place at various spatial scales from atomic to macroscopic [1,2,3,4]

  • Since the energy dissipation of a vortex in a plastically deformable material is capable of ensuring its rapid attenuation [32], in this paper, we considered the “limiting” case of a linearly-elastic material

  • The results show that the interaction of surfaces in mesoscale and macroscale contact areas containing a large number of microscale and submicroscale asperities (Ncont ≈ 103 –104 and more) should lead to the nucleation of elastic vortices characterized by high shear stresses and propagating along the normal to the contact surface

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Summary

Introduction

The contact interaction of dry surface layers of solid bodies is a complex multiscale phenomenon, simultaneously taking place at various spatial scales from atomic to macroscopic [1,2,3,4]. In spite of pronounced differences in the mechanical behavior of surface layers with different internal structures and rheological properties under contact interaction, some fundamental dynamic phenomena are common for various solids and take place at various spatial scales. Collective vortex motions arise near the external and internal boundaries in the material under dynamic loading with a significant lateral (with respect to the plane of the boundary) component. Such conditions are realized, in particular, in the surface regions under conditions of the dynamic contact interaction of solids. In the case of ductile materials, dynamic contact interaction with

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