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软黏附界面中的慢波传播。

Slow wave propagation in soft adhesive interfaces.

机构信息

Center for Materials Processing and Tribology, Purdue University, West Lafayette, IN 47907-2023, USA.

Department of Civil Engineering, Indian Institute of Science, Bangalore 560012, India.

出版信息

Soft Matter. 2016 Nov 16;12(45):9185-9201. doi: 10.1039/c6sm01960a.

DOI:10.1039/c6sm01960a
PMID:27747360
Abstract

Stick-slip in sliding of soft adhesive surfaces has long been associated with the propagation of Schallamach waves, a type of slow surface wave. Recently it was demonstrated using in situ experiments that two other kinds of slow waves-separation pulses and slip pulses-also mediate stick-slip (Viswanathan et al., Soft Matter, 2016, 12, 5265-5275). While separation pulses, like Schallamach waves, involve local interface detachment, slip pulses are moving stress fronts with no detachment. Here, we present a theoretical analysis of the propagation of these three waves in a linear elastodynamics framework. Different boundary conditions apply depending on whether or not local interface detachment occurs. It is shown that the interface dynamics accompanying slow waves is governed by a system of integral equations. Closed-form analytical expressions are obtained for the interfacial pressure, shear stress, displacements and velocities. Separation pulses and Schallamach waves emerge naturally as wave solutions of the integral equations, with oppositely oriented directions of propagation. Wave propagation is found to be stable in the stress regime where linearized elasticity is a physically valid approximation. Interestingly, the analysis reveals that slow traveling wave solutions are not possible in a Coulomb friction framework for slip pulses. The theory provides a unified picture of stick-slip dynamics and slow wave propagation in adhesive contacts, consistent with experimental observations.

摘要

在软黏附表面的滑动中,黏滑一直与慢表面波沙尔拉马赫波的传播有关。最近,通过原位实验证明,另外两种慢波——分离脉冲和滑动脉冲也介导了黏滑(Viswanathan 等人,《软物质》,2016 年,12 卷,5265-5275)。虽然分离脉冲与沙尔拉马赫波一样,涉及局部界面分离,但滑动脉冲是没有分离的移动应力波。在这里,我们在线性弹性动力学框架中对这三种波的传播进行了理论分析。根据是否发生局部界面分离,应用了不同的边界条件。结果表明,伴随慢波的界面动力学由一个积分方程系统控制。获得了界面压力、剪切应力、位移和速度的封闭形式解析表达式。分离脉冲和沙尔拉马赫波自然地作为积分方程的波解出现,传播方向相反。在线性弹性是物理有效近似的应力状态下,发现波传播是稳定的。有趣的是,分析表明在滑动脉冲的库仑摩擦框架中,不可能存在慢行波解。该理论提供了黏附接触中黏滑动力学和慢波传播的统一图像,与实验观察一致。

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