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由摩擦诱导石墨转移层包覆的胶体原子力显微镜探针的滑动摩擦与超润滑性

Sliding Friction and Superlubricity of Colloidal AFM Probes Coated by Tribo-Induced Graphitic Transfer Layers.

作者信息

Buzio Renato, Gerbi Andrea, Bernini Cristina, Repetto Luca, Vanossi Andrea

机构信息

CNR-SPIN, C.so F.M. Perrone 24, Genova16152, Italy.

Dipartimento di Fisica, Università degli Studi di Genova, Via Dodecaneso 33, Genova16146, Italy.

出版信息

Langmuir. 2022 Oct 18;38(41):12570-12580. doi: 10.1021/acs.langmuir.2c02030. Epub 2022 Oct 3.

Abstract

Colloidal probe atomic force microscopy (AFM) allows us to explore sliding friction phenomena in graphite contacts of nominal lateral size up to hundreds of nanometers. It is known that contact formation involves tribo-induced material transfer of graphite flakes from the graphitic substrate to the colloidal probe. In this context, sliding states with nearly vanishing friction, i.e., superlubricity, may set in. A comprehensive investigation of the transfer layer properties is mandatory to ascertain the origin of superlubricity. Here we explore the friction response of micrometric beads, of different size and pristine surface roughness, sliding on graphite under ambient conditions. We show that such tribosystems undergo a robust transition toward a low-adhesion, low-friction state dominated by mechanical interactions at one dominant tribo-induced nanocontact. Friction force spectroscopy reveals that the nanocontact can be superlubric or dissipative, in fact undergoing a load-driven transition from dissipative stick-slip to continuous superlubric sliding. This behavior is excellently described by the thermally activated, single-asperity Prandtl-Tomlinson model. Our results indicate that upon formation of the transfer layer, friction depends on the energy landscape experienced by the topographically highest tribo-induced nanoasperity. We consistently find larger dissipation when the tribo-induced nanoasperity is slid against surfaces with higher atomic corrugation than graphite, like MoS and WS, in prototypical van der Waals layered heterojunctions.

摘要

胶体探针原子力显微镜(AFM)使我们能够探究标称横向尺寸达数百纳米的石墨接触中的滑动摩擦现象。已知接触形成过程涉及石墨薄片从石墨基底向胶体探针的摩擦诱导材料转移。在此背景下,可能会出现摩擦力几乎消失的滑动状态,即超润滑状态。对转移层特性进行全面研究对于确定超润滑的起源至关重要。在这里,我们探究了在环境条件下,不同尺寸和原始表面粗糙度的微米级珠子在石墨上滑动时的摩擦响应。我们表明,此类摩擦系统会经历向低粘附、低摩擦状态的稳健转变,这种状态由一个主要的摩擦诱导纳米接触处的机械相互作用主导。摩擦力谱表明,纳米接触可以是超润滑的或耗散的,实际上会经历从耗散的粘滑到连续超润滑滑动的载荷驱动转变。热激活的单峰普朗特 - 汤姆林森模型能很好地描述这种行为。我们的结果表明,在转移层形成后,摩擦力取决于地形上最高的摩擦诱导纳米峰所经历的能量景观。我们一致发现,在典型的范德华层状异质结中,当摩擦诱导纳米峰与比石墨具有更高原子起伏的表面(如MoS和WS)相对滑动时,会有更大的耗散。

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