Colloidal probe Atomic Force Microscopy (AFM) allows to explore sliding states of vanishing friction, i.e. superlubricity, in mesoscopic graphite contacts. In this respect, superlubricity is known to appear upon formation of a triboinduced transfer layer, originated by material transfer of graphene flakes from the graphitic substrate to the colloidal probe. It was suggested that friction vanishes due to crystalline incommensurability at the sliding interface thus formed. However several details are missing, including the roles of tribolayer roughness and of loading conditions. Hereafter we gain deeper insight into the tribological response of micrometric silica beads sliding on graphite under ambient conditions. We show that the tribotransferred flakes increase interfacial roughness from tenths to several nanometers, in fact causing a breakdown of adhesion and friction by one order of magnitude. Furthermore, they behave as protruding asperities dissipating mechanical energy via atomic-scale stick-slip instabilities. Remarkably, such contact junctions can undergo a load-driven transition from continuous superlubric sliding to dissipative stick-slip, that agrees with the single-asperity Prandtl-Tomlinson model. Our results indicate that friction at mesoscopic silica-graphite junctions depends on the specific energy landscape experienced by the topographically-highest triboinduced nanoasperity. Superlubricity may arise from the load-controlled competition between interfacial crystalline incommensurability and contact pinning effects.
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