Understanding
friction at diamond–rock interfaces is crucial
to increase the energy efficiency of drilling operations. Harder rocks
usually are usually more difficult to drill; however, poor performance
is often observed for polycrystalline diamond compact (PDC) bits on
soft calcite-containing rocks, such as limestone. Using macroscale
tribometer experiments with a diamond tip, we show that soft limestone
rock (mostly calcite) gives much higher friction coefficients compared
to hard granite (mostly quartz) in both humid air and aqueous environments.
To uncover the physicochemical mechanisms that lead to higher kinetic
friction at the diamond–calcite interface, we employ nonequilibrium
molecular dynamics simulations (NEMD) with newly developed reactive
force field (ReaxFF) parameters. In the NEMD simulations, higher friction
coefficients are observed for calcite than quartz when water molecules
are included at the diamond–rock interface. We show that the
higher friction in water-lubricated diamond–calcite than diamond–quartz
contacts is due to increased interfacial bonding in the former. For
diamond–calcite, the interfacial bonds mostly form through
chemisorbed water molecules trapped between the tip and the substrate,
while mainly direct tip–surface bonds form inside diamond–quartz
contacts. For both rock types, the rate of interfacial bond formation
increases exponentially with pressure, which is indicative of a stress-augmented
thermally activated process. The friction force is shown to be linearly
dependent on the number of interfacial bonds during steady-state sliding.
The agreement between the friction behavior observed in the NEMD simulations
and tribometer experiments suggests that interfacial bonding also
controls diamond–rock friction at the macroscale. We anticipate
that the improved fundamental understanding provided by this study
will assist in the development of bit materials and coatings to minimize
friction by reducing diamond–rock interfacial bonding.