13.07.2015 Views

Friction and energy dissipation mechanisms in adsorbed molecules ...

Friction and energy dissipation mechanisms in adsorbed molecules ...

Friction and energy dissipation mechanisms in adsorbed molecules ...

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

Advances <strong>in</strong> Physics 203Downloaded by [North Carol<strong>in</strong>a State University] at 09:24 22 April 2013<strong>in</strong> contact-mode images is now attributed to the effect of atomic lattice stick–slip motion, whichis ever-present <strong>in</strong> AFM experimental studies [264] <strong>and</strong> <strong>in</strong>tr<strong>in</strong>sically reflects the stiffness of thedevice. It also represents a major departure from the viscous friction law (Equation (2)) thatgoverns the films <strong>adsorbed</strong> <strong>in</strong> the unconf<strong>in</strong>ed geometries discussed so far. Static friction <strong>and</strong>stick–slip phenomenon are ubiquitous for the AFM geometry, <strong>and</strong> <strong>in</strong> the vast majority of cases,one stick–slip event is observed per unit cell of the substrate. This is true even <strong>in</strong> cases where theatomic cell conta<strong>in</strong>s more than one species. <strong>Friction</strong> levels <strong>and</strong> stick–slip phenomena thus exhibitvery strong dependencies on the direction that the tip moves with respect to the crystall<strong>in</strong>e axesof the substrate (Figure 30). At the macroscopic scale, macroscopic contacts between solids, <strong>in</strong>general, obey Amontons law, Equation (1), <strong>and</strong> exhibit friction that is <strong>in</strong>dependent of velocity.For AFM contact sizes <strong>in</strong> the nanometer range, friction has been reported to <strong>in</strong>crease, decrease,or be <strong>in</strong>dependent of slid<strong>in</strong>g velocity. A logarithmic <strong>in</strong>crease of friction with scann<strong>in</strong>g velocitywas reported, for example, [265], for polymer layers grafted on silica over a range of velocities<strong>and</strong> with four different probes. A thermally activated Eyr<strong>in</strong>g model was employed to analyzethe data, <strong>and</strong> estimates of the <strong>in</strong>terfacial shear stresses <strong>and</strong> energetic barriers to slid<strong>in</strong>g wereobta<strong>in</strong>ed. While some of the approximations that were used <strong>in</strong> the analysis lead to large variations<strong>in</strong> calculated contact areas, the fits for the shear stresses <strong>and</strong> <strong>energy</strong> barriers were consistentbetween the different probes. Shear stresses were found to lie mostly between 200 <strong>and</strong> 300 MPafor bare silica <strong>and</strong> between 400 <strong>and</strong> 600 MPa for the grafted layers, with barrier heights <strong>in</strong> therange 1–2 × 10 −19 J for both systems.AFM studies of diamond, graphite, <strong>and</strong> amorphous carbon were reported to exhibit no dependenceon velocity [266] so long as the scann<strong>in</strong>g velocity was much lower than a characteristic slipvelocity of the tip. Consequently, no velocity dependence of friction was observed for scann<strong>in</strong>gspeeds of up to about 10 μm s −1 . A logarithmic dependence was observed for higher velocitiesconsistent with the result of Bouhac<strong>in</strong>a et al. A different trend was reported by Bennewitz et al.Figure 30. (color onl<strong>in</strong>e) <strong>Friction</strong> anisotropy <strong>in</strong> decagonal quasicrystal [416]. <strong>Friction</strong> levels <strong>in</strong> periodicdirections are eight times higher than <strong>in</strong> aperiodic directions. Repr<strong>in</strong>ted figure with permission from J.Y.Park et al., Physical Review B 74, p. 024203, 2006 [416]. Copyright (2006) by the American PhysicalSociety.

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!