The experiment: a graphite flake on graphite
Vanossi and co-workers review the experiments of Dienwiebel, Verhoeven and co-workers: a graphite flake attached to the tip of a friction force microscope slides on an atomically flat graphite surface, and the friction is measured as a function of the twist between the two. The course has not read these original papers; the numbers below come from the review.
For most orientations the surfaces are mismatched and the friction is below 50 pN. Only in narrow ranges of twist that correspond to matching contacts does stick-slip appear, with high friction, typically 250 pN.
Fig. 4 of the review plots these data together with a generalized Prandtl–Tomlinson model: the graphite flake is treated as a rigid finite lattice, a symmetric flake of 96 atoms, and its twist is assumed not to change while it is dragged. The computed mean friction has narrow peaks near the matching angles, separated by wide ranges of ultra-low friction. The course’s flake Lab uses the same kind of model, with graphite replaced by the three-cosine potential of chapter 6.
Source: A. Vanossi
How wide is the friction peak
At small twist, turning the flake changes the phase of each atom by times its offset from the centre measured perpendicular to . Treat the flake as a continuum disk and the structure factor becomes the Airy-type function of diffraction by a circular hole, with its first zero at radians, where is the diameter in substrate lattice spacings.
For lattice disks of diameter 10, 20 and 40 the course model puts the first minimum at 6.008°, 3.008° and 1.510°; the continuum disk gives 6.052°, 3.026° and 1.513°, within 0.8%. The half width at half maximum times the diameter is 0.61 radians for all three sizes.
Vanossi and co-workers write that the angular width of a friction peak obeys , so that the peak width can be used to estimate the flake diameter. It gives 5.711°, 2.862° and 1.432°: about 6% below the first zero and about 1.6 times the half width. The review does not say which width means; put a measured half width into the rule and the diameter comes out about 1.6 times too large.
Source: A. Vanossi · A. S. de Wijn
Dragging a twisted flake
Twist the 127-atom hexagon of chapter 6 to different angles and drag it, as before, with a spring of stiffness at zero temperature, reduced speed 0.003 and damping 3. The mean friction (in ) and the stick-slip parameter are: 280.4 at 0° (), 193.2 at 2° (8.29), 108.2 at 3° (5.43), 28.9 at 4° (2.51), 1.155 at 5° (0.16), 11.23 at 7° (1.67), and 1.141 at both 10° and 30°.
The rise at 7° comes from the first side lobe of the structure factor. Scanned in steps of 0.02°, holds in two ranges: 0° to 4.60° and 5.76° to 8.56°, the second peaking at at 7°. So a finite flake still sticks weakly beside the main peak; only beyond 9° does it slide smoothly all the way.
At 10° and 30° the remaining friction is the viscous drag at the same speed, , to within 0.2%. The damping is a model parameter chosen by the course, not a measured value; a rigid flake on a rigid substrate has no phonons, so the model has no other way to dissipate energy. Friction falling to the viscous drag therefore shows only that the stick-slip channel has closed; the friction of a real flake also depends on dissipation channels the model leaves out.
Source: A. S. de Wijn · A. Vanossi
Superlubricity is not zero friction
Vanossi and co-workers note that the term superlubricity has been criticized, because it suggests zero resistance by analogy with superconductivity and superfluidity. Mismatch removes only one channel of dissipation, the stick-slip instability at low speed; other dissipative processes, such as the emission of sound waves, remain, so even a completely mismatched contact has nonzero net kinetic friction. They still expect friction to be substantially reduced compared with a similar matching contact.
The low-friction state may also not last. The review cites experiments of Filippov and co-workers in which flake superlubricity disappears because the flake turns back into the matching orientation. de Wijn writes that mismatched orientations usually have a higher mean energy than matching ones and can be destroyed by large enough thermal fluctuations; in experiments with small graphite flakes on graphite the mismatched orientations decayed, while larger crystals were found theoretically to rotate more slowly, so their mismatched orientations survive. Like the model in the review, the course Lab locks the twist and cannot show this decay.
Defects also bring friction back. At 10° and on a softer spring, a perfect flake of about 1000 atoms has 0.97 times the viscous drag; a flake missing 10% of its atoms at random has 3.0 times; a flake with rough edges has 3.1 times. The size scaling of chapter 6 shows that the corrugation from this kind of disorder grows with area.
Source: A. Vanossi · A. S. de Wijn
Worked example: how far must the 127-atom hexagon turn to stop sticking
Problem. The aligned hexagon of chapter 6, , . Using only the continuum-disk formula, estimate the twist at which stick-slip vanishes and whether the side lobe sticks again, then compare with the course model.
Step 1, the stick-slip parameter shrinks with the structure factor. The substrate is fixed, so twisting changes only . The hexagon is centrosymmetric and its three structure factors are equal, so both the corrugation and scale with . Stick-slip vanishes when .
Step 2, replace the hexagon by a disk of equal area. Each atom occupies , so the flake area is and the disk of equal area has diameter .
Step 3, solve. The first root of is , which gives ; the first zero is at 5.11°.
Step 4, the side lobe. The first negative extremum of is at . Times 11.14 this gives a side-lobe , above 1, at 6.85°; from 5.85° to 8.05°.
Comparison with the model. In the course model falls to 1 at 4.60° and the first minimum of the corrugation is at 5.09°; the side lobe peaks at at 7.0° and spans 5.76° to 8.56°. The disk formula gets the main peak to within 1%; the side lobe is more sensitive to shape, because a hexagon is not a disk. Conclusion: this flake stops sticking beyond 4.6°, but weak stick-slip returns near 7°.
Source: A. S. de Wijn · A. Vanossi