A chain of atoms: the Frenkel–Kontorova model
Eq. (6) of Vanossi and co-workers is the Frenkel–Kontorova model: a chain of atoms joined by springs with natural spacing , lying on a sinusoidal potential of period .
When the number of atoms equals the number of substrate valleys, adding one atom makes a kink: a local compression of the chain. Kinks move far more easily than atoms; the Peierls–Nabarro barrier they must cross is always smaller, often much smaller, than . Each run of a kink from one end of the chain to the other moves the whole chain by one period.
Vanossi and co-workers use this to explain an old puzzle: Frenkel estimated the yield stress of a perfect crystal to be of the order of the shear modulus, but measured values are much smaller. The reason is that dislocations, which play the part of kinks in a real crystal, move at much smaller stresses.
Source: A. Vanossi
Mismatched chains and the Aubry transition
If is irrational, an infinite chain takes a staircase shape: regions of near match separated by regularly spaced kinks. Vanossi and co-workers write that when the chain stiffness exceeds a critical value , the kinks move freely, the smallest force makes the chain slide and static friction vanishes; below the kinks are pinned and stick-slip appears.
For the golden-mean ratio, takes its smallest possible value, about 1.0291926 in units of .
Three limits matter for the next two chapters. First, even when static friction vanishes, kinetic friction does not, because sliding at any finite speed excites phonons in the chain. Second, a chain of finite length at zero temperature is always statically pinned, because its free ends lock. Third, the model describes only how a crystalline contact starts to slide; the plastic deformation of real friction experiments lies outside it.
Source: A. Vanossi
A rigid flake is a sum of phases
de Wijn writes the energy of one gold atom on graphite as a sum of three cosines with prefactor ; the corrugation one gold atom feels, , is about 50 meV. The course’s flake model uses the same form in units of and the substrate lattice constant ; in the course these are model parameters, not a specific material.
For a rigid flake, adding up the energies of all atoms can be rewritten exactly as three structure factors . Each atom contributes a phase of unit length, . When the lattices match and are aligned, all phases are equal, , and the corrugation is times that of one atom. Twist the flake and the phases spread around the unit circle; most of them cancel.
The course checks two things: the structure-factor form differs from the atom-by-atom sum by no more than per atom, and for matching lattices at 0° and 60° the corrugation of hexagonal, triangular and disk flakes is exactly per atom.
Source: A. S. de Wijn · A. Vanossi
How friction scales with contact area
de Wijn classifies the mismatch by the exponent with which the corrugation grows with flake diameter. For perfect crystals his Eq. (21) gives three branches, , and , and most orientations belong to , which does not grow with size.
Real particles have ragged edges. de Wijn writes an irregular shape as a sum of many regular shapes with random phases and obtains his Eq. (31): the exponents become , and 1. He also notes that the friction of amorphous crystals grows as whatever their shape.
At a 10° twist the course fits the exponent of corrugation against atom number : 1.000 for aligned flakes; for twisted regular hexagons, consistent with 0, with the corrugation jumping between 0.5 and 9.3 with no trend; for flakes with rough edges, against de Wijn’s 0.25; and for flakes missing 10% of their atoms at random. de Wijn makes no direct prediction for the last case; random vacancies also have random phases, and the argument he uses for amorphous crystals says the exponent should approach 0.5, so we fit only flakes above 357 atoms.
Gold on graphite. de Wijn gives the lattice ratio of gold to graphite as 1.354 in his length unit, which is 1.1726 in the course’s units. At 0° the course model’s corrugation varies erratically between 0.97 and 26.4 as the atom number runs from 19 to 4921. de Wijn also points out that this ratio is close to , so first-order corrections from lattice deformation can be as large as the leading terms; the course’s rigid model leaves them out.
Source: A. S. de Wijn
Worked example: an aligned flake of 127 atoms
Problem. A hexagonal flake of 6 shells on a matching lattice, aligned at 0°, dragged along by a spring of stiffness at zero temperature. Find the atom number, corrugation, stick-slip parameter and quasi-static friction, and compare with simulation and with viscous drag.
Step 1, atom number and corrugation. A hexagon of shells has atoms, so for . Aligned, every atom has the same phase and the corrugation is .
Step 2, reduce to one dimension. Along the line , one of the three cosines is always 1 and the other two are equal, so the energy is a cosine of period and amplitude : exactly the Tomlinson model of chapter 2.
Step 3, the stick-slip parameter. , close to the 11.48 of the tip of Sang and co-workers. For we need : on this spring, only the aligned flake of one shell (7 atoms) fails to stick and slip.
Step 4, friction. The energy-drop method of chapter 3 gives a quasi-static friction of . The course simulation, dragged at reduced speed 0.003 with damping 3, gives , 1.5% higher.
Explanation. The viscous drag at the same speed is , so stick-slip friction is about 245 times larger. The next chapter twists this flake and watches that ratio fall.
Source: A. S. de Wijn · A. Vanossi