Slow shear: smooth loading, sudden slips
Quasistatic shear moves the top of a periodic cell sideways by a small strain, here , and lets the disks relax to the nearest energy minimum before the next step. There is no inertia and no temperature: the packing always sits in a minimum, and shear slowly changes the shape of that minimum. While the minimum exists, the stress rises along a smooth curve and each step can be undone: shearing back returns every load-bearing disk to where it was.
A slip is the moment that minimum disappears. The disks fall into another minimum, the stress drops, and the step cannot be undone. In our packings of 64 Hertzian disks at , the smooth stretches last a median strain of 0.0098, and the disk that moves most in a slip jumps a median of about 0.1 small-disk diameters. To locate a slip within in strain, the failed step is halved again and again.
Source: C. E. Maloney and A. Lemaître
Why one mode goes soft first
Expand the energy along the one collective motion that is about to fail, with coordinate . Near the slip the lowest terms that matter are a cubic in and a tilt that the shear gradually removes. Keeping only these two terms gives the stiffness of the mode:
Source: C. E. Maloney and A. Lemaître
How close to the slip the square root holds
The square root holds only close to the slip. In our Hertzian packings the local slope of against between and has a median of 0.475 over 288 slips; between and it is only 0.254, because the other terms of the expansion still matter there.
Harmonic contacts behave differently. Their stiffness does not depend on the overlap, and drops to zero at once when a contact opens. With harmonic contacts the lowest stiffness usually stays flat until the slip and then collapses: only 12% of slips soften gradually, against 98% with Hertzian contacts.
Reading soft spots from the vibrations
The stiffness of each collective motion comes from the dynamical matrix, the second derivatives of the energy with respect to the disk positions. Its eigenvectors are the vibration modes and its eigenvalues their stiffnesses. Disks with no load-bearing contact, the rattlers, are removed first; otherwise each rattler adds a mode of zero stiffness.
Manning and Liu (2011) sheared 2500 Hertzian disks at . From each of the 30 softest modes they took the 20 particles that move most and grouped them into soft spots, about a tenth of all particles. Each rearrangement fell in one spot; the example in their Fig. 2 has an overlap score of 0.64. Soft spots had 6% fewer contacts and 103% more free volume than the rest, yet those local quantities alone did not find them.
Source: M. L. Manning and A. J. Liu
A blind test on packings the method never saw
We repeated the idea on smaller packings with a simpler score. At the start of each smooth stretch, the disks with the largest are named. After the slip, the six load-bearing disks with the largest non-affine jump are the movers. The hit fraction is the share of named disks that are movers. Two simpler guesses are scored the same way: the six disks with the fewest load-bearing contacts, and the six with the lowest local pressure.
The number of modes was chosen on eight training packings (96 slips) only: one and two modes scored 0.276 and 0.278, and more modes did worse, so . Sixteen other packings then gave 192 test slips. The two softest modes named 26% of the movers, the fewest-contacts guess 18%, the lowest-pressure guess 15%, and a random guess 9%. Slip by slip, the soft modes beat the fewest-contacts guess by 0.080 on average, with a standard error of 0.014. In 44 of the 192 slips they named none of the movers.
These packings are small, 64 disks against 2500 in Manning and Liu, and our score is not their overlap score, so the two sets of percentages cannot be compared directly. A denser packing () gave 28%, and so did harmonic contacts; chance stayed at 9%.
Source: M. L. Manning and A. J. Liu
Worked example: scoring one slip
Open the Lab’s default preset. The first slip comes at . All 64 disks are load-bearing, so . At the start of the smooth stretch the two softest modes named disks 62, 36, 26, 22, 23 and 12. The six largest jumps were disks 36, 10, 62, 28, 60 and 26, the largest 0.291 diameters. The shear stress fell from to .
Step one, the hit fraction: disks 62, 36 and 26 are on both lists, so . The fewest-contacts guess (26, 32, 62, 28, 12, 48) also hits three; the lowest-pressure guess (26, 12, 1, 25, 32, 39) hits one.
Step two, chance: . The probability that six random disks include three or more movers, worked out below, is under 1%. A single slip this good rarely happens by luck, but the fewest-contacts guess did as well here, so one slip cannot rank the methods. That is why the test averages 192 slips.
Step three, the approach: the lowest stiffness was at before the slip and at , a local slope of . One decade farther out, at it was , a slope of 0.49. Both are close to the one half of a fold.