Objects, units and directions first
The objects are disks in a plane, half with diameter and half with diameter . Mixing two sizes stops them from settling into a neat crystal. Lengths are in units of , energies in units of the contact stiffness , so forces are in .
Take disks and with radii and and centre distance . They just touch when . Soft disks can press slightly into each other; call the overlap . There is a force only when .
Source: C. S. O’Hern
More overlap, harder push
The contact energy used by O’Hern and co-workers is non-zero only while disks overlap. With exponent it is a spring; with it is a Hertzian contact. Elastic spheres in three dimensions behave that way; using it for disks in two dimensions is a modelling choice.
Minus the derivative with respect to gives a force along the line of centres that pushes the disks apart. For the harmonic case , with a constant stiffness . For the Hertzian case the force grows as , so the contact stiffens as it is pressed.
There is no friction, so the contact force has only this one component along the line of centres. That stays true until friction enters in Chapter 5, and it fixes how many unknowns Chapter 2 has to count.
Source: C. S. O’Hern · C. P. Goodrich
A wall acts like a mirror
The Lab’s box has four flat walls without friction. When a centre is closer to a wall than its radius, , the wall pushes as if the disk had met its own mirror image: the energy is , and the harmonic stiffness is .
This wall law is our own choice. O’Hern and co-workers used periodic cells without walls; when we compare with their data in Chapter 4, we recompute in a periodic cell.
Worked example: two disks squeezed between walls
Put a small disk () and a large one () on one horizontal line between a left and a right wall. Their natural length is . Bring the walls to apart, so the contacts must absorb of overlap in total. Use harmonic contacts.
First the model. Each disk feels only a left and a right force, and to balance they must be equal. So all three contacts carry the same force : springs in series. Their stiffnesses are , and in units of .
Then the numbers. The three overlaps add up to , which gives . The overlaps are , and , which add back to . The disk–disk contact is the softest and takes about two thirds of the squeeze.
Finally a check. Our code relaxes the same configuration with FIRE and matches this closed form to a relative error of at most , for three overlaps and both contact laws.
Source: C. S. O’Hern · J. Guénolé
A hundred disks: force follows a few paths
Pack 128 disks into the box and squeeze. Every contact follows the law above, yet the forces differ widely. At the tightest point of the Lab’s default cycle (packing fraction 0.86) there are 303 load-bearing contacts. About 25 % of them carry less than half the mean force, about 6 % carry more than twice the mean, and the strongest carries about 3.1 times the mean. Half of the total contact force runs through 29 % of the contacts.
Draw each contact as a line whose width is proportional to its force, and the strong contacts link into chains that cross the whole box. These are force chains. Fig. 20 of O’Hern et al. draws the force network of a 2D bidisperse packing the same way.
Experiments can see force chains directly. A photoelastic material changes how it transmits polarised light when it is stressed. Zhao and co-workers photograph photoelastic disks between crossed polarisers and read the pressure of each frame from how sharply the brightness varies across the image.
Source: C. S. O’Hern · Y. Zhao