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Using Newton's second law -- Forces on the slab are
ma = F
- Gravity
- Spring above - models tension
- Spring below - models compression
- Dashpots - model viscoelasticity
Using linear models of the springs and dashpots
mx'' + c x' + (ku-kd) x = mg sin(angle)
- x(t) is position
- c is the viscous damping coefficient
- ku, kd are the spring stiffness coefficients
- Assumed to be constant
- Hooke's law springs
- Resting lengths are zero (should vary slowly with time)
Solutions of the linear problem
- Equilibrium position
x = mg sin(angle)/(ku-kd)
- If c > 0 then all solutions but the equilibrium solution are transient.
- Choose c big enough so the system is overdamped.
This model does not predict avalanches or depend on crystal type
- Can be used as a basis for more complex models
- Hooke's law spring will be abandoned