Recent resonant bar experiments on Berea sandstone show that nonlinear
excitation of the sample excites a slow dynamics with a time scale ma
ny orders of magnitude longer than the excitation period, 2 pi/omega.
That is, a nonlinear resonant frequency decays to the linear resonant
frequency long after the high amplitude drive has been turned off. We
postulate a phenomenological theory of slow nonlinear dynamics in the
context of a resonant bar experiment. The normalized elastic modulus o
f the resonant bar is allowed to be nonlinear and time dependent. The
nonlinear terms are derived from a model of elasticity in rocks that i
ncludes anharmonic and hysteretic contributions. We use this theory to
explain the experimental results. We find an explanation for the slow
relaxation of the experimental resonant frequency using an anharmonic
contribution to the modulus that responds instantaneously to a distur
bance, and a contribution derived from elastic hysteresis that display
s slow dynamics. We suggest an acoustic NMR-type experiment to explore
slow nonlinear dynamics.