Knowledge of the pore pressure behavior during dynamic impacts on mode
rately low permeability soils is essential in averting possible liquef
action and effective field implementation of dynamic consolidation. Al
though field observations of dynamically induced pore pressures are ab
undant in the literature, analytical or numerical approaches for pore
pressure prediction are scarce. Herein, the authors advance a simple t
echnique to analytically model the laboratory dynamic consolidation by
modifying the classical Terzaghi's static consolidation theory. Since
the analytical prediction of dynamic surface stress and experimental
verification are performed in a companion paper, the surface stress du
e to a dynamic impact is assumed to be known in this work. Then, the t
ime dependent stress pulse is de-synthesized into a number of constant
load steps to predict the subsequent pore pressure behavior. Since th
is methodology accounts for even the dynamic stress attenuation within
the soil sample, a rigorous closed form solution has to be replaced b
y a numerical solution. It is shown how this solution rapidly converge
s when the load steps are made sufficiently small. Finally, the analyt
ical predictions of dynamic pore pressure are verified by well control
led laboratory experiments performed on a special apparatus set up at
the University of South Florida.