While doing slug tests in high permeability aquifers, we have consiste
ntly seen deviations from the expected response of linear theoretical
models. Normalized curves do not coincide for various initial heads, a
s would be predicted by linear theories, and are shifted to larger tim
es for higher initial hi:ads. We have developed a general nonlinear mo
del based on the Navier-Stokes equation, nonlinear frictional loss, no
n-Darcian flow, acceleration effects, radius changes in the well bore.
and a Hvorslev model for the aquifer, which explains these data featu
res. The model produces a very good fit for both oscillatory and nonos
cillatory field data, using a single set of physical parameters to pre
dict the field data for various initial displacements at a given well.
This is in contrast to linear models which have a systematic lack of
fit and indicate that hydraulic conductivity varies with the initial d
isplacement. We recommend multiple slug tests with a considerable vari
ation in initial head displacement to evaluate the possible presence o
f nonlinear effects. Our conclusion is that the nonlinear model presen
ted here is an excellent tool to analyze slug tests, covering the rang
e from the underdamped region to the overdamped region.