An asymptotic formulation of the inverse problem for flow reveals that the
inversion may be partitioned into two complementary subproblems. In the fir
st problem the arrival time associated with the peak slope of the transient
curve is directly related to reservoir properties. The second inverse prob
lem is similar to current methods for. interpreting flow data; the transien
t head amplitudes are related to reservoir storage and conductivity. The fi
rst subproblem,,the arrival time inversion, involves much less computation
than does amplitude matching. Furthermore, it appears to be more robust wit
h respect to the starting model. Therefore the solution to the arrival time
inversion provides a starting model for amplitude matching. The methodolog
y is particularly suited to the analysis of observations from well tests. W
e apply the approach to observations from two interference tests conducted
at the Borehole Test Facility in Oklahoma. Using the transient pressure mea
surements, we image a shallow conductive fracture. The existence and locati
on of the fracture has been verified by both geophysical and borehole data.
In particular, core from a slant well contains an open, vertical fracture
which coincides with our conductive feature.