Pressure data from well tests and interference tests contain informati
on about the distribution of permeability and porosity within the rese
rvoir, but the relationship between the data and the rock properties i
s quite complex. Estimates of permeability and porosity are easily obt
ained through standard applications of inverse theory methods, yet the
relationship of the estimates to the true values is usually not clear
. In this paper I discuss the concept of ''resolution of the model,''
the idea that the estimate at any location is influenced by the rock p
roperties at neighboring locations and, sometimes, by rock properties
at quite distant locations. If the estimation process is very good, th
e estimate is influenced only by rock properties near the estimation p
oint and the spread of the resolution is said to be small. I use this
measure to compare the value of interference tests with standard well
tests for estimating permeability and porosity in the interwell region
. In general, adding a third well test is more effective than adding a
n interference test to estimate permeability. Porosity is more difficu
lt to resolve, but interference tests are generally more effective tha
n well tests at improving the resolution of the estimate.