Smoothing is a characteristic inherent to all minimum mean-square-erro
r spatial estimators such as kriging. Cross-validation can be used to
detect and model such smoothing. Inversion of the model produces a new
estimator-compensated kriging. A numerical comparison based on an exh
austive permeability sampling of a 4-ft(2) slab of Berea Sandstone sho
ws that the estimation surface generated by compensated kriging has pr
operties intermediate between those generated by ordinary kriging and
stochastic realizations resulting from simulated annealing and sequent
ial Gaussian simulation. The frequency distribution is well reproduced
by the compensated kriging surface, which also approximates the exper
imental semivariogram well-better that ordinary kriging, but not as we
ll as stochastic realizations. Compensated kriging produces surfaces t
hat are more accurate than stochastic realizations, but not as accurat
e as ordinary kriging.