G. Christakos et Xy. Li, BAYESIAN MAXIMUM-ENTROPY ANALYSIS AND MAPPING - A FAREWELL TO KRIGINGESTIMATORS, Mathematical geology, 30(4), 1998, pp. 435-462
The Bayesian Maximum Entropy (BME) method of spatial analysis and mapp
ing provides definite rules for incorporating prior information, hard
and soft data into the mapping process. It has certain unique features
that make it a loyal guardian of plausible reasoning under conditions
of uncertainty. BME is a general approach that does not make any assu
mptions regarding the linearity of the estimator, the normality of the
underlying probability laws, or the homogeneity of the spatial distri
bution. By capitalizing on various sources of information and data, BM
E introduces an epistemological framework that produces predictive map
s that are more accurate and in many cases computationally more effici
ent than those derived by traditional techniques. In fact, kriging tec
hniques can be derived as special cases of the BME approach, under res
trictive assumptions regarding the prior information and the data avai
lable. BME is a more rigorous approach than indicator kriging for inco
rporating soft data. The BME formulation, in fact, applies in a spatia
l or a spatiotemporal domain and its extension to the case of block an
d vector random fields is straightforward. New theoretical results are
presented and numerical examples are discussed, which use the BME app
roach to account for important sources of knowledge in a systematic ma
nner. BME can be useful in practical situations in which prior informa
tion can be used to compensate for the limited amount of measurements
available (e.g., preliminary of feasibility study levels) or soft data
are available that can be combined with hard data to improve mapping
significantly. BME may be then viewed as an effort towards the develop
ment of a more general framework of spatial/temporal analysis and mapp
ing, which includes traditional geostatistics as its limiting case, an
d it also provides the means to derive novel results that could nor be
obtained by traditional geostatistics.