Soil living organisms currently exhibit complex spatial patterns at va
rious scales. Conventional methods for studying spatial dispersion are
based on various aggregation indices or probability distribution anal
ysis. Since these methods do not take into account the actual location
of the sampling sites, they provide no information on the spatial dis
tribution at scales larger than the sampling unit size. The geostatist
ical analysis is a way to analyse the spatial pattern of a variable at
scales ranging from the minimum to the largest intersample distance.
The variogram indicates whether the variable is spatially dependent or
not. If a structure is present, the kriging local interpolation proce
dure provides estimates of the variable and their estimation error. Co
ntour mapping of these values gives accurate maps of both the variable
and the reliability of the estimated values. Kriging is a local estim
ation method that yields fine description of short and large-scale str
uctures whereas traditional interpolation procedure by trend surface a
nalysis only describes large-scale patterns. At a further stage, the r
elationship between two spatially dependent variables can be examined
by cross-variogram analysis. The latter procedure allows the study of
the complex relationships that occur either between biological variabl
es or biological and environmental variables.