Dimensional equivalents of spatial objects and their projected images are w
ell identified in stereology. However, at present, it is not clear if these
and the Delesse and Rosiwal principles are applicable to fractal sets. Sca
ling properties of statistically selfsimilar solid and pore sets of four so
ils and sediments with contrasting genesis were described by the divider me
thod. Two programs were used for the image analysis. Both programs are vari
ants of the box-counting technique and are useful for the fractal analysis
along the lines (Linfrac) and across the areas (Fractal). These programs we
re tested using the images of ideal fractals and of some statistical fracta
l sets. For all analysed images, the fractal dimension across an area was c
lose to double the value of the set dimension along the Line. This relation
was independent regarding the material nature, management system applied,
horizon depth and profile localisation. Therefore, it seems to be necessary
to correct the classical Delesse and Rosiwal principles for the statistica
lly self-similar fractal sets. (C) 1998 Published by Elsevier Science B.V.
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