A number of distinct differential equations, known as generalized diffusion
equations, have been proposed to describe the phenomenon of anomalous diff
usion on fractal objects. Although all are constructed to correctly reprodu
ce the basic subdiffusive property of this phenomenon, using similarity met
hods it becomes very clear that this is far from sufficient to confirm thei
r validity. The similarity group that they all have in common is the natura
l basis for making comparisons between these otherwise different equations,
and a practical basis for comparisons between the very different modelling
assumptions that their solutions each represent. Similarity induces a natu
ral space in which to compare these solutions both with one another and wit
h data from numerical experiments on fractals. It also reduces the differen
tial equations to (extra-) ordinary ones, which are presented here for the
first time. It becomes clear here from this approach that the proposed equa
tions cannot agree even qualitatively with either each other or the data, s
uggesting that a new approach is needed.