In order to individuate the modifications induced in the soil by fires rela
tively to the mobility of metals and rare earth three soils of Sardinia whi
ch differ in their mineralogical and physico-chemical characteristics were
sampled. The analytical results obtained on the samples drawn at different
depths (0-5 and 10-30 cm) three months after a fire and on the tests indica
te that only the surface layer underwent significant modifications. The dyn
amics of metals and the distribution of the rare earths were found to depen
d, besides the amount and quality of the burned material, on the different
behaviour of elements towards leaching. The diffractometric analysis showed
that the soil surface layer of all the samples did not exceed 400 degreesC
.