The kinetics of thermal dehydroxylation of aluminuous goethites [1] synthes
ised from a ferrous salt has been re-examined using the general reaction or
der kinetic law. The utilised data processing was based on the procedures e
mployed by dissolution kinetics. Recalculation of the activation energies E
-A of the dehydroxylation yielded the values 130, 132, 128, and 123 kJ mol(
-1) for pure goethite, goethite with 10, 20, and 30 mol% Al substitution, r
espectively. The values of E-A are in a good agreement with those given for
goethite in literature. The E-A values are linearly related with the chemi
cally bound excess H2O/OH- in the crystal lattice that is apparently influe
nced by Al substitution.