The thermal conductivity and diffusivity of lithium sulphate have been
measured simultaneously, using the transient plane source technique o
ver the temperature range 300-900 K. The thermal conductivity decrease
s slowly up to about 640 K, whereupon a distinct rise occurs, indicati
ng the onset of a pre-transitional behaviour, which causes a continuou
s growth of the conductivity up to the structural phase transition at
851 K, whereupon a very sharp increase occurs. A similar behaviour has
been observed for the thermal diffusivity, for which a very sharp dip
occurs at the transition point due to the exceptionally large transit
ion enthalpy. The pre-transitional behaviour of heat transport is asso
ciated with the librational disorder of the sulphate anions known from
Raman scattering studies of both phases (and neutron scattering from
the cubic phase), whereas the translational disorder of lithium cation
s is of hardly any importance. It is thus possible to link the 'paddle
-wheel' concept of ion migration in the cubic phase to the enhancement
of heat transport observed in the 'pre-transition' region, as well as
to the large difference in heat-transport rates between the monoclini
c and cubic phases.