A thermoanalytical (TGA/DSC) and diffractometric (XRD) study has been perfo
rmed on the solid state reaction system Li2CO3-Fe2O3 in the x(Li) range 0.1
0 divided by 0.50. A detailed analysis of the results shows that the data a
re in agreement with a reaction model where the carbonate decomposition is
regulated by the formation of both LiFeO2 and LiFe5O8, and the relative amo
unt of the two phases depends on the initial composition. The DSC evidence
offers the possibility to directly quantify the LiFe5O8 phase. Furthermore
it allows one to obtain the enthalpies of formation of both LiFeO2, and LiF
e5O8.