Electronic structure calculations are carried out to estimate the heats of formation of rareearth orthophosphates from their oxides. The calculated heats of formation are systematically about 40 kJ/mol less exothermic than the measured values. Based on estimated corrections for zero-point energies and H(298.15)-H(0), the discrepancy is almost entirely electronic in origin. The decreasingly exothermic H f ox with decreasing ionic radius (i.e. LaPO 4 more exothermic than ScPO 4 ) results from the higher charge localization on the oxide anion (O 2-) relative to the phosphate anion (PO 4 3-). The lattice energy, of course, becomes more negative with decreasing ionic radius for both oxide and phosphate phases, but does so more rapidly for the oxide, making the reaction less exothermic as ionic radius becomes smaller. This effect should carry over to H f ox other oxyacids, such as silicates and sulfates. a Ni et al., 1995; b antiferromagnetic electronic states; c ferromagnetic electronic state