Abstract
The magnetic susceptibility χ of UO2 diluted by its diamagnetic isomorph, ThO2 , is reported for 1.7° ≤  T ≤ 60°K . In dilute samples, 5%–10% UO2 in ThO2 , χ−1 decreases monotonically with decreasing temperature. Blume's singlet ground‐state mechanism for the first‐order magnetic phase transition in UO2 requires a Γ1 singlet ground state 50°K below a Γ5 triplet. The crystal‐field structure of U4+ in ThO2 should be similar and should lead to a rise in χ−1 at low temperature as the triplet depopulates, in striking contrast with observation. Concentrated samples with 0%–40% ThO2 in UO2 show a linear dependence of TN on concentration, with a critical concentration of 42% ThO2 . The singlet ground‐state mechanism in the molecular field approximation predicts that TN is sharply nonlinear with dilution of the molecular field and falls steeply to zero when diluted by 14%. It is apparent from these two lines of evidence that the static ground state in UO2 is not a singlet. The first‐order transition in UO2 is probably related to a dynamic lattice interaction which opposes ordering down to 30°K where a cooperative lattice and magnetic transition takes place.