“…In this case, there are no electrons in valence f orbitals and the use of the standard GGA approximation supplemented with empirical dispersion corrections has produced highly accurate results for the structural, spectroscopic, mechanic and thermodynamic properties of a large series of uranyl containing minerals as rutherfordine, soddyite, uranophane-a, studtite, metastudtite, g-UO 3 , dehydrated schoepite, schoepite and metaschoepite. 88,[90][91][92][111][112][113][114][115][116][117][104][105][106] It must be emphasized that the calculated thermodynamic properties of these materials were very accurate in those cases in which experimental values of these properties were available for comparison even at very low and high temperatures. [90][91][92]115,116 As an example, the errors in the computed enthalpies of formation of rutherfordine, 90 g-UO 3 , 90 and metaschoepite 92 at 700, 900, and 800 K were 1.6%, 1.0% and 2.0%, respectively.…”