“…U 5+ has been documented to occur in nature in various minerals (Burns et al, 1997;Burns and Finch, 1999;Schindler et al, 2009;Vance and Mackey, 1978), during oxidative dissolution of UO 2 (Ulrich et al, 2008(Ulrich et al, , 2009Shoesmith et al, 2004;Santos et al, 2004), and only fleetingly during bacterial respiration (Renshaw et al, 2005). Various U 5+ solids have been synthesized using solid-state techniques (e.g., Van den Berghe et al, 2000Liu et al, 2009) as well as hydrothermal routes (e.g., Belai et al, 2008).…”