“…Examples of these are some forms of UO 3 solids and U(VI)-doped perovskites like La 2 MgTiO 6 (AZENHA et al, 1992;KHILLA et al, 1986;WEIGEL, 1986;TANNER et al, 1997). However, these forms have not been identified in the geologic environment (BURNS, 1999 and references therein) and they typically form at high temperature under aqueous and non-aqueous conditions (GRIFFITHS and VOLKOVICH, 1999, and references therein). Under chemically reducing conditions soluble U(VI) species can undergo biotic reduction to the sparingly soluble U(IV) species such as UO 2(s) as in FIG.…”