Zirconium in aqueous flows was moderately biomineralized by immobilized Cit
robacter N14 cells, in the form of gel-like deposits, probably comprising a
mixture of zirconium hydrogen phosphate (Zr(HPO4)(2)) and hydrated zirconi
a (ZrO2). The simultaneous presence of uranyl ion (UO22+) did not facilitat
e zirconium deposition and the biomineralization of uranium itself as HUO2P
O4 was repressed by zirconium in the presence of excess inorganic phosphate
, Liberated enzymatically. Nickel (Ni2+) was not significantly removed from
aqueous flows by sorption into cell-bound zirconium deposits, although cel
l-bound hydrogen uranyl phosphate (HUP) facilitated nickel removal via inte
rcalative ion exchange into its polycrystalline lattice. A preformed layer
of HUP also promoted zirconium removal, at 100% efficiency at pH 2.6, maint
ained over 38 column fluid-volumes before saturation. (C) 1999 Society of C
hemical Industry.