Abstract
The magnetic susceptibility (?T) and saturation magnetization (MS) of microbially synthesized magnetites were systematically examined. Transition metal (Cr, Mn, Co, Ni, and Zn)- and lanthanide (Nd, Gd, Tb, Ho, and Er)-substituted magnetites were microbially synthesized by the incubation of transition metal (TM)- and lanthanide (L)-mixed magnetite precursors with either thermophilic (TOR-39) or psychrotolerant (PV-4) metal-reducing bacteria
(MRB). Zinc incorporated congruently into both the precursor and substituted magnetite, while Ni and Er predominantly did not. Microbially synthesized Mn- and Zn-substituted magnetites had higher ?T than pure biomagnetite depending on bacterial species and they exhibited a maximum ?T at 0.2 cationic mole fraction (CMF). Other TMs?substitution linearly decreased the ?T with increasing substitution amount. Based on the MS values of TM- and L-substituted
magnetite at 0.1 and 0.02 CMF, respectively, Zn- (90.7 emu/g for TOR-39 and 93.2 emu/g for PV-4) and Mn- (88.3 emu/g by PV-4) substituted magnetite exhibited higher MS than standard chemical magnetite (84.7 emu/g) or pure biomagnetite without metal substitution (76.6 emu/g for TOR-39 and 80.3 emu/g for PV-4). Lanthanides tended to decrease MS, with Gd- and Hosubstituted magnetites having the highest magnetization. The higher magnetization of
microbially synthesized TM-substituted magnetites by the psychrotroph, PV-4 may be explained by the magnetite formation taking place at low temperatures slowing mechanics, which may alter the magnetic properties compared to the thermophile, through suppression of the random distribution of substituted cations.
