Sie sind hier:
was released by brucite or olivine dissolution and was subsequently oxidized and precipitated as ferric hydroxide. Thermodynamic computations show that this process may be a potential source of catabolic
Bereich: Sites
sequestering important quantities of Fe as FeS2. The in situ oxidation of ferrous Fe and precipitation of ferric hydroxides at the olivine surface commonly observed in oxic environments were obviously impeded.