Abstract:
Ferrihydrite nanoparticles formed as a result of the microorganism activity have been studied using Mössbauer spectroscopy, X-ray powder diffraction analysis, and X-ray fluorescence analysis. Three positions of trivalent iron with nonoverlapping ranges of quadrupole splittings have been revealed in bacterial ferrihydrite: QS$\{$Fe$^{3+}$(1)$\}$ = 0.49–0.83 mm/s, QS$\{$Fe$^{3+}$(2)$\}$ = 0.84–1.10 mm/s, and QS$\{$Fe$^{3+}$(3)$\}$ = 1.25–1.73 mm/s. It has been experimentally demonstrated that the Fe$^{3+}$(3) positions are the centers of nucleation of the hematite phase in the course of heat treatment.