Room-Temperature Synthesis, Hydrothermal Recrystallization, and Properties of Metastable Stoichiometric FeSe.

Room-temperature precipitation from aqueous solutions yields the hitherto unknown metastable stoichiometric iron selenide (ms-FeSe) with tetragonal anti-PbO type structure. Samples with improved crystallinity are obtained by diffusion-controlled precipitation or hydrothermal recrystallization. The relations of ms-FeSe to superconducting &bgr;-FeSe1-x and other neighbor phases of the iron--selenium system are established by high-temperature X-ray diffraction, DSC/TG/MS (differential scanning calorimetry/thermogravimetry/mass spectroscopy), Fe Mössbauer spectroscopy, magnetization measurements, and transmission electron microscopy. Above 300 °C, ms-FeSe decomposes irreversibly to &bgr;-FeSe1-x and Fe7Se8. The structural parameters of ms-FeSe (P4/nmm, a = 377.90(i) pm, c = S51.1l{3) pm, Z = 2), obtained by Rjetveld refinement, differ significantly from hterature data for &bgr;-FeSe1-x The Mössbauer spectrum rules out interstitial iron atoms or additional phases. Magnetization data suggest canted antiferromagnetism below TN, = 50 K. Stoichiometric non-superconducting ms-FeSe can be regarded as the tme "parent" compound for the "11" iron-chalcogenide superconductors and may serve as starting point for new chemical modifications. [ABSTRACT FROM AUTHOR]