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

• Published in: Inorganic chemistry 2012-07, Vol.51 (13), p.7370-7376
• Main Authors: Nitsche, F, Goltz, T, Klauss, H.-H, Isaeva, A, Müller, U, Schnelle, W, Simon, P, Doert, Th, Ruck, M
• Format: Article
• Language: English
• ISSN: 0020-1669; 1520-510X
• DOI: 10.1021/ic300798p

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 β-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), 57Fe Mössbauer spectroscopy, magnetization measurements, and transmission electron microscopy. Above 300 °C, ms-FeSe decomposes irreversibly to β-FeSe1–x and Fe7Se8. The structural parameters of ms-FeSe (P4/nmm, a = 377.90(1) pm, c = 551.11(3) pm, Z = 2), obtained by Rietveld refinement, differ significantly from literature data for β-FeSe1–x . The Mössbauer spectrum rules out interstitial iron atoms or additional phases. Magnetization data suggest canted antiferromagnetism below T N = 50 K. Stoichiometric non-superconducting ms-FeSe can be regarded as the true “parent” compound for the “11” iron-chalcogenide superconductors and may serve as starting point for new chemical modifications.