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| Journal Article | PUBDB-2026-00365 |
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2025
ACS Publications
Washington, DC
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Please use a persistent id in citations: doi:10.1021/jacs.5c15843 doi:10.3204/PUBDB-2026-00365
Abstract: Iron sulfides (FexSy), including greigite (Fe$_3$S$_4$), are key materials in geological processes and technological applications. However, in the context of colloidal synthesis, the mechanism by which these nanoparticles form remains unexplored. Here, we employ in situ X-ray diffraction and photon-in photon-out spectroscopic studies to elucidate the reaction pathway of Fe(acac)$_3$ and thioacetamide (TAA) in benzyl alcohol (BA), which yields crumpled Fe$_3$S$_4$ nanosheets. Using powder X-ray diffraction (PXRD), we identify FeS (mackinawite) as a crystalline intermediate whose anisotropic growth, driven by its layered crystal structure, governs the crumpled nanosheet-like morphology of Fe$_3$S$_4$ (greigite) through a topotactic transition. By performing high-resolution fluorescence-detected X-ray absorption near-edge structure (HERFD-XANES) spectroscopy, we show that the formation of Fe$_3$S$_4$ proceeds through a multistep mechanism involving two intermediates. Supported by density functional theory (DFT), we find that Fe(acac)$_3$ is initially reduced in the presence of TAA in BA, forming a molecular intermediate [Fe(acac)$_2$(BA)$_2$], which subsequently transforms into FeS and ultimately into Fe$_3$S$_4$. Complementary valence-to-core X-ray emission spectroscopy (vtc-XES) reveals the evolution of the coordination environment from Fe–O to Fe–S throughout the reaction. Our work provides a comprehensive understanding of the formation mechanism of Fe$_3$S$_4$ nanosheets in solution, shedding light on how crystal growth dynamics and electronic structure evolution dictate their unique crumpled nanosheet morphology.
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