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Cation Disorder and Large Tetragonal Supercell Ordering in the Li-Rich Argyrodite Li 7 Zn 0.5 SiS 6 .

Bernhard T LeubeChristopher M CollinsLuke M DanielsBenjamin B DuffYun DangRuiyong ChenMichael W GaultoisTroy D ManningFrédéric BlancMatthew S DyerJohn B ClaridgeMatthew J Rosseinsky
Published in: Chemistry of materials : a publication of the American Chemical Society (2022)
A tetragonal argyrodite with >7 mobile cations, Li 7 Zn 0.5 SiS 6 , is experimentally realized for the first time through solid state synthesis and exploration of the Li-Zn-Si-S phase diagram. The crystal structure of Li 7 Zn 0.5 SiS 6 was solved ab initio from high-resolution X-ray and neutron powder diffraction data and supported by solid-state NMR. Li 7 Zn 0.5 SiS 6 adopts a tetragonal I 4 structure at room temperature with ordered Li and Zn positions and undergoes a transition above 411.1 K to a higher symmetry disordered F 43 m structure more typical of Li-containing argyrodites. Simultaneous occupation of four types of Li site (T5, T5a, T2, T4) at high temperature and five types of Li site (T5, T2, T4, T1, and a new trigonal planar T2a position) at room temperature is observed. This combination of sites forms interconnected Li pathways driven by the incorporation of Zn 2+ into the Li sublattice and enables a range of possible jump processes. Zn 2+ occupies the 48 h T5 site in the high-temperature F 43 m structure, and a unique ordering pattern emerges in which only a subset of these T5 sites are occupied at room temperature in I 4 Li 7 Zn 0.5 SiS 6 . The ionic conductivity, examined via AC impedance spectroscopy and VT-NMR, is 1.0(2) × 10 -7 S cm -1 at room temperature and 4.3(4) × 10 -4 S cm -1 at 503 K. The transition between the ordered I 4 and disordered F 43 m structures is associated with a dramatic decrease in activation energy to 0.34(1) eV above 411 K. The incorporation of a small amount of Zn 2+ exercises dramatic control of Li order in Li 7 Zn 0.5 SiS 6 yielding a previously unseen distribution of Li sites, expanding our understanding of structure-property relationships in argyrodite materials.
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