2019
DOI: 10.1016/j.jssc.2018.12.015
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Superionic lithium conductor with a cubic argyrodite-type structure in the Li–Al–Si–S system

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Cited by 43 publications
(36 citation statements)
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“…Topological analysis of the connectivity between tetrahedral interstices within the argyrodite lattice, 38,42 as well as experimental data for Li6+xSb1-xMxS5I (M = Si, Ge), Li6.15Mʹ1.5S6 and the related oxysulfide Li6.15Mʹ1.5S5.4O0.6 (Mʹ = Al0.1Si0.9), 33,47,48 and the recent theoretical predictions for Li6PS5X (X = I, Cl), 42 all highlight the possible occupation of non-type 5 sites in the Li6PS5X lithium argyrodites. While these non-type 5 sites must play a role in long-ranged Li diffusion in all argyrodites, to our knowledge, no previous experimental evidence exists for non-negligible occupation in Li6PS5X (X= Cl, Br, I).…”
Section: Resultsmentioning
confidence: 99%
“…Topological analysis of the connectivity between tetrahedral interstices within the argyrodite lattice, 38,42 as well as experimental data for Li6+xSb1-xMxS5I (M = Si, Ge), Li6.15Mʹ1.5S6 and the related oxysulfide Li6.15Mʹ1.5S5.4O0.6 (Mʹ = Al0.1Si0.9), 33,47,48 and the recent theoretical predictions for Li6PS5X (X = I, Cl), 42 all highlight the possible occupation of non-type 5 sites in the Li6PS5X lithium argyrodites. While these non-type 5 sites must play a role in long-ranged Li diffusion in all argyrodites, to our knowledge, no previous experimental evidence exists for non-negligible occupation in Li6PS5X (X= Cl, Br, I).…”
Section: Resultsmentioning
confidence: 99%
“…Topological analysis of the connectivity between tetrahedral interstices within the argyrodite lattice, 38,42 as well as experimental data for Li6+xSb1-xMxS5I (M = Si, Ge), Li6.15Mʹ1.5S6 and the related oxysulfide Li6.15Mʹ1.5S5.4O0.6 (Mʹ = Al0.1Si0.9), 33,47,48 and the recent theoretical predictions for Li6PS5X (X = I, Cl), 42 all highlight the possible occupation of non-type 5 sites in the Li6PS5X lithium argyrodites. While these non-type 5 sites must play a role in long-ranged Li diffusion in all argyrodites, to our knowledge, no previous experimental evidence exists for non-negligible occupation in Li6PS5X (X= Cl, Br, I).…”
Section: Resultsmentioning
confidence: 99%
“…Some computational evidence for the role of non-type 5 tetrahedra in lithium diffusion in Li 6 PS 5 X argyrodites comes from previous bond-valence calculations, which predict three distinct lithium sites [26,27,29]. Non-type 5 sites have also been identified in recent neutron diffraction studies of Li 6 PS 5 Br and Li 6 PS 5 Cl [46,47], as well as in lithiumargyrodites with lithium stoichiometries x(Li) > 6 [48][49][50]. A general mechanistic description of lithium conduction in lithium-argyrodites that describes the role of different lithium sites and that can explain the relationship between substitutional anion disorder and fast lithium transport, however, is currently lacking.…”
Section: Structural Considerationsmentioning
confidence: 92%