Ge 4+ substitution into the recently discovered superionic conductor Li 7 Si 2 S 7 I is demonstrated by synthesis of Li 7 Si 2–x Ge x S 7 I, where x ≤1.2. The anion packing and tetrahedral silicon location of Li 7 Si 2 S 7 I are retained upon substitution. Single crystal X‐ray diffraction shows that substitution of larger Ge 4+ for Si 4+ expands the unit cell volume and further increases Li + site disorder, such that Li 7 Si 0.88 Ge 1.12 S 7 I has one Li + site more (sixteen in total) than Li 7 Si 2 S 7 I. The ionic conductivity of Li 7 Si 0.8 Ge 1.2 S 7 I ( x =1.2) at 303 K is 1.02(3)×10 −2 S cm −1 with low activation energies for Li + transport demonstrated over a wide temperature range by AC impedance and 7 Li NMR spectroscopy. All sixteen Li + sites remain occupied to temperatures as low as 30 K in Li 7 Si 0.88 Ge 1.12 S 7 I as a result of the structural expansion. This differs from Li 7 Si 2 S 7 I, where the partial Li + site ordering observed below room temperature reduces the ionic conductivity. The suppression of Li + site depopulation by Ge 4+ substitution retains the high mobility to temperatures as low as 200 K, yielding low temperature performance comparable with state‐of‐the‐art Li + ion conducting materials.
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Han et al. (2024) studied this question.
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