Understanding
the origins of fast ion transport in solids is important
to develop new ionic conductors for batteries and sensors. Nature
offers a rich assortment of rather inspiring structures to elucidate
these origins. In particular, layer-structured materials are prone
to show facile Li
+
transport along their inner surfaces.
Here, synthetic hectorite-type Li
0.5
[Mg
2.5
Li
0.5
]Si
4
O
10
F
2
, being a phyllosilicate,
served as a model substance to investigate Li
+
translational
ion dynamics by both broadband conductivity spectroscopy and diffusion-induced
7
Li nuclear magnetic resonance (NMR) spin–lattice relaxation
experiments. It turned out that conductivity spectroscopy, electric
modulus data, and NMR are indeed able to detect a rapid 2D Li
+
exchange process governed by an activation energy as low
as 0.35 eV. At room temperature, the bulk conductivity turned out
to be in the order of 0.1 mS cm
–1
. Thus, the silicate
represents a promising starting point for further improvements by
crystal chemical engineering. To the best of our knowledge, such a
high Li
+
ionic conductivity has not been observed for any
silicate yet.