Abstract
The layered structural type of FeOCl1 has often been reported for its ability to be intercalated by lithium and various molecules2,3,4. The lattice is built up with two alternate metal oxygen-layers sandwiched by a double layer of chlorine atoms (Fig. 1).
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Bujoli, B., Janvier, P., Villieras, J., Palvadeau, P., Rouxel, J. (1987). Lamellar ferric oxychloride properties from intercalation to topochemical reaction. In: Legrand, A.P., Flandrois, S. (eds) Chemical Physics of Intercalation. NATO ASI Series, vol 172. Springer, Boston, MA. https://doi.org/10.1007/978-1-4757-9649-0_30
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