Abstract
Intercalation compounds generally consist of porous host structures which can ingest a variety of guest species into the pore spaces with little or no distortion of the host structure itself. 1–3 The porous regions within the host may exhibit full three dimensional connectivity as in zeolites4 or alkali tungsten bronzes5, completely constrained one dimensional character as in polyacetylene6 or partially constrained two dimensional regions as in graphite intercalation compounds,7 intercalated layer dichalcogenides,8 and clay intercalation compounds. These latter solids are members of a large class of materials, the layered intercalation compounds, which has been heavily investigated during the past decade. This class of intercalation compound has been interesting primarily because it exhibits not only unusual physical properties which may be of technological importance but also because it serves as an arena in which to study novel physical phenomena in reduced, i.e. 2, dimensions.
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Solin, S.A. (1993). The Structure, Morphology and Layer Rigidity of Clay Intercalation Compounds. In: Bernier, P., Fischer, J.E., Roth, S., Solin, S.A. (eds) Chemical Physics of Intercalation II. NATO ASI Series, vol 305. Springer, Boston, MA. https://doi.org/10.1007/978-1-4615-2850-0_8
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DOI: https://doi.org/10.1007/978-1-4615-2850-0_8
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