Assumption of “free” electrons in the intercalation complex (1) of FeOCl and ferrocene rationalizes the finding that the high‐spin Fe 3+ state of the FeOCl host lattice is retained on intercalation of the guest molecule (Mössbauer spectrum), while the Mössbauer absorptions of ferrocene disappear completely. The conductivity of the crystal also supports formulation as (1) . equation image
No takes yet. Share an insight, caveat, or question.
Schäfer‐Stahl et al. (1980) studied this question.
Synapse has enriched 5 related papers. Consider them for comparative context: