Abstract

The magnetisation of the third stage graphite intercalation compound (GIC) with CrCl 3 exhibits an anomalous behaviour in high magnetic fields analogous to the first stage CoCl 2 GIC. This anomaly can be explained by magnetostriction. The ternary graphite compound with CrCl 3 and MnCl 2 is a stacking of ferromagnetic CrCl 3 layers alternating with paramagnetic MnCl 2 layers. It is shown that a magnetic polarisation is induced by the ordered ferromagnetic layers on the paramagnetic ones. At low temperatures a long range antiferromagnetic order sets in.

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