Graphite intercalation compounds (GICs) with electron donors such as alkali
metals, alkaline earth metals, or lanthanides, can be obtained by conversi
on of graphite with solutions of the respective metal in liquid ammonia. In
case of using flake graphite as the starting material for the conversion w
ith Li-ammonia solutions metastable GICs are formed, whose stoichiometry de
pends on the Li-concentration in the solution. Whereas such flake graphite
based Li-ammonia GICs decompose slowly by expelling NH3 gas, samples based
on highly oriented pyrolytic graphite (HOPG) decompose immediately after ha
ving been separated from the reaction solution. The so formed residual comp
ound contains only small traces of Li metal, but still some amount of NH3 g
as. If the residual compound is exposed to vacuum, it expands by a factor 2
to 3. This process proved to be reversible: even after 100 expansion-contr
action cycles no degradation of the material could be detected.