The electrical conductivity of cubic samples (monoliths) made of moderately
compressed expanded graphite has been measured along two orthogonal direct
ions, namely parallel and perpendicular to the pressing force. It is found
that these highly porous materials exhibit a percolation behaviour, with a
transition from insulator to conductor occurring at a very low critical den
sity. Besides, the monoliths are found to be quite isotropic as their poros
ity is high; conversely, increasing their apparent density makes them becom
e more and more anisotropic thanks to the orientation of their constitutive
graphite particles. Both percolation and effective media theories are show
n to accurately fit the conductivity data as far as isotropic materials are
concerned. Microstructural parameters derived from the fits are discussed
and found to be in fair agreement with the expected description of compress
ed expanded graphite, i.e. insulating voids surrounded by thin conducting f
lakes.