An effective conductivity (thermal or electrical) is derived for polyc
rystalline graphite using a very simple approach. The material is mode
led as a series of links and junctions, the former representing the cr
ystallies and the latter the intercrystallite region. The large anisot
ropy of the principal conductivities permits definition of an excluded
region in which conduction contributes negligibly to the overall ther
mal/electrical transport. Two approximations are obtained for the valu
e of the excluded region, which depend not only upon the principal con
ductivities ratio, but also upon the crystallite shape anisotropy. Thi
s model allows estimation of the effective conductivity of polycrystal
line graphite from a knowledge of the principal conductivities ratio,
the conductivity along the graphite basal plane, the microstructural f
eatures (crystallite shape and size, number, and geometry of intercrys
tallite contacts per crystallite), and the density. Applications to nu
clear-grade graphites gave satisfactory agreement with experimentally
measured electrical and thermal conductivities.