The structure factor of AgI, both Bragg and diffuse scattering, has be
en measured at 12 temperatures between 293 and 790 K by powder neutron
diffraction. Below 420 K gamma- and beta-phases coexist, but there is
evidence for considerable conversion of gamma-to beta-phase above 400
K. The reverse Monte Carlo technique has been used to model the alpha
-phase data above 420 K. The maximum Ag+ density is found to occur in
the tetrahedral sites, with diffusion between them through trigonal an
d, to a lesser extent, octahedral positions. The Ag+ density distribut
ion is only weakly temperature dependent. An effective single site pot
ential has been derived from the Ag+ density distribution; the energy
barrier between tetrahedral sites is in good agreement with that deter
mined from the ionic conductivity. However the motion of Ag+ is not si
mple hopping diffusion across this barrier, but is correlated with the
motion of the I- and of the other Ag+. Many studies have reported une
xpected behaviour between 600 and 700 K, which has been attributed to
some kind of ''order-disorder'' transition. In this work no evidence w
as found for such a transition, suggesting that it is not caused by a
change in short range order.