Reverse Monte Carlo modelling of isotopic substitution neutron diffrac
tion data for molten CuBr (D Allen and R A Howe 1992 J. Phys.: Condens
. Matter 4 6029) is used to show that a flat partial radial distributi
on function g(CuCu)(r) is a possible numerical solution, but not a pos
sible physical solution. The best model derived is a close-packed liqu
id of Br- ions within which Cu+ ions occupy approximately tetrahedral
interstices. This structure is a natural continuation of trends as a f
unction of temperature within the crystalline gamma-phase and the fast
-ion-conducting beta- and alpha-phases.