Neutron-diffraction data presented in this paper demonstrate the relevance
of lattice displacement above Tc, in our understanding of the evolution of
the crystal structure with temperature in the layered colossal magnetoresis
tance manganite La1.2Sr1.8Mn2Mn2O7. The anomalous temperature behavior of t
hermal diffuse scattering in (La1.2Sr1.8MnO7)-O-2 strongly suggests that it
arises from lattice displacements and correlates directly with anomalies i
n the displacement parameters of the O and Mn atoms and the Mn-O bond lengt
hs. From our measurements, the insulator-metal transition can be described
as a transition from a high-temperature state with disordered Mn-O bond len
gths to a low-temperature stare with a more uniform distribution on Mn-O bo
nds. These observations are in agreement with polaronic charge transport ab
ove T-C in the perovskite manganites; as electron hopping is responsible fo
r bond disorder above T-C, below the transition where e(g) carriers are del
ocalized, any lattice displacements are uniformly averaged. [S0163-1829(99)
04429-X].