The effect of disorder arising from the mismatch between the average sizes
of the A-site cations in the rare-earth manganates, L(0.5)A(0.5)MnO(3) (L =
rare earth, A = alkaline earth), on their charge-ordering behavior has bee
n investigated. Measurements on two series of manganates with a fixed avera
ge cation radius, < r(A)>, of 1.17 and 1.24 Angstrom, reveal that the charg
e-ordering transition temperature, T-CO, is not very sensitive to the size
mismatch unlike ferromagnetic T-C or metal-insulator transition data. Furth
ermore, T-CO is not affected greatly by the orthorhombic lattice distortion
. The observed decrease in T-CO with increase in < r(A)> is consistent with
a quadratic dependence upon (r(A)(0) - < r(A)>) where r(A)(0) = 1.13 Angst
rom.