A method for curve fitting was used to study and compare the variation
in the density of state responsible for the occurrence of the white l
ine associated with the L(II) and L(III) absorption discontinuities of
rare earths in their oxides and cuprates. It is observed that the inc
reased covalent character of the rare earth-oxygen bond in rare earth
cuprate results in a decrease in the density of the final energy state
responsible for the white line.