Aa. Martin et Mjg. Lee, OXYGEN-ISOTOPE EFFECT ON THE VIBRATIONAL-MODES OF BI2SR2CACU2O8+DELTA, Physica. C, Superconductivity, 254(3-4), 1995, pp. 222-232
The O-16-O-18 oxygen isotope effect has been studied in the Raman spec
tra of single crystals of the high-T-c superconductor Bi2Sr2CaCu2O8+de
lta. It is found that the oxygen isotope shifts of all of the vibratio
nal peaks fall into one of three narrow ranges. The absence of a signi
ficant isotope shift for certain peaks indicates either that they corr
espond to normal modes that involve only the motion of cations (peaks
at and below 181 cm(-1)), or that they involve the vibration of oxygen
on sites where isotope exchange proceeds extremely slowly (peaks at 3
10 cm(-1) and 661 cm(-1)). The isotope-shift data provide strong evide
nce that, contrary to previous assignments, the A(1g) peaks at 287 cm(
-1) and 350 cm(-1) correspond to vibrational modes of oxygen atoms in
the copper layer. Large oxygen isotope shifts support the assignment o
f the 386 cm(-1) peak to in-plane vibrations of oxygen atoms in the st
rontium layer, and of the 458 cm(-1) peak to c-axis vibrations of thes
e same atoms. The!! are inconsistent with an earlier suggestion that t
he 458 cm(-1) peak corresponds to a vibrational mode of oxygen atoms i
n the copper layer.