P. Ganguly et al., EVIDENCE FOR MULTIPLE M SITES IN AMO(2) COMPOUNDS - CO-59 SOLID-STATENMR-STUDIES ON LICOO2, JOURNAL OF PHYSICAL CHEMISTRY B, 101(51), 1997, pp. 11099-11105
The layered AMO(2) compounds (A = alkali metal, M = trivalent octahedr
al site cations) derived from the simple rock-salt structure have alwa
ys been considered to have only one crystallographic site for the A an
d the M atoms. These structures are described in terms of close-packed
oxygen layers with interstitial A and M atoms, especially when A = Li
. This gives a layer sequence (AO)(-) and (MO)(+). The AMO(2) compound
s are part of the compounds in the A-M-O systems such as A(2)MO(3) and
A(5)MO(6), which are derived from the rock-salt structure with altern
ating layers of pure (AO)(-) and mixed [(A,M)O](+) layers with multipl
e interstitial octahedral sites in the (A,M)O layer for occupation by
the different A and M cations. Evidence is presented from Co-59 NMR ex
periments on LiCoO2 for the existence of at least two sites in the (Co
O)(+) layer. Several NMR methodologies, such as the use of various pul
se sequence, nutation experiments, and magic angle sample spinning (MA
SS) are employed. Magic-angle-sample-spinning experiments show only on
e isotropic peak. However, an analysis of spinning sidebands envelope
at various spinning speeds clearly shows the presence of at least two
sites. One of these has orthorhombic symmetry and another has axial sy
mmetry, with closely related chemical shift anisotropy components that
result in the observation of nearly identical isotropic chemical shif
ts. The possible importance of the absence or presence of holes on oxy
gen has been discussed in accounting for the two sites.