The synthesis of orthorhombic LiMnO2 (O-LiMnO2) with very small crysta
ls (diameter approximate to 0.3 mu m) leads to peculiar X-ray diffract
ion patterns. Some reflections (with k even) remain thin allowing for
cell parameter refinements, showing that, compared to phases with bigg
er crystals, b and c remain unchanged, whereas an important increase o
f the a parameter is observed. Other reflections (with k = 2n + 1 and
h not equal 0) are widened substantially, while the remnant peaks (k =
2n + 1 and h = 0) undergo a strong asymmetrization. These features ha
ve been related successfully to faults corresponding to a b/2 translat
ion of a basic unit constituting O-LiMnO2. A simulation made with the
Diffax program allowed good reproduction of the experimental X-ray dif
fraction data, showing a statistic distribution of the faults, at leas
t for the low fault concentrations corresponding to the samples under
study. The insertion of the fault corresponds to the insertion of a mo
noclinic cell between two blocks of orthorhombic symmetry. This cell (
a approximate to 5.53 Angstrom, b approximate to 2.80 Angstrom, c appr
oximate to 5.30 Angstrom) corresponds to a newly obtained monoclinic L
iMnO2 phase obtained through a topotactic deintercalation of alpha-NaM
nO2. The fault percentage of the compounds studied goes from 1 to 6% a
nd is well correlated to the substitution ratio between lithium and ma
nganese when the fault occurrence is treated as a cationic disorder (o
nly in the case of small disorder for which the lines remain treatable
with the Rietveld refinement program). The fault percentage can also
be determined easily from the cell parameter relation a = x(0)n(0) + x
(m)a(m)sin gamma, where a(0) and a(m) are the parameters of the orthor
hombic and monoclinic cell of the pure phases and x(0) and x(m) their
relative fractions, a being the parameter of the faulted phase as refi
ned from the fault-unaffected thin reflection peaks.