Abstract
The electrochemically lithiated form of R-Li3Fe2(PO4)3, synthesised by ion exchange of fine powders of Na3Fe2(PO4)3 in a concentrated aqueous solution of LiNO3 at a slightly elevated temperature (40 °C), has been investigated by a combination of ex situ X-ray and ) is totally vacated in R-Li3+xFe2(PO4)3, 0 ≤
x
≤ 1.8, with the lithium ions moving into two new general (18f) positions, Li(1) and Li(2), with 74(4)% and 86(4)% occupation, respectively. This corresponds to the Li+ ions moving cooperatively from pairs of layers (alternate separations: 2.2 and 5.4 Å) for x
= 0 to equally spaced layers (separation: 3.8 Å) for x
= 1.8.