The protonic species formed in spinel lambda-MnO2 by proton exchange f
or lithium ions in Li1+xMn2-xO4 precursors have been characterised by
infrared and inelastic neutron scattering spectroscopies. Proton diffu
sion into the lattice appears to depend on the presence of octahedral
manganese vacancies, with formation of lattice hydroxyl co-existing wi
th water. Mechanisms of proton transfer are considered in relation to
lithium-proton exchange during reinsertion of lithium into the materia
ls, and for insertion of additional protons by chemical reduction.