Apatite-type oxides taking the general formula [A I 4 ][A II 6 ][(BO 4) 6 ][X 2±y ], particularly those of the rare earth silicate and germanate systems, are among the more promising materials being considered as alternative solid oxide fuel cell electrolytes. Nonstoichiometric lanthanum silicate and germanate apatites display pure ionic conductivities exceeding those of yttria-stabilized zirconia at moderate temperatures (500-800 ºC). Indeed, it is the underlying complexity and flexibility of these substances that endows them with such promise as ion conductors. Many factors influence the ionic mobility, the most important being the concentration of cation vacancies and excess anions incorporated in the structure, the valence and atomic size of the substitutional elements, crystal/grain orientations, and phase purity. In this thesis, the main focus falls on the synthesis and characterization of various apatite electrolyte materials and establishing underlying correlations between oxygen ion percolation and crystal chemistry. Apatites can be synthesized in various ways, including solid state sintering, sol-gel methods and hydrothermal reactions. The former is favored since large quantities are readily fabricated for division and multi-technique characterization, while the latter has the advantage of lower synthesis temperature. This thesis examined two synthesis methods (solid state and hydrothermal) for powdered apatites, and the growth of single-crystal apatites for investigating anisotropic ion migration. Laboratory X-ray, synchrotron, and neutron diffraction were employed to refine crystal structures by the Rietveld method. The microstructures, local structures and chemical compositions were analyzed by electron diffraction, spectroscopic and microscopic methods. Vanadium-doped apatites of nominal composition [La 8 AE 2 ][Ge 6-x V x ]O 26+x/2 (AE = Ca, Sr, Ba; 0 ≤ x ≤ 1.5) were prepared by conventional solid state sintering. Single-phase products were obtained for x ≤ 0.5, with a combination of powder synchrotron X-ray and neutron diffraction confirming these products to be P6 3 /m apatites. The ionic conductivities extracted by complex impedance spectroscopy showed that small vanadium amendments enhanced oxygen mobility at Abstract iv intermediate temperatures (500-800 ºC) by more than one order of magnitude, as the incorporation of V 5+ through displacement of Ge 4+ is charge balanced with interstitial O 2that improves ionic conduction. The most promising composition was La 7.88 Ca 2 Ge 5.35 V 0.65 O 26.15 that delivered σ = 3.44×10-4 S•cm-1 at 500 ºC. The superstoichiometric oxygen was delocalised, without fixed X-ray or neutron scattering centres. Crystal chemistry systematics demonstrate that the Ca-apatite was superior because the relatively small framework expanded through (La/AE)O 6 metaprism twisting (φ) that widened the tunnel, ensuring P6 3 /m symmetry was adopted, which favours the passage of O 2with lower activation energy. Mixed Si/Ge-based apatites were prepared by hydrothermal synthesis under ...