“…They comprise a large class of isomorphous compounds with composition A x Ti 2-y M y O 4 , where A= K, Rb, or Cs, and M represents a vacancy or Li, Mg, Co, Ni, Cu, Zn, or Mn. 15,16,17,18 Lepidocrocite titanates usually crystallize in an orthorhombic structure, consisting of two-dimensional layers of edge and corner sharing octahedra with the large alkali metal ions (A) located in the interlayers. These compensate for the negative charges that arise from the substitution of low valency metal ions or vacancies (M) for Ti 4+ .…”