“…A cubic structure is found for phosphates of the type A 4+ P 2 O 7 , where A 4+ may be Si, Ge, Sn, Pb, Ti, Zr, Hf, Mo, W, Re, Ce, Th, U, or Pu. − Double substitution on the A site leads to a series of the type A 3+ 0.5 A 5+ 5.5 P 2 O 7 , where A 3+ may be Bi, Sb, or a rare earth and A 5+ may be Nb, Ta, or Sb . One form of Sb 3+ Sb 5+ (P 2 O 7 ) 2 also has a closely related structure …”