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12.15 Phospho-Olivine LiMPO 4  363
               a simple oxide such as Fe 2 O 3 to polyanion hosts like Fe 2 (XO 4 ) 3 and a difference
               of 0.6 V between the isostructural Fe 2 (SO 4 ) 3 and Fe 2 (MoO 4 ) 3 polyanion hosts, all
               operating with the same Fe 2+/3+  couple, were attributed to the influence of inductive
               effect and consequent differences in the location of the Fe 2+/3+  redox levels relative
                       +
               to the Li/Li redox level, as seen in Figure 12.17. In the Nasicon-related Fe 2 (SO 4 ) 3
               and Fe 2 (MoO 4 ) 3 hosts with corner-shared FeO 6 octahedra, XO 4 tetrahedra, and
               Fe–O–X–O–Fe (X = S, Mo, or W) linkages, the strength of the X–O bond can
               influence the Fe–O covalence and thereby the relative position of the Fe 2+/3+
               redox energy. The stronger the X–O bonding, the weaker the Fe–O bonding, and
               consequently the lower the Fe 2+/3+  redox energy relative to that in a simple oxide
               like Fe 2 O 3 . The net result is a higher cell voltage on going from Fe 2 O 3 to Fe 2 (MoO 4 ) 3
               or Fe 2 (SO 4 ) 3 . Comparing Fe 2 (MoO 4 ) 3 and Fe 2 (SO 4 ) 3 , the S–O covalent bonding
               in Fe 2 (SO 4 ) 3 is stronger compared to the Mo–O bonding in Fe 2 (MoO 4 ) 3 , leading
               to a weaker Fe–O covalence in Fe 2 (SO 4 ) 3 than that in Fe 2 (MoO 4 ) 3 , resulting in a
               lowering of the Fe 2+/3+  redox energy in Fe 2 (SO 4 ) 3 compared to that in Fe 2 (MoO 4 ) 3
               and a consequent increase in cell voltage by 0.6 V. Thus, the replacement of simple
               O 2−  ions by XO 4  n−  polyanions was recognized as a viable approach to tune the
               position of redox levels in solids and consequently to realize higher cell voltages
               with chemically more stable, lower-valent redox couples like Fe 2+/3+ .


               12.15
               Phospho-Olivine LiMPO 4

               Although the above findings in the late 1980s demonstrated an important funda-
               mental concept in tuning the redox energies in solids, the cathode hosts pursued
               did not contain any lithium, so they could not be combined with the carbon anode
               in a lithium-ion cell. Following this initial concept, several phosphates have been
               investigated [94–96], and, in 1997, Goodenough’s group identified LiFePO 4 ,crystal-
               lizing in the olivine structure (Figure 12.18), as a facile lithium extraction/insertion
               host that could be combined with a carbon anode in lithium-ion cells [94]. They
               also identified other olivines of the general formula LiMPO 4 (M = Mn, Co, and
               Ni) as lithium insertion/extraction hosts. Since its identification as a potential
               cathode, LiFePO 4 has been the subject of extensive studies from both scientific and
               technological points of view.

                 Li
                 Fe
                 P
                 O


                  a
               c
               Figure 12.18  Crystal structure of olivine LiFePO 4 .
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