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102  3 Structural Chemistry of Manganese Dioxide and Related Compounds

                    true symmetry respective to the atomic arrangement is monoclinic), or monoclinic
                    cell.
                      The presence of the foreign cations stabilizes the crystal structure of α-MnO 2
                    compounds. This manganese dioxide modification (more exactly it is not a real
                    MnO 2 modification, since the structure contains a considerable proportion of
                                                                           ◦
                    foreign atoms) can be heated to relatively high temperatures (300–400 C) without
                    destruction of the lattice. Although Thackeray et al. reported the synthesis of
                    cation-and water- free α-MnO 2 [48, 49], which is reported to be stable up to 300 C
                                                                                  ◦
                    without destruction of the [2 × 2] tunnel structure, it is commonly believed that a
                    small, but significant, amount of water or foreign cations is necessary to prevent
                    the collapse of the lattice. Otherwise submicro heterogeneities are formed, in which
                    pyrolusite, ramsdellite, and intergrowth domain of these two structural elements
                    coexist with the [2 × 2] tunnel structure of α-MnO 2 within the real lattice.
                      An interesting property of the sieve-like structure of α-MnO 2 is that it shows
                    pronounced cation exchange. For example, an α-MnO 2 with a high barium content
                    is easily prepared by stirring a sample of (NH 4 ) 2−x Mn 8 O 16 (obtained from
                    oxidation of MnSO 4 with a concentrated solution of (NH 4 ) 2 S 2 O 8 in the presence
                    of additional NH 4 ions) in an acidified solution of barium nitrate at elevated
                    temperatures. Consequently, the crystal structure of α-MnO 2 must contain OH −
                    groups, cation vacancies, and/or a proportion of manganese with an oxidation
                    state below Mn 4+  in order to maintain the charge balance. This is reflected in the
                    significantly longer Mn–O distances in the MnO 6 ocathedra in α-MnO 2 (198 pm)
                    compared with those in β-MnO 2 (188 pm).
                      The wide variety of natural minerals with [2 × 2] tunnels already indicates that
                    a huge number of different compounds of the α-MnO 2 type can be obtained by
                    a laboratory synthesis. Most chemical synthesis can be modified by working with
                    concentrated solutions of the chosen foreign cations or by adding larger quantities,
                    for example, of potassium salts or ammonium salts during the reaction in order
                    to produce the α-modification as the major product (for references, see Ref. [47]).
                    Similarly, it is possible to produce samples with a controlled α-MnO 2 /γ -MnO 2
                    ratio by electrolysis in the presence of various amounts of K 2 SO 4 or CaSO 4 [50].

                    3.2.5
                    Roman` echite, Todorokite, and Related Compounds
                    The crystal structure of roman` echite (or psilomelane) is closely related to that
                    of α-MnO 2 . Whereas the α-modification of manganese dioxide consists of
                    corner-sharing double chains of MnO 6 octahedra connected through common
                    edges, the roman` echite structure is build up by crosslinking of chains of double
                    and triple octahedra, as shown in Figure 3.7b. The resulting [2 × 3] tunnels,
                    extending in the b direction of the monoclinic cell, are partially filled by potassium
                    cations or barium cations and by water molecules. Both an orthorhombic
                    setting [22] and a monoclinically distorted structure [24] have been described
                    in the literature (Table 3.1). Mukherjee found a doubling of the short b-axis of
                    an orthorhombic subcell [23] due to cation/water ordering within the [2 × 3]
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