In situ phase separation following dehydration in bimetallic sulfates: a variable-temperature X-ray diffraction study.

Phase separation resulting in a single-crystal-single-crystal transition accompanied by a polycrystalline phase following the dehydration of hydrated bimetallic sulfates [Na(2)Mn(1.167)(SO(4))(2)S(0.33)O(1.167) x 2 H(2)O and K(4)Cd(3)(SO(4))(5) x 3 H(2)O] has been investigated by in situ variable-temperature single-crystal X-ray diffraction. With two examples, we illustrate the possibility of generating structural frameworks following dehydration in bimetallic sulfates, which refer to the possible precursor phases at that temperature leading to the mineral formation. The room-temperature structure of Na(2)Mn(1.167)(SO(4))(2)S(0.33)O(1.167) x 2 H(2)O is trigonal, space group R3. On heating the crystal in situ on the diffractometer, the diffraction images display spherical spots and concentric rings suggesting phase separation, with the spherical spots getting indexed in a monoclinic space group, C2/c. The structure determination based on this data suggests the formation of Na(2)Mn(SO(4))(2). However, the diffraction images from concentric rings could not be indexed. In the second example, the room-temperature structure is determined to be K(4)Cd(3)(SO(4))(5) x 3 H(2)O, crystallizing in a monoclinic space group, P2(1)/n. On heating the crystal in situ, the diffraction images collected also have both spherical spots and diffuse rings. The spherical spots could be indexed to a cubic crystal system, space group P2(1)3, and the structure is K(2)Cd(2)(SO(4))(3). The possible mechanism for the phase transition in the dehydration regime resulting in this remarkable single-crystal to single-crystal transition with the appearance of a surrogate polycrystalline phase is proposed.