Structures and Phase Transition of Vaterite-Type Rare Earth Orthoborates: A Neutron Diffraction Study

球霰石 单斜晶系 结晶学 中子衍射 粉末衍射 晶体结构 化学 材料科学 方解石 矿物学 有机化学 文石
作者
Jianhua Lin,Denis Sheptyakov,Yingxia Wang,P. Allenspach
出处
期刊:Chemistry of Materials [American Chemical Society]
卷期号:16 (12): 2418-2424 被引量:105
标识
DOI:10.1021/cm0499388
摘要

The structure of vaterite-type rare earth orthoborate (LnBO3) has long been a subject of interest and controversy. In the present work, the crystal structures of two polymorphs of the vaterite-type rare earth orthoborates, i.e., the low- and high-temperature modifications of (Y0.92Er0.08)BO3, were solved and refined from neutron powder diffraction data. The low-temperature polymorph crystallizes in a C-centered monoclinic cell with C2/c space symmetry, the unit cell parameters being a = 11.3138(3) Å, b = 6.5403(2) Å, c = 9.5499(2) Å, and β = 112.902(1)°. The boron atoms in the structure are all tetrahedrally coordinated and form the three-membered ring borate B3O9 groups. The high-temperature form crystallizes in a new structure type in a monoclinic cell with C2/c space symmetry, and the unit cell constants a = 12.2019(3) Å, b = 7.0671(2) Å, c = 9.3424(2) Å, and β = 115.347(1)°. The borate groups in the high-temperature structure are all isolated flat BO3 triangles. As far as the structural chemistry is concerned, both structures are different from the typical CaCO3 vaterite. However, they do share some common features, particularly the packing fashion of the cations, which results in similarly looking X-ray diffraction patterns as that of the typical vaterite.
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