Mineralogy and Petrology ( IF 1.8 ) Pub Date : 2023-01-04 , DOI: 10.1007/s00710-022-00807-w Manfred Wildner , Gerald Giester
Crystals of the compound LiCo(SO4)OH were synthesised at low-hydrothermal conditions, and the crystal structure was determined and refined from single crystal X-ray diffraction data. LiCo(SO4)OH crystallises monoclinic, space group P21/c, Z = 4, a = 9.586(2), b = 5.425(1), c = 7.317(1) Å, β = 109.65(1)°, V = 358.3 Å3, wR2 = 0.0485 (2215 unique reflections, 78 variables). The structure is built from chains of edge-sharing, quite strongly bond-length and -angle distorted Co(OH)3O3 octahedra (< Co–O > = 2.126 Å), which are further linked by common corners, hydrogen bonds, and by properly shaped SO4 tetrahedra (< S–O > = 1.476 Å) to sheets parallel (100). These sheets are connected to a three-dimensional framework by sharing corners with distorted LiO4 polyhedra (< Li–O > = 1.956 Å). Apart from the isotypic sulfates of Mn2+ and Fe2+, only the molybdate LiCd(MoO4)OH crystallises isostructural with LiCo(SO4)OH. However, a very close structural relationship exists with the rare mineral hodgkinsonite, Zn2Mn(SiO4)(OH)2, yielding crystal chemically very uncommon topological equivalents of Zn2+ ≡ S6+ and Si4+ ≡ Li+, aside from the expectable substitution Mn2+ ≡ Co2+. Polarised optical absorption spectra of LiCo(SO4)OH reveal that the dominating spin-allowed 4T1(P) band system of Co2+ (d7 configuration) is strongly split up and covers a prominent part (~ 15,500–24,500 cm−1) of the visible spectral range, in accordance with the significant distortion of the Co(OH)3O3 polyhedron. The spectra are interpreted in terms of the Superposition Model of crystal fields, yielding a new set of intrinsic and interelectronic repulsion parameters for Co2+.
中文翻译:
LiCo(SO4)OH的晶体结构和光学吸收光谱及其与锌锰硅酸盐霍奇金石的显着关系
在低水热条件下合成化合物 LiCo(SO 4 )OH 的晶体,并根据单晶 X 射线衍射数据确定和精炼晶体结构。LiCo(SO 4 )OH 结晶为单斜晶系,空间群P 2 1 / c,Z = 4,a = 9.586(2),b = 5.425(1),c = 7.317(1) Å,β = 109.65(1)° , V = 358.3 Å 3 , wR 2 = 0.0485(2215 次独特反射,78 个变量)。该结构由共享边的链构成,具有相当强的键长和角度扭曲的 Co(OH) 3 O3 个八面体 (< Co–O > = 2.126 Å),它们通过公共角、氢键和适当形状的 SO 4四面体 (< S–O > = 1.476 Å) 进一步连接到平行的片 (100)。这些薄片通过与扭曲的 LiO 4多面体 (< Li–O > = 1.956 Å)共享角连接到三维框架。除了 Mn 2+和 Fe 2+的同型硫酸盐,只有钼酸盐 LiCd(MoO 4 )OH 与 LiCo(SO 4 )OH 同构结晶。然而,与稀有矿物霍奇金石 Zn 2 Mn(SiO 4 )(OH) 2存在非常密切的结构关系,产生晶体化学上非常罕见的拓扑等效物 Zn 2+ ≡ S 6+和 Si 4+ ≡ Li +,除了预期的取代 Mn 2+ ≡ Co 2+。LiCo(SO 4 )OH的偏振光学吸收光谱表明,Co 2+的主导自旋允许4 T 1 (P) 带系统(d 7构型)强烈分裂并覆盖突出部分(~ 15,500–24,500 cm −1 ) 的可见光谱范围,根据 Co(OH) 3 O 3的显着畸变多面体。根据晶体场的叠加模型解释光谱,产生一组新的 Co 2+固有和电子间排斥参数。