Gonzalez-Platas Javier, Muñoz Alfonso, Rodríguez-Hernández Placida, Errandonea Daniel
Departmento de Física, Instituto Universitario de Estudios Avanzados en Física Atómica, Molecular y Fotónica (IUDEA) and MALTA Consolider Team , Universidad de La Laguna , Avda. Astrofísico Fco. Sánchez s/n , E-38206 La Laguna, Tenerife , Spain.
Departamento Física, Malta Consolider Team and Instituto de Materiales y Nanotecnología , Universidad de La Laguna , 38206 La Laguna, Tenerife , Spain.
Inorg Chem. 2019 May 6;58(9):5966-5979. doi: 10.1021/acs.inorgchem.9b00291. Epub 2019 Apr 15.
We have investigated the high-pressure behavior of PbCrO. In particular, we have probed the existence of structural transitions under high pressure (at 4.5 GPa) by single-crystal X-ray diffraction and density functional theory calculations. The structural sequence of PbCrO is different than previously determined. Specifically, we have established that PbCrO, under pressure, displays a monoclinic-tetragonal phase transition, with no intermediate phases between the low-pressure monoclinic monazite structure (space group P2/ n) and the high-pressure tetragonal structure. The crystal structure of the high-pressure polymorph is, for the first time, undoubtedly determined to a tetragonal scheelite-type structure (space group I4/ a) with unit-cell parameters a = 5.1102(3) Å and c = 12.213(3) Å. These findings have been used for a reinterpretation of previously published Raman and optical-absorption results. Information of calculated infrared-active phonons will be also provided. In addition, the pressure dependence of the unit-cell parameters, atomic positions, bond distances, and polyhedral coordination are discussed. The softest and stiffest direction of compression for monazite-type PbCrO are also reported. Finally, the theoretical pressure dependence of infrared-active modes is given, for the first time, for both polymorphs.
我们研究了铬酸铅(PbCrO₄)的高压行为。具体而言,我们通过单晶X射线衍射和密度泛函理论计算,探究了高压(4.5吉帕)下结构转变的存在情况。铬酸铅(PbCrO₄)的结构序列与先前确定的不同。具体来说,我们确定了铬酸铅(PbCrO₄)在压力下呈现单斜-四方相转变,在低压单斜独居石结构(空间群P2₁/n)和高压四方结构之间不存在中间相。首次明确确定高压多晶型物的晶体结构为四方白钨矿型结构(空间群I4₁/a),晶胞参数a = 5.1102(3) Å,c = 12.213(3) Å。这些发现已被用于重新解释先前发表的拉曼光谱和光吸收结果。还将提供计算出的红外活性声子的信息。此外,讨论了晶胞参数、原子位置、键距和多面体配位的压力依赖性。还报告了独居石型铬酸铅(PbCrO₄)最软和最硬的压缩方向。最后,首次给出了两种多晶型物红外活性模式的理论压力依赖性。