Temperature and pressure effects on the structural and vibrational properties of forsterite from density functional theory studies

IF 1.2 4区 地球科学 Q4 MATERIALS SCIENCE, MULTIDISCIPLINARY Physics and Chemistry of Minerals Pub Date : 2024-08-08 DOI:10.1007/s00269-024-01287-4
Sha Chen, Udo Becker
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Abstract

Due to experimental challenges and computational complexities, limited research has explored high-temperature and high-pressure conditions on mineral vibrations. This study employs the quasi-harmonic approximation (QHA) and density functional theory (DFT) to investigate the impact of temperature and pressure on the structural properties and infrared and Raman vibrational modes of forsterite. The computational process involves determining lattice parameters, optimizing the internal crystal structure, and calculating IR and Raman spectra at various temperature and pressure values, both separately and combined. Results highlight significant anisotropy in forsterite, with the b-axis being most sensitive to temperature and pressure, followed by the c-axis, while the a-axis exhibits greater stiffness. The positions of vibrational modes typically shift to higher frequencies with increasing pressure (average shift of 2.70 ± 1.30 cm−1/GPa) or to lower frequencies with increasing temperature (average shift of − 0.017 ± 0.018 cm−1/K). Modes associated with SiO4 stretching and bending are less affected by temperature or pressure than translational and rotational modes. A brief investigation into isotope and chemical substitution, as well as cation distribution, in the solid solution (Mg, Fe)2SiO4 reveals lower wavenumbers in fayalite modes compared to forsterite modes, attributed to the heavier Fe mass and larger cell parameters. This study establishes a methodology for computing vibrational frequencies under simultaneous temperature and pressure and emphasizes the significant impact of various factors on vibrational modes. Caution is advised when using vibrational modes for identifying compositions within solid solutions.

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从密度泛函理论研究看温度和压力对绿柱石结构和振动特性的影响
由于实验挑战和计算复杂性,探索高温高压条件下矿物振动的研究十分有限。本研究采用准谐波近似(QHA)和密度泛函理论(DFT)来研究温度和压力对绿柱石结构特性以及红外和拉曼振动模式的影响。计算过程包括确定晶格参数、优化内部晶体结构,以及在不同温度和压力值下分别和合并计算红外光谱和拉曼光谱。结果表明,绿柱石具有明显的各向异性,其中 b 轴对温度和压力最为敏感,其次是 c 轴,而 a 轴则表现出更大的刚性。振动模式的位置通常会随着压力的增加而向高频移动(平均移动量为 2.70 ± 1.30 cm-1/GPa),或随着温度的增加而向低频移动(平均移动量为 - 0.017 ± 0.018 cm-1/K)。与平移和旋转模式相比,与 SiO4 拉伸和弯曲相关的模式受温度或压力的影响较小。对固溶体 (Mg,Fe)2SiO4 中同位素和化学取代以及阳离子分布的简要调查显示,与绿柱石模式相比,辉绿岩模式的文数较低,这归因于较重的铁质量和较大的晶胞参数。这项研究确立了在温度和压力同时作用下计算振动频率的方法,并强调了各种因素对振动模式的重要影响。建议在使用振动模式确定固体溶液中的成分时要谨慎。
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来源期刊
Physics and Chemistry of Minerals
Physics and Chemistry of Minerals 地学-材料科学:综合
CiteScore
2.90
自引率
14.30%
发文量
43
审稿时长
3 months
期刊介绍: Physics and Chemistry of Minerals is an international journal devoted to publishing articles and short communications of physical or chemical studies on minerals or solids related to minerals. The aim of the journal is to support competent interdisciplinary work in mineralogy and physics or chemistry. Particular emphasis is placed on applications of modern techniques or new theories and models to interpret atomic structures and physical or chemical properties of minerals. Some subjects of interest are: -Relationships between atomic structure and crystalline state (structures of various states, crystal energies, crystal growth, thermodynamic studies, phase transformations, solid solution, exsolution phenomena, etc.) -General solid state spectroscopy (ultraviolet, visible, infrared, Raman, ESCA, luminescence, X-ray, electron paramagnetic resonance, nuclear magnetic resonance, gamma ray resonance, etc.) -Experimental and theoretical analysis of chemical bonding in minerals (application of crystal field, molecular orbital, band theories, etc.) -Physical properties (magnetic, mechanical, electric, optical, thermodynamic, etc.) -Relations between thermal expansion, compressibility, elastic constants, and fundamental properties of atomic structure, particularly as applied to geophysical problems -Electron microscopy in support of physical and chemical studies -Computational methods in the study of the structure and properties of minerals -Mineral surfaces (experimental methods, structure and properties)
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