543 K 下液-液相分离的 MgSO4 溶液中物种的 Ab Initio 分子动力学模拟和振动频率计算

IF 1.2 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS Geofluids Pub Date : 2024-02-21 DOI:10.1155/2024/8852421
Mengzi Zhou, Xiancai Lu, Xiandong Liu, Yingchun Zhang, Xiaoyu Zhang, Kai Wang
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引用次数: 0

摘要

由于热液中存在金属硫酸盐复合物,含硫酸盐盐水的迁移与硫化物矿床的成矿密切相关。在各种金属-硫酸盐体系中显然会发生液-液相分离,其传输和沉淀与均质流体不同。之前的研究发现,在液-液相分离的 MgSO4 溶液的富浓度相中,有一种在 ~1020 cm-1 处具有拉曼峰的新物种,并将其解释为链状结构聚合物。为了揭示这一物种,研究人员进行了分子动力学模拟(AIMD)和自相关函数频率计算。结果表明,围绕 SO42- 阴离子的 Mg2+ 离子越多,拉曼峰的波长数就越高,这表明形成了与基色石类似的复杂离子群。此外,在均相溶液中,v-980 拉曼带在 ~980、990 和 1005 cm-1 处的分裂峰代表更多的单价镁-Os(SO42- 的 Os:O)结合,而不是某些种类,这有利于形成预核簇。此外,通过自由能计算,双齿 Mg-SO4 配体在 543 K 时的稳定性低于单齿配体。我们的发现从原子水平上确认了液-液相分离的 MgSO4 流体中的浓相,并从理论上解释了 980 cm-1 拉曼峰的移动,这将进一步启发对水合硫酸盐矿物成核过程的理解以及对其他硫酸盐体系拉曼光谱的解析。
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Ab Initio Molecular Dynamics Simulations and Vibrational Frequency Calculations of Species in Liquid-Liquid Phase Separated MgSO4 Solution at 543 K

The transport of sulfate-bearing brines is closely relevant to mineralization of sulfide deposits as metal-sulfate complexes exist in hydrothermal fluids. Liquid-liquid phase separation evidently occurs in various metal-sulfate systems with transport and precipitating different from homogeneous fluids. Previous studies have revealed a new species with a Raman peak at ~1020 cm-1 in rich concentration phase of liquid-liquid phase separated MgSO4 solution, and it was interpreted as chain structure polymers. Ab initio molecular dynamics simulations (AIMD) and autocorrelation functions for frequency calculation have been performed to disclose the speciation. The results show that more Mg2+ ions surrounding a SO42- anion lead to higher wavenumber of Raman peaks, which indicates the formation of complicate clusters with ion associations similar to kieserite. Besides, the splitting peaks of v-980 Raman bands at ~980, 990, and 1005 cm-1 in homogeneous solution represent more monodentate Mg-Os (Os: O of SO42-) associations instead of certain species, which favors the formation of prenucleation clusters. Furthermore, bidentate Mg-SO4 ligand is less stable than monodentate ligands at 543 K by applying free energy calculations. Our findings give atomic level recognition of concentrated phase in liquid-liquid phase separated MgSO4 fluids and theoretical explanation of the 980 cm-1 Raman peak shifting, which will further inspire understandings on nucleation processes of hydrated sulfate minerals and Raman spectra resolving of other sulfate systems.

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来源期刊
Geofluids
Geofluids 地学-地球化学与地球物理
CiteScore
2.80
自引率
17.60%
发文量
835
期刊介绍: Geofluids is a peer-reviewed, Open Access journal that provides a forum for original research and reviews relating to the role of fluids in mineralogical, chemical, and structural evolution of the Earth’s crust. Its explicit aim is to disseminate ideas across the range of sub-disciplines in which Geofluids research is carried out. To this end, authors are encouraged to stress the transdisciplinary relevance and international ramifications of their research. Authors are also encouraged to make their work as accessible as possible to readers from other sub-disciplines. Geofluids emphasizes chemical, microbial, and physical aspects of subsurface fluids throughout the Earth’s crust. Geofluids spans studies of groundwater, terrestrial or submarine geothermal fluids, basinal brines, petroleum, metamorphic waters or magmatic fluids.
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