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Main Authors: Zhao, Xiaodong, Song, Duo, Mergelsberg, Sebastian, Prange, Micah, Boglaienko, Daria, Zhu, Zihua, Wang, Zheming, Pearce, Carolyn I., Sun, Chengjun, Rosso, Kevin M., Guo, Xiaofeng, Zhang, Xin
Format: Preprint
Published: 2025
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Online Access:https://arxiv.org/abs/2503.14816
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author Zhao, Xiaodong
Song, Duo
Mergelsberg, Sebastian
Prange, Micah
Boglaienko, Daria
Zhu, Zihua
Wang, Zheming
Pearce, Carolyn I.
Sun, Chengjun
Rosso, Kevin M.
Guo, Xiaofeng
Zhang, Xin
author_facet Zhao, Xiaodong
Song, Duo
Mergelsberg, Sebastian
Prange, Micah
Boglaienko, Daria
Zhu, Zihua
Wang, Zheming
Pearce, Carolyn I.
Sun, Chengjun
Rosso, Kevin M.
Guo, Xiaofeng
Zhang, Xin
contents Rare earth elements (REEs) are critical for advanced technologies, yet in hydrothermal aqueous solutions the molecular level details of their interaction with ligands that control their geochemical transport and deposition remain poorly understood. This study elucidates the coordination behavior of Yb(III) in sulfate-rich hydrothermal fluids using in situ extended X-ray absorption fine structure (EXAFS) spectroscopy and ab initio molecular dynamics (AIMD) simulations. By integrating multi-angle EXAFS with AIMD-derived constraints, we precisely resolve Yb(III) coordination structures and ligand interactions under hydrothermal conditions. At room temperature, Yb (III) is coordinated by five water molecules and two sulfate ligands (coordination number, CN = 8), forming a distorted square antiprism geometry. Increasing temperature induces progressive dehydration, reducing the hydration shell and favoring stronger sulfate complexation. At 200 Celsius, sulfate ligands reorganize around Yb(III), shifting its geometry to a capped dodecahedron (CN = 7). At 300 Celsius, sulfate binding dominates, leading to structural reorganization that parallels the onset of sulfate mineral precipitation, consistent with the retrograde solubility of REE sulfates. These findings provide direct molecular-scale evidence that sulfate acts as both a transport and deposition ligand, critically influencing REE mobility in geochemical environments. Our results can also help to refine thermodynamic models of REE speciation in high-temperature hydrothermal fluids and improve our understanding of REE ore formation processes in nature.
format Preprint
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institution arXiv
publishDate 2025
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spellingShingle Molecular Insights into Yb(III) Speciation in Sulfate-Bearing Hydrothermal Fluids from X-ray Absorption Spectra Informed by ab initio Molecular Dynamics
Zhao, Xiaodong
Song, Duo
Mergelsberg, Sebastian
Prange, Micah
Boglaienko, Daria
Zhu, Zihua
Wang, Zheming
Pearce, Carolyn I.
Sun, Chengjun
Rosso, Kevin M.
Guo, Xiaofeng
Zhang, Xin
Chemical Physics
Rare earth elements (REEs) are critical for advanced technologies, yet in hydrothermal aqueous solutions the molecular level details of their interaction with ligands that control their geochemical transport and deposition remain poorly understood. This study elucidates the coordination behavior of Yb(III) in sulfate-rich hydrothermal fluids using in situ extended X-ray absorption fine structure (EXAFS) spectroscopy and ab initio molecular dynamics (AIMD) simulations. By integrating multi-angle EXAFS with AIMD-derived constraints, we precisely resolve Yb(III) coordination structures and ligand interactions under hydrothermal conditions. At room temperature, Yb (III) is coordinated by five water molecules and two sulfate ligands (coordination number, CN = 8), forming a distorted square antiprism geometry. Increasing temperature induces progressive dehydration, reducing the hydration shell and favoring stronger sulfate complexation. At 200 Celsius, sulfate ligands reorganize around Yb(III), shifting its geometry to a capped dodecahedron (CN = 7). At 300 Celsius, sulfate binding dominates, leading to structural reorganization that parallels the onset of sulfate mineral precipitation, consistent with the retrograde solubility of REE sulfates. These findings provide direct molecular-scale evidence that sulfate acts as both a transport and deposition ligand, critically influencing REE mobility in geochemical environments. Our results can also help to refine thermodynamic models of REE speciation in high-temperature hydrothermal fluids and improve our understanding of REE ore formation processes in nature.
title Molecular Insights into Yb(III) Speciation in Sulfate-Bearing Hydrothermal Fluids from X-ray Absorption Spectra Informed by ab initio Molecular Dynamics
topic Chemical Physics
url https://arxiv.org/abs/2503.14816