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Haipeng Song, Jianheng He, Jiong Li, Yu Wang, Yu Ye, Xiang Wu. Hydrothermal large-cavity high-temperature-pressure device combined with Synchrotron radiation X-ray absorption spectroscopy. Journal of Earth Science. doi: 10.1007/s12583-025-0321-3
Citation: Haipeng Song, Jianheng He, Jiong Li, Yu Wang, Yu Ye, Xiang Wu. Hydrothermal large-cavity high-temperature-pressure device combined with Synchrotron radiation X-ray absorption spectroscopy. Journal of Earth Science. doi: 10.1007/s12583-025-0321-3

Hydrothermal large-cavity high-temperature-pressure device combined with Synchrotron radiation X-ray absorption spectroscopy

doi: 10.1007/s12583-025-0321-3
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This research was supported by and the National Key Research and Development Program of China (Grant No. 2018YFA0702700) and the National Science Foundation of China (Grant Nos. 42225202, 41827802). The XAS experiments were performed at the 11B beamline at SSRF. We would like to express our gratitude to SSRF for providing experimental time and to engineers Yu Chen, Yibin Zhang and Zhengxing Lv for their technical support.

  • Available Online: 04 Jul 2025
  • A hydrothermal large-cavity high-temperature and high-pressure device has been meticulously devised for synchrotron radiation X-ray absorption spectroscopy. The experimental temperature and pressure can reach 600 ℃ and 200 MPa with an independent control system. The hydrothermal reactor vessel is equipped with three beryllium windows and is ingeniously designed to accommodate diverse testing modalities within the experimental facility. This apparatus was implemented to investigate the complex species of Au (gold) in chlorine-containing fluids under high-temperature and high-pressure circumstances at the Shanghai Synchrotron Radiation Facility (SSRF). The experimental outcomes disclose that, at relatively low temperatures and pressures, Au predominantly exists in the form of the [AuCl4]- complex. Nevertheless, within the temperature range of 200 - 500 ℃ and pressure range of 72.1 - 92.4 MPa, the complexation form transitions to [AuCl2]-. These discoveries are congruent with prior research, further substantiating the dependability of our experimental methodologies and equipment. Moreover, this device holds the potential to simulate the evolution, species, as well as the physical and chemical properties of metallogenic elements in geological fluids under simultaneous high-pressure and high-temperature conditions.

     

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      沈阳化工大学材料科学与工程学院 沈阳 110142

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