Notice on the organization of advanced research class on high-pressure science and new materials of engineering knowledge of professional and technical personnel Notice on the organization of advanced research class on high-pressure science and new materials of engineering knowledge of professional and technical personnel
Volume 32 Issue 4
Apr 2018
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Chinese Journal of High Pressure Physics  > 2018  >  32(4): 041201.
JI Guangfu. Some Viewpoints on the Simulation Research of Energetic Materials under Extreme Conditions[J]. Chinese Journal of High Pressure Physics, 2025, 39(1): 010102. doi: 10.11858/gywlxb.20240911
Citation: HE Yunhong, TIAN Yu, ZHAO Huifang, JIANG Feng, TAN Dayong, XIAO Wansheng. Raman Evidences for Phase Transition of Sodium Perchlorate at High Pressure[J]. Chinese Journal of High Pressure Physics, 2018, 32(4): 041201. doi: 10.11858/gywlxb.20180543
shu

Raman Evidences for Phase Transition of Sodium Perchlorate at High Pressure

doi: 10.11858/gywlxb.20180543
  • 1.

    CAS Key Laboratory of Mineralogy and Metallogeny, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China

  • 2.

    Key Lab of Guangdong Province for Mineral Physics and Materials, Guangzhou 510640, China

  • 3.

    University of Chinese Academy of Sciences, Beijing 100049, China

  • Received Date: 23 Apr 2018
  • Rev Recd Date: 11 Jun 2018
    Abstract
  • Using a diamond anvil cell apparatus, we investigated the sodium perchlorate (NaClO4) by Raman spectroscopy at pressure up to 20 GPa, and calculated the Raman spectra of anhydrite-(Cmcm), monazite-(P21/n), AgMnO4-(P21/n), and barite-type (Pnma) structures of NaClO4 by density function theory.The experimental data show that anhydrite-type NaClO4 undergoes a structural transition at about 4 GPa.A new peak at lower Raman frequencies (975 cm-1) than that of the ClO4- internal mode ν1 (Ag) of the NaClO4 ambient phase was obviously observed at 4.4 GPa.At the same time, several peaks at the corresponding wave numbers of the ClO4- internal modes (ν2、ν3、ν4) arise.The phase transition is completed at about 6.1 GPa, and remains stable up to 19.5 GPa.The high pressure structure can be recovered at about 3.1 GPa in decompression.By comparison with the calculated Raman spectral profiles (at 8.0 GPa) of three potential high pressure structures, we infer that the high pressure phase has a monoclinic monazite-type structure.The pressure-induced phase transition of NaClO4 is consistent with the anhydrite-monazite phase transition found in CaSO4 at about 2 GPa.However, our finding appears inconsistency with the previous observations that the anhydrite-type NaClO4 transforms to AgMnO4-type at about 2 GPa and furthermore to the barite-type structure at around 3 GPa.The previous results could probably be influenced by the moisture of the sample combining with the high temperature and high pressure conditions.It may bring more complicated changes by simultaneous high pressure and high temperature environments.The research progress contributes to the understanding of not only the relationship between volcanic activity and the widespread distribution of perchlorate on Mars, but also the changes and functions of chlorine element during the recycles of subduction and mantle plume in the Earth's deep interior.

     

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