4.7 Article

Ethane and methane at high pressures: Structure and stability

期刊

JOURNAL OF CHEMICAL PHYSICS
卷 155, 期 18, 页码 -

出版社

AIP Publishing
DOI: 10.1063/5.0067828

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资金

  1. Army Research Office [56122-CH-H, 71650-CH]
  2. Deep Carbon Observatory
  3. Helmholtz Young Investigators Group CLEAR [VH-NG1325]
  4. National Science Foundation Earth Sciences [EAR-1634415]
  5. Department of Energy GeoSciences [DE-FG02-94ER14466]
  6. DOE Office of Science [DE-AC02-06CH11357]
  7. Russian Ministry of Science and Higher Education [H III-2711.2020.2]
  8. European Community's Seventh Framework Programme (FP7/2007-2013) [312284]

向作者/读者索取更多资源

A combined experimental and theoretical study was conducted on ethane and methane at high pressures, determining their crystal structures, phase transitions, and equation of state. The study resulted in the identification of pressure-induced phase transitions and provided a solid basis for discussing the relative stability of these compounds at high pressures.
We have performed a combined experimental and theoretical study of ethane and methane at high pressures of up to 120 GPa at 300 K using x-ray diffraction and Raman spectroscopies and the USPEX ab initio evolutionary structural search algorithm, respectively. For ethane, we have determined the crystallization point, for room temperature, at 2.7 GPa and also the low pressure crystal structure (phase A). This crystal structure is orientationally disordered (plastic phase) and deviates from the known crystal structures for ethane at low temperatures. Moreover, a pressure induced phase transition has been identified, for the first time, at 13.6 GPa to a monoclinic phase B, the structure of which is solved based on good agreement with the experimental results and theoretical predictions. For methane, our x-ray diffraction measurements are in agreement with the previously reported high-pressure structures and equation of state (EOS). We have determined the EOSs of ethane and methane, which provides a solid basis for the discussion of their relative stability at high pressures.

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