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Volumn 275, Issue 5304, 1997, Pages 1288-1290

Dissociation of methane into hydrocarbons at extreme (planetary) pressure and temperature

Author keywords

[No Author keywords available]

Indexed keywords

HYDROCARBON; METHANE;

EID: 0031055530     PISSN: 00368075     EISSN: None     Source Type: Journal    
DOI: 10.1126/science.275.5304.1288     Document Type: Article
Times cited : (156)

References (29)
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    • note
    • The simulation cell is allowed to vary in shape and volume, driven by the quantum mechanically calculated internal stress (21). The ion-electron interaction is modeled with a fully nonlocal pseudopotential for carbon and a local pseudopotential for hydrogen. Electron-electron interactions are treated within the local density approximation, with gradient corrections as described in (22). A plane-wave basis set with a kinetic energy cutoff of 40 rydberg has been used for the electronic wave functions, which are assumed to have the same periodicity as the (varying) simulation cell.
  • 10
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    • note
    • 4 equation of state at 20 GPa and 2000 K.
  • 11
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    • note
    • The time scale of our simulations is such that a few hundred C-H stretching oscillations and a few tens of molecular collisions take place in each run. Although this is typically a sufficient time scale for thermalization, and in fact dissociation took place in a fraction of a picosecond, processes like segregation and diffusion occur on a longer time scale. These processes are energetically minor in comparison with dissociation and will not significantly alter the dissociation picture as proposed.
  • 13
    • 0000171469 scopus 로고
    • W. J. Nellis et al., Science 240, 779 (1988).
    • (1988) Science , vol.240 , pp. 779
    • Nellis, W.J.1
  • 16
    • 1842360222 scopus 로고    scopus 로고
    • note
    • Mixtures, of course, do not represent a well-defined state at T = 0. Their enthalpy is an upper bound to that of the true low-temperature system, where single phases are likely to prevail.
  • 17
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    • note
    • 4 molecule.
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    • note
    • 4 dissociation in forthcoming low-temperature diamond-anvil cell experiments.
  • 21
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    • 2 do not withstand the pressure conditions of the middle ice layers (23).
  • 23
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    • A. D. Becke, Phys. Rev. A 38, 3098 (1988); J. P. Perdew, Phys. Rev. B 33, 8822 (1986).
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    • Becke, A.D.1
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    • A. D. Becke, Phys. Rev. A 38, 3098 (1988); J. P. Perdew, Phys. Rev. B 33, 8822 (1986).
    • (1986) Phys. Rev. B , vol.33 , pp. 8822
    • Perdew, J.P.1
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    • note
    • 4 and hydrocarbon mixtures were obtained from low-temperature simulations. Results for diamond and hydrogen were obtained from standard total-energy calculations carried out separately, with the same level of accuracy, for carbon (24) and for hydrogen (25).
  • 29
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    • note
    • We acknowledge useful discussions with J. Kohanoff. The work at SISSA was partly supported by the European Commission and the Italian Research Council.


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.