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Volumn 277, Issue 5328, 1997, Pages 930-933

Structure, bonding, and geochemistry of xenon at high pressures

Author keywords

[No Author keywords available]

Indexed keywords

XENON;

EID: 0030862903     PISSN: 00368075     EISSN: None     Source Type: Journal    
DOI: 10.1126/science.277.5328.930     Document Type: Article
Times cited : (101)

References (38)
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    • Experimentally, we find evidence for a topotactic relation between the two phases, which suggests a martensitic or "military" type transformation [J. W. Christian, The Theory of Transformations in Metals and Alloys, Part I (Pergamon, New York, ed. 2, 1975)]. The (111) peak of the fcc phase and the (002) peak of the hcp phase appear at the same d spacing, which implies identical orientations for the close-packed planes in the two structures [A. F. Schuch, R. L. Mills, D. A. Depatie, Phys. Rev. 165, 1032 (1968)]. A similar geometrical relation explains why three other hcp peaks, (004), (112), and (110), are also coincident with the (222), (311), and (220) fcc peaks. It is possible that the detailed transformation mechanism is sensitive to the presence of even small nonhydrostatic stresses, however, so there is no reason to infer a disagreement between experiment and theory on this point.
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    • note
    • Supported by NASA, NSF, and the U.S. Department of Energy (DOE), including grants NSF DMR-9520554 and DOE DE-AC03-76SF00098. The computations were performed on the National Energy Research Scientific Computing Center T3E at Lawrence Berkeley National Laboratory. We thank M. S. T. Bukowinski, R. J. Hemley, M. L. Klein, and R. O. Pepin for helpful discussions.


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.