Crystalline polymeric carbon dioxide stable at megabar pressures

被引:29
|
作者
Dziubek, Kamil F. [1 ]
Ende, Martin [2 ]
Scelta, Demetrio [1 ,3 ]
Bini, Roberto [1 ,3 ,4 ]
Mezouar, Mohamed [5 ]
Garbarino, Gaston [5 ]
Miletich, Ronald [2 ]
机构
[1] LENS, European Lab Nonlinear Spect, Via N Carrara 1, I-50019 Florence, Italy
[2] Univ Wien, Inst Mineral & Kristallog, Althanstr 14, A-1090 Vienna, Austria
[3] Natl Res Council Italy, Inst Chem OrganoMetall Cpds, ICCOM CNR, Via Madonna Piano 10, I-50019 Florence, Italy
[4] Univ Firenze, Dipartimento Chim Ugo Schiff, Via Lastruccia 3, I-50019 Florence, Italy
[5] European Synchrotron Radiat Facil, 71 Ave Martyrs,CS 40220, F-38043 Grenoble 9, France
来源
NATURE COMMUNICATIONS | 2018年 / 9卷
关键词
DEEP LOWER-MANTLE; X-RAY; PHASE V; CO2; TEMPERATURE; OXYGEN; MAGNESITE; TRANSFORMATIONS; STABILITY; HYDROGEN;
D O I
10.1038/s41467-018-05593-8
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Carbon dioxide is a widespread simple molecule in the Universe. In spite of its simplicity it has a very complex phase diagram, forming both amorphous and crystalline extended phases above 40 GPa. The stability range and nature of these phases are still debated, especially in view of their possible role within the deep carbon cycle. Here, we report static synchrotron Xray diffraction and Raman high-pressure experiments in the megabar range providing evidence for the stability of the polymeric phase V at pressure-temperature conditions relevant to the Earth's lowermost mantle. The equation of state has been extended to 120 GPa and, contrary to earlier experimental findings, neither dissociation into diamond and e-oxygen nor ionization was observed. Severe deviatoric stress and lattice deformation along with preferred orientation are removed on progressive annealing, thus suggesting CO2-V as the stable structure also above one megabar.
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页数:6
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