Carbon in iron phases under high pressure

被引:35
作者
Huang, L
Skorodumova, NV
Belonoshko, AB
Johansson, B
Ahuja, R
机构
[1] Uppsala Univ, Dept Phys, Condensed Matter Theory Grp, S-75121 Uppsala, Sweden
[2] Royal Inst Technol, Dept Mat & Engn, S-10044 Stockholm, Sweden
[3] Royal Inst Technol, Dept Phys, Stockholm Ctr Phys Astron & Biotechnol, Condensed Matter Theory Grp, S-10044 Stockholm, Sweden
关键词
D O I
10.1029/2005GL024187
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The influence of carbon impurities on the properties of iron phases (bcc, hcp, dhcp, fcc) has been studied using the first-principles projector augmented-wave ( PAW) method for a wide pressure range. It is shown that the presence of similar to 6 at. % of interstitial carbon has a little effect on the calculated structural sequence of the iron phases under high pressure. The bcc ! hcp transition both for pure iron and iron containing carbon takes place around 9 GPa. According to the enthalpies comparison, the solubility of carbon into the iron solid is decreased by high pressure. The coexistence of iron carbide (Fe3C) + pure hcp Fe is most stable phase at high pressure compared with other phases. Based on the analysis of the pressure-density dependences for Fe3C and hcp Fe, we suggest that there might be some fraction of iron carbide present in the core.
引用
收藏
页码:1 / 4
页数:4
相关论文
共 25 条
[1]   Thermodynamics from first principles:: temperature and composition of the Earth's core [J].
Alfè, D ;
Gillan, MJ ;
Price, GD .
MINERALOGICAL MAGAZINE, 2003, 67 (01) :113-123
[2]   DENSITY + COMPOSITION OF MANTLE + CORE [J].
BIRCH, F .
JOURNAL OF GEOPHYSICAL RESEARCH, 1964, 69 (20) :4377-+
[3]   COMPOSITION OF THE EARTHS MANTLE [J].
BIRCH, F .
GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY, 1961, 4 :295-311
[4]   ELASTICITY AND CONSTITUTION OF THE EARTH INTERIOR [J].
BIRCH, F .
JOURNAL OF GEOPHYSICAL RESEARCH, 1952, 57 (02) :227-286
[5]   PROJECTOR AUGMENTED-WAVE METHOD [J].
BLOCHL, PE .
PHYSICAL REVIEW B, 1994, 50 (24) :17953-17979
[6]   MELTING, THERMAL-EXPANSION, AND PHASE-TRANSITIONS OF IRON AT HIGH-PRESSURES [J].
BOEHLER, R ;
VONBARGEN, N ;
CHOPELAS, A .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH AND PLANETS, 1990, 95 (B13) :21731-21736
[7]   WHAT THE LATEST DIFFRACTION TECHNIQUES CAN TELL US ABOUT AN OLD MATERIAL - STEEL [J].
BUTLER, BD ;
COHEN, JB .
ULTRAMICROSCOPY, 1993, 52 (3-4) :238-242
[8]   Experimental and theoretical identification of a new high-pressure TiO2 polymorph -: art. no. 275501 [J].
Dubrovinskaia, NA ;
Dubrovinsky, LS ;
Ahuja, R ;
Prokopenko, VB ;
Dmitriev, V ;
Weber, HP ;
Osorio-Guillen, JM ;
Johansson, B .
PHYSICAL REVIEW LETTERS, 2001, 87 (27) :275501-1
[9]   Experimental and theoretical identification of a new high-pressure phase of silica [J].
Dubrovinsky, LS ;
Saxena, SK ;
Lazor, P ;
Ahuja, R ;
Eriksson, O ;
Wills, JM ;
Johansson, B .
NATURE, 1997, 388 (6640) :362-365
[10]   Materials science - The hardest known oxide [J].
Dubrovinsky, LS ;
Dubrovinskaia, NA ;
Swamy, V ;
Muscat, J ;
Harrison, NM ;
Ahuja, R ;
Holm, B ;
Johansson, B .
NATURE, 2001, 410 (6829) :653-654