Related Content
Search Google Scholar for:
|
|
Science 31 January 1997: Vol. 275. no. 5300, pp. 654 - 657 DOI: 10.1126/science.275.5300.654
|
|
Reports
Magnetic Collapse in Transition Metal Oxides at High Pressure: Implications for the Earth
Ronald E. Cohen,
*
I. I. Mazin,
Donald G. Isaak
Magnetic collapse in transition metal ions is predicted from
first-principles computations at pressures reached in the Earth's lower mantle and core. Magnetic collapse would lead to marked changes
in geophysically important properties, such as elasticity and
conductivity, and also to different geochemical behavior, such as
element partitioning, than estimated by extrapolating low-pressure
data, and thus change the understanding of Earth's structure and
evolution. Magnetic collapse results from band widening rather than
from changes in crystal field splitting under pressure. Seismic
anomalies in the outer core and the lowermost mantle may be due to
magnetic collapse of ferrous iron, dissolved in iron liquid in the
outer core, and in solution in magnesiowüstite in the lowermost
mantle.
R. E. Cohen and I. I. Mazin, Geophysical Laboratory and Center for
High-Pressure Research, Carnegie Institution of Washington, 5251 Broad
Branch Road, NW, Washington, DC 20015, USA.
D. G. Isaak, Institute of Geophysics and Planetary Physics, University
of California at Los Angeles, Los Angeles, CA 90095-1567, and
Department of Mathematics and Physics, Azusa Pacific University, Azusa,
CA 91702, USA.
*
To whom correspondence should be addressed.
Visit the authors' site for additional information
Read the Full Text
THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
- Electronic and magnetic structures of the postperovskite-type Fe2O3 and implications for planetary magnetic records and deep interiors.
- S.-H. Shim, A. Bengtson, D. Morgan, W. Sturhahn, K. Catalli, J. Zhao, M. Lerche, and V. Prakapenka (2009)
PNAS
106, 5508-5512
| Abstract »
| Full Text »
| PDF »
- Effect of A-site cation radius on ordering of BX6 octahedra in (K,Na)MgF3 perovskite.
- C. D. Martin, S. Chaudhuri, C. P. Grey, and J. B. Parise (2005)
American Mineralogist
90, 1522-1533
| Abstract »
| Full Text »
| PDF »
- A synchrotron Mossbauer spectroscopy study of (Mg,Fe)SiO3 perovskite up to 120 GPa.
- J. M. Jackson, W. Sturhahn, G. Shen, J. Zhao, M. Y. Hu, D. Errandonea, J. D. Bass, and Y. Fei (2005)
American Mineralogist
90, 199-205
| Abstract »
| Full Text »
| PDF »
- Electronic spin state of iron in lower mantle perovskite.
- J. Li, V. V. Struzhkin, H.-k. Mao, J. Shu, R. J. Hemley, Y. Fei, B. Mysen, P. Dera, V. Prakapenka, and G. Shen (2004)
PNAS
101, 14027-14030
| Abstract »
| Full Text »
| PDF »
- Iron Partitioning in Earth's Mantle: Toward a Deep Lower Mantle Discontinuity.
- J. Badro, G. Fiquet, F. Guyot, J.-P. Rueff, V. V. Struzhkin, G. Vanko, and G. Monaco (2003)
Science
300, 789-791
| Abstract »
| Full Text »
| PDF »
- Stability of magnesiowustite in Earth's lower mantle.
- J.-F. Lin, D. L. Heinz, H.-k. Mao, R. J. Hemley, J. M. Devine, J. Li, and G. Shen (2003)
PNAS
100, 4405-4408
| Abstract »
| Full Text »
| PDF »
- Structure, metal-insulator transitions, and magnetic properties of FeO at high pressures.
- S. A. Gramsch, S. A. Gramsch, R. E. Cohen, and S. Y. Savrasov (2003)
American Mineralogist
88, 257-261
| Abstract »
| Full Text »
| PDF »
- New windows on earth and planetary interiors.
- R. J. Hemley and H. K. Mao (2002)
Mineralogical Magazine
66, 791-811
| Abstract »
| Full Text »
| PDF »
- Stability of Ferropericlase in the Lower Mantle.
- L. S. Dubrovinsky, N. A. Dubrovinskaia, S. K. Saxena, H. Annersten, E. Hålenius, H. Harryson, F. Tutti, S. Rekhi, and T. L. Bihan (2000)
Science
289, 430-432
| Abstract »
| Full Text »
- Pressure-induced transformations in deep mantle and core minerals.
- R. J. Hemley, H. K. Mao, and S. A. Gramsch (2000)
Mineralogical Magazine
64, 157-184
| Abstract »
| Full Text »
| PDF »
|
|