2005
DOI: 10.1038/nature03825
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Spin transition of iron in magnesiowüstite in the Earth's lower mantle

Abstract: Iron is the most abundant transition-metal element in the mantle and therefore plays an important role in the geochemistry and geodynamics of the Earth's interior. Pressure-induced electronic spin transitions of iron occur in magnesiowüstite, silicate perovskite and post-perovskite. Here we have studied the spin states of iron in magnesiowüstite and the isolated effects of the electronic transitions on the elasticity of magnesiowüstite with in situ X-ray emission spectroscopy and X-ray diffraction to pressures… Show more

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Cited by 330 publications
(381 citation statements)
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“…[6][7][8] ) for which Fe II exhibits a high-spin (S = 2) configuration at ambient pressure. In fact, for CoFe-PBA, the high-spin Fe II is of significantly higher energy (1.94 eV/fu) than the LS-Fe II (S = 0).…”
Section: Resultsmentioning
confidence: 99%
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“…[6][7][8] ) for which Fe II exhibits a high-spin (S = 2) configuration at ambient pressure. In fact, for CoFe-PBA, the high-spin Fe II is of significantly higher energy (1.94 eV/fu) than the LS-Fe II (S = 0).…”
Section: Resultsmentioning
confidence: 99%
“…1,2,12,13 However, neither the microscopic transition mechanisms nor the effects of Fe-vacancies, water, and alkali metals on these mechanisms are completely understood, despite considerable experimental and theoretical effort. [16][17][18][19] 6 ] does not influence the charge transfer excitation energy. 23 Here we investigate the microscopic spin transition mechanisms via an ab initio lattice model for CoFe-PBA.…”
mentioning
confidence: 99%
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“…[2][3][4] Similar to Earth's interior conditions, high-pressure techniques have emerged as efficient tools to attain structural conditions for spin change, even dealing with systems where ⌬Ӷ⌬ SCO . Although we know the relevance of the spin state of Fe 2+ in ͑Mg,Fe͒O, the second most abundant phase in lower mantle, on the radiative conductivity 5,6 or that highspin Fe 3+ ͑S =5/2͒ transits to the low-spin state ͑S =1/2͒ in Fe 2 O 3 at pressures around 50 GPa, 7,8 the problem of predicting spin-crossover pressures in materials science is still a challenge. A comprehensive characterization of high-spin to low-spin ͑or intermediate spin͒ 1 phenomena requires knowledge of the electronic structure of materials, a major problem because optical absorption measurements in extreme conditions are tricky.…”
Section: Introductionmentioning
confidence: 99%
“…Spin-transition phenomena have been intensively investigated in materials providing ligand fields close to the spin crossover. [1][2][3][4][5][6][7][8][9] Current research of this kind is focused on materials involving transition-metal complexes with C, O, or N ligands. Their strong neuphelaxetic effect makes those complexes well suited to exhibiting bistability around ambient conditions.…”
Section: Introductionmentioning
confidence: 99%