2006
DOI: 10.1103/physrevb.73.174208
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First-principles calculations of the structural, dynamical, and electronic properties of liquid MgO

Abstract: The structural, dynamical, and electronic properties of liquid MgO have been investigated over a wide range of pressure ͑0 to ϳ 240 GPa͒ and temperature ͑3000-10 000 K͒ using first-principles molecular dynamics ͑FPMD͒ within the framework of density-functional theory and the pseudopotential approximation. Our results show that the liquid structure is highly sensitive to compression: the Mg-O coordination number increases from 5 at zero pressure to 7 at high pressure. The Grüneisen parameter and heat capacity a… Show more

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Cited by 72 publications
(88 citation statements)
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“…We find a higher result for ⟨Z FeO ⟩ by as much as 1.0 when Fe is in the high-spin state as compared to the low-spin state, which reflects the larger spatial extent of the 3d-like orbitals in the former electronic configuration and hence a larger ionic radius. The Mg-O coordination is very close to previous ab initio results on pure MgO [15] and appears independent of the spin state of Fe in the liquid. We find ⟨Z MgO ⟩ ≈ 5.2 at 11.4Å 3 /atom, very close to the experimental value of 4.95 at the same atomic volume [47].…”
Section: Mechanical Propertiessupporting
confidence: 72%
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“…We find a higher result for ⟨Z FeO ⟩ by as much as 1.0 when Fe is in the high-spin state as compared to the low-spin state, which reflects the larger spatial extent of the 3d-like orbitals in the former electronic configuration and hence a larger ionic radius. The Mg-O coordination is very close to previous ab initio results on pure MgO [15] and appears independent of the spin state of Fe in the liquid. We find ⟨Z MgO ⟩ ≈ 5.2 at 11.4Å 3 /atom, very close to the experimental value of 4.95 at the same atomic volume [47].…”
Section: Mechanical Propertiessupporting
confidence: 72%
“…3. The diffusivity of (Mg,Fe)O appears thus overall fairly similar to that of MgO [15], the small but systematic difference being possibly attributable to the difference in exchange-correlation functional (PBEsol + U vs LDA) and the different chemical composition. The diffusivities of high-spin Fe, low-spin Fe, Mg, and O reveal a weak dependence of D on element and spin state [31], the weak dependence on spin state being at odds with earlier results on Fe diffusivity in crystalline (Mg,Fe)O, where the diffusivity was found to vary by a factor of three between high-spin and low-spin Fe [42].…”
Section: B Diffusivitymentioning
confidence: 80%
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“…With production runs of only 5ps, it is not possible to check with much accuracy if the imposed density (see below) for the melt under investigation corresponds to P~0 in the simulation. On the other hand it is known that the use of the generalized gradient approximation (GGA) for the exchange correlation energy tends to underestimate by ~2-3% the density of silicate minerals when the use of the local density approximation (LDA), a priori less accurate, leads (fortuitously) to a better estimation [8,10]. In fact GGA remedies some of the weaknesses of LDA, and especially its tendency to overbinding, and the slight underestimation of the density comes from a lack of dispersion energy between atoms [23,24].…”
Section: Introductionmentioning
confidence: 99%
“…With regard to mantle minerals and their melts, the number of studies using ab initio molecular dynamics simulations (AIMD) is increasing late years and now cover a rather large range of composition (e.g. SiO2 [5,6], MgO [7,8], MgSiO3 [9,10], Mg2SiO4 [11][12], Na2SiO4 [13] and CaO(0.12)Al2O3(0.21)SiO2(0.67) [14]). …”
Section: Introductionmentioning
confidence: 99%