We present a high-pressure study of Mg$_{1–x}$Fe$_{x}$O (ferropericlase, Fp) single crystals 0.04(1)$\leqslant x \leqslant$ 0.33(1) with a focus on ferrous iron spin-state crossover and the material behavior preceding it. Using Vegard's law and highly accurate high-pressure single-crystal experimental data, we extract the lattice parameter $a^{HS}_{FeO}$ of the “FeO high spin lattice contribution” in the MgO-FeO solid solution. We find that ferropericlases with a wide range of compositions share the same critical parameter $a_C$ (defined as the minimum $a^{HS}_{FeO}$ after which spin crossover starts). Furthermore, we discuss the effect of composition on spin crossover in ferrous iron in ferropericlase in the limits of low and moderate conc...
Using synchrotron-based X-ray diffraction, we explore characteristic signatures for nonhydrostatic s...
We have performed a series of experiments to investigate the compositional effect on the compression...
Systematic change of structural transition and high-spin (HS) to low-spin (LS) transition of Fe2+ in...
We present a high-pressure study of Mg$_{1–x}$Fe$_{x}$O (ferropericlase, Fp) single crystals 0.04(1)...
The thermodynamics properties of ferropericlase (Mg(1-x)Fe(x)O where x=0.1875) (Fp) throughout its s...
The thermodynamics properties of ferropericlase (Mg(1-x)Fe(x)O where x=0.1875) (Fp) throughout its s...
The thermodynamics properties of ferropericlase (Mg(1-x)Fe(x)O where x=0.1875) (Fp) throughout its s...
(MgFe)O is a solid solution with ferrous iron undergoing high to low spin state (HS-LS) crossover un...
The thermodynamics properties of ferropericlase (Mg1-xFexO, x = 0.1875) (Fp) throughout its spin cro...
Iron-bearing periclase is thought to represent a significant fraction of Earth's lower mantle. Howev...
Iron-bearing periclase is thought to represent a significant fraction of Earth's lower mantle. Howev...
Iron-bearing periclase is thought to represent a significant fraction of Earth’s lower mantle. Howev...
Ferropericlase (fp), (Mg$_{1-x}$Fe$_x$)O, the second most abundant mineral in the Earth's lower mant...
Iron-bearing periclase is thought to represent a significant fraction of Earth’s lower mantle. Howev...
Iron-bearing periclase is thought to represent a significant fraction of Earth’s lower mantle. Howev...
Using synchrotron-based X-ray diffraction, we explore characteristic signatures for nonhydrostatic s...
We have performed a series of experiments to investigate the compositional effect on the compression...
Systematic change of structural transition and high-spin (HS) to low-spin (LS) transition of Fe2+ in...
We present a high-pressure study of Mg$_{1–x}$Fe$_{x}$O (ferropericlase, Fp) single crystals 0.04(1)...
The thermodynamics properties of ferropericlase (Mg(1-x)Fe(x)O where x=0.1875) (Fp) throughout its s...
The thermodynamics properties of ferropericlase (Mg(1-x)Fe(x)O where x=0.1875) (Fp) throughout its s...
The thermodynamics properties of ferropericlase (Mg(1-x)Fe(x)O where x=0.1875) (Fp) throughout its s...
(MgFe)O is a solid solution with ferrous iron undergoing high to low spin state (HS-LS) crossover un...
The thermodynamics properties of ferropericlase (Mg1-xFexO, x = 0.1875) (Fp) throughout its spin cro...
Iron-bearing periclase is thought to represent a significant fraction of Earth's lower mantle. Howev...
Iron-bearing periclase is thought to represent a significant fraction of Earth's lower mantle. Howev...
Iron-bearing periclase is thought to represent a significant fraction of Earth’s lower mantle. Howev...
Ferropericlase (fp), (Mg$_{1-x}$Fe$_x$)O, the second most abundant mineral in the Earth's lower mant...
Iron-bearing periclase is thought to represent a significant fraction of Earth’s lower mantle. Howev...
Iron-bearing periclase is thought to represent a significant fraction of Earth’s lower mantle. Howev...
Using synchrotron-based X-ray diffraction, we explore characteristic signatures for nonhydrostatic s...
We have performed a series of experiments to investigate the compositional effect on the compression...
Systematic change of structural transition and high-spin (HS) to low-spin (LS) transition of Fe2+ in...