Figure 4
X-ray emission spectra of Fe Kβ collected from a single crystal of magnesiowüstite-(Mg0.75,Fe0.25)O at high pressures. The spectrum under ambient conditions was measured outside the DAC. The spectra were normalized to unity and shifted in energy to compensate for the pressure-induced shift of the line maximum based on the main fluorescence peak (Kβ) at 7058 eV. The presence of the satellite peak () at 0, 21, 47 GPa and 300 K is characteristic of the high-spin state of iron whereas the disappearance of the satellite peak at 72 and 79 GPa indicates the occurrence of the low-spin state of ferrous iron in (Mg0.75,Fe0.25)O (Lin, Struzhkin et al., 2005). |