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A deeper and hotter Martian core-mantle differentiation inferred from . . . In this study, we aim to constrain the Martian core-mantle differentiation by examining FeO partitioning between core and mantle materials, incorporating improved Martian compositional data from the InSight mission Using ab initio thermodynamic techniques, we calculated the FeO partition coefficient between liquid iron and silicate melt
Equation of state and phase diagram of FeO - ScienceDirect Wüstite, Fe 1 − x O, is an important component in the mineralogy of Earth's lower mantle and may also be a component in the core Therefore the high pressure, high temperature behavior of FeO, including its phase diagram and equation of state, is essential knowledge for understanding the properties and evolution of Earth's deep interior We performed X-ray diffraction measurements using a
Facile synthesis and electrochemical properties of FeO Fe (OH) By using the surfactant-assisted method for synthesizing FeO Fe (OH) 3 nanosheets, we identified the synthesis conditions that simultaneously provide excellent electrochemical properties and surface stability to the nanosheets [35], [36], [37]
Properties evaluation of electric smelting furnace slag: Viscosity and . . . This study investigated the viscosity and sulfide capacity of electric smelting furnace (ESF) slag (CaO-SiO2 -6wt %MgO-10 wt%Al 2 O 3-FeO) with a basicity of 0 8 through cylinder rotating method and gas-slag equilibrium experiments Additionally, the high-temperature structure of the slag was analyzed using FTIR and Raman spectroscopy The results showed that as the FeO content increased from
High pressure and high temperature phase transitions of FeO We investigated the phase transitions of FeO at high pressure and high temperature up to 87 GPa and 1730 K by in situ synchrotron X-ray diffraction measurements in a laser-heated diamond anvil cell (DAC) The results demonstrated that the NaCl-type (B1) structure of FeO undergoes transition to the NiAs-type (B8) structure above 70 GPa at 1600 K The density increase across this transition is
Iron-rich Fe–O compounds at Earth’s core pressures Thus far, iron monoxide (FeO) is the only known stoichiometric compound in the Fe–FeO system, and the existence of iron-rich Fen O compounds has long been speculated Here, we report that iron reacts with FeO and Fe 2 O 3 at 220–260 GPa and 3000–3500 K in laser-heated diamond anvil cells