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Ming Geng

Publications and source records attributed to Ming Geng.

5 recordsLinked to original sources

Influence of electronic entropy on Hellmann-Feynman forces in ab initio molecular dynamics with large temperature changes

The Z method is a popular atomistic simulation method for determining the melting temperature where a sequence of molecular dynamics runs are carried out to target the lowest system energy where the solid always melts. Homogeneous melting at the limit of critical superheating, Th, is accompanied by a drop in temperature as kinetic energy is converted to potential energy and the equilibrium melting temperature, Tm, can be calculated directly from the liquid state. Implementation of the Z method interfaced with modern ab initio electronic structure packages use Hellmann-Feynman forces to propagate the ions in the microcanonical(NVE) ensemble where the Mermin free energy plus the ionic kinetic energy is conserved. The electronic temperature, Tel, is kept fixed along the trajectory which may introduce some spurious ion-electron interactions in MD runs with large temperature changes such as often seen in homogeneous melting and freezing processes in the NVE ensemble. We estimate systematic errors in the calculated melting temperature to choice of Tel for two main mantle components, SiO2 and CaSiO3 at high pressure. Comparison of the calculated melting temperature from runs where the Tel=Th and Tel=Tm representing reasonable upper and lower boundaries respectively to choice of Tel shows that the difference in melting temperature is 200-300 K for our two test systems. The melting temperature decreases with increasing Tel due to the increasing entropic stabilisation of the liquid and the systems melts typically about 3 times faster in MD runs with Tel = Th compared to runs where Tel = Tm. A careful choice of electron temperature in BOMD simulations where the ions are propagated using Hellmann-Feynamn forces with the Mermin free energy + the ionic kinetic energy being conserved is therefore essential for the critical evaluation of the Z method and in particular at very high temperatures.

cond-mat.mtrl-sci

Ab initio constraints on silica melting to 500 GPa

The melting curve of pure silica (SiO$_2$) was determined using {\it ab initio} density functional theory together with the solid-liquid coexisting approach, thermodynamic integration and the Z method. The melting curves are consistent with a smooth slow increase in a large region from 50 GPa (dT/dP $\approx$ 15 K/GPa) to about 500 GPa (dT/dP $\approx$ 5 K/GPa) without any abrupt changes at around 120 GPa and 300 GPa as seen in some recent experimental and computational studies. The topography of the melting curve above 50 GPa is consistent with a gradual change in the distribution of the Si coordination numbers in the liquid state and the absence of large changes in the density following solid-solid phase transitions. The pair distribution functions show that the structural correlation in the liquid is mainly short-ranged and that the Si-O bond is stiff. The densification of the melt structure with pressure above 50 GPa is therefore due to an increase in 7- and 8-fold coordinated silicon.

cond-mat.mtrl-sci

Surface sites drive Fe enrichment at reactive olivine interfaces

Calculations based on density functional theory and statistical mechanics reveal how Fe site preference in olivine is altered at interfaces. Although the M1 site is favoured in bulk olivine, surface metal sites provide greater stabilisation for high-spin Fe2+. This enrichment accounts for the enhanced reactivity of olivine interfaces towards dissolution, carbonation and catalysis.

cond-mat.mtrl-sci

Density functional theory calculation and thermodynamic analysis of the bridgmanite surface structure

Bridgmanite, a high temperature and pressure form of $MgSiO_3$, is believed to be Earth's most abundant mineral and responsible for the observed seismic anisotropy in the mantle. Little is known about surfaces of bridgmanite but knowledge of the most stable surface terminations is important for understanding various geochemical processes as well as likely slip planes. A density functional theory based thermodynamic approach is used here to establish the range of stability of bridgmanite as well as possible termination structures of the (001), (010), (100) and (011) surfaces as a function of the chemical potential of oxygen and magnesium. The results presented provide a basis for further theoretical studies of the chemical processes on bridgmanite surfaces in the Earth's mantle and slip plane analysis.

physics.chem-ph

Density functional theory calculations and thermodynamic analysis of the forsterite $Mg_{2}SiO_{4}$(010) surface

The stability of possible termination structures for the (010) surface of forsterite, $ Mg_2SiO_4 $, is studied using a density functional theory (DFT) based thermodynamic approach. The DFT calculations are used to estimate the surface Gibbs free energy of various surface structures and compare their stability as a function of the chemical environment. Among 9 possible terminations, the SiO-II, M2, O-II terminations are found to be most stable as conditions range from Mg-poor to Mg-rich. This relative stability order remains the same at an elevated temperature. The surface phase diagram obtained provides ground for further theoretical studies of chemical processes on forsterite surfaces in terrestrial planets.

physics.chem-ph