Abstract
Molecular dynamics (MD) simulations of the thermodynamic properties of Al/Si-ordered plagioclase were performed for two different crystallographic configurations: a solid solution structure and a lamellar structure. MD-simulated plagioclase feldspar solid solution has three space groups -C1̅ - , I1̅-, and P1̅ - at 300 K, and two space groups -C1̅ - and I1̅ - at higher temperatures. In addition, the MD-simulated, composition-dependent I1̅-C1̅ and P1̅-I1̅ phase transitions are non-first order. However, the temperature-dependent I1̅ - C1̅ phase transition is not observed for any plagioclase composition. The calculated excess enthalpy and excess Gibbs free energy of the MD-simulated solid solution structure are convex upward, and for a given plagioclase composition the excess Gibbs free energy of the MD-simulated lamellar structure is smaller than that of the MD-simulated solid solution structure. These results indicate that a lamellar structure (created by phase separation) consisting of fully ordered albite and anorthite is more stable than the solid solution structure, which consists of randomly distributed clusters of both phases. Therefore, when plagioclase feldspar is heated for a long period of time at a low temperature, phase separation between pure albite and pure anorthite can be expected if equilibrium is achieved.
© 2015 by Walter de Gruyter Berlin/Boston
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Articles in the same Issue
- Measurement of crystal size distributions
- Pressure dependence of the solubility of Ar and Kr in melts of the system SiO2-NaAlSi2O6
- Solubility behavior of water in haploandesitic melts at high pressure and high temperature
- Proton-containing defects at forsterite {010} tilt grain boundaries and stepped surfaces
- Incorporation of Fe3+ into forsterite and wadsleyite
- Molecular dynamics simulation of Al/Si-ordered plagioclase feldspar
- Cation ordering and structural variations with temperature in MgAl2O4 spinel: An X-ray single-crystal study
- Aluminium coordination in tektites: A XANES study
- Crystal structure of Cr-mullite
- Structure of synthetic 2-line ferrihydrite by electron nanodiffraction
- Transmission electron microscopy study of gaudefroyite, Ca8Mn6 3+[(BO3)6(CO3)2O6]
- Nano- to micro-scale decompression products in ultrahigh-pressure phengite: HRTEM and AEM study, and some petrological implications
- New insights into the mechanism for chloritization of biotite using polytype analysis
- The dissolution of hectorite: In-situ, real-time observations using atomic force microscopy
- Quantification of minor phases in growth kinetics experiments with powder X-ray diffraction
- Illite-smectite structural changes during metamorphism in black Cambrian Alum shales from the Baltic area
- The tremolite-actinolite-ferro–actinolite series: Systematic relationships among cell parameters, composition, optical properties, and habit, and evidence of discontinuities
- Cordierite I: The coordination of Fe2+
- Cordierite II: The role of CO2 and H2O
- Crystal chemical variations in Li- and Fe-rich micas from Pikes Peak batholith (central Colorado)
- The crystal structure of TlAlSiO4: The role of inert pairs in exclusion of Tl from silicate minerals
- The structure of agrinierite: a Sr-containing uranyl oxide hydrate mineral
- The crystal structure of namibite, Cu(BiO)2VO4(OH), and revision of its symmetry
- The crystal structure of pararobertsite and its relationship to mitridatite
- Description and crystal structure of cabalzarite Ca(Mg,Al,Fe)2(AsO4)2(H2O,OH)2, a new mineral of the tsumcorite group
- Tegengrenite, a new, rhombohedral spinel-related Sb mineral from the Jakobsberg Fe-Mn deposit, Värmland, Sweden