Molecular dynamics simulation of PVT properties of geological fluids and a general equation of state of nonpolar and weakly polar gases up to 2,000 K and 20,000 bar

The PVT properties of CH[sub 4] from 30-360 cm[sup 3] mol and roughly from 273-2,000 K and from 100-20,000 bar have been simulated by molecular dynamics using Lennard-Jones potentials. The simulated results compare with data within 1.5% in volume. Using these simulated values and experimental PVT da...

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Veröffentlicht in:Geochimica et cosmochimica acta 1992-10, Vol.56:10
Hauptverfasser: Zhenhao Duan, Moeller, N., Weare, J.H.
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Weare, J.H.
description The PVT properties of CH[sub 4] from 30-360 cm[sup 3] mol and roughly from 273-2,000 K and from 100-20,000 bar have been simulated by molecular dynamics using Lennard-Jones potentials. The simulated results compare with data within 1.5% in volume. Using these simulated values and experimental PVT data, an equation of state (EOS) was developed. Because of the choice of potential, a simple scaling generalizes the EOS to predict the supercritical PVT properties of CO[sub 2], N[sub 2], CO, H[sub 2], O[sub 2], and Cl[sub 2] within an average error of about 1.5%.
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1872-9533
language eng
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source Elsevier ScienceDirect Journals
subjects 580000 - Geosciences
ALKANES
CARBON COMPOUNDS
CARBON DIOXIDE
CARBON MONOXIDE
CARBON OXIDES
CHALCOGENIDES
CHLORINE
COMPUTERIZED SIMULATION
CRITICAL PRESSURE
CRITICAL TEMPERATURE
ELEMENTS
EQUATIONS
EQUATIONS OF STATE
GEOSCIENCES
HALOGENS
HYDROCARBONS
HYDROGEN
METHANE
NITROGEN
NONMETALS
ORGANIC COMPOUNDS
OXIDES
OXYGEN
OXYGEN COMPOUNDS
PHYSICAL PROPERTIES
PRESSURE EFFECTS
SIMULATION
SUPERCRITICAL STATE
TEMPERATURE EFFECTS
THERMODYNAMIC PROPERTIES
TRANSITION TEMPERATURE
title Molecular dynamics simulation of PVT properties of geological fluids and a general equation of state of nonpolar and weakly polar gases up to 2,000 K and 20,000 bar
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