Two-phase equilibrium conditions in nanopores

Journal Article (2020)
Author(s)

Michael T. Rauter (Norwegian University of Science and Technology (NTNU))

Olav Galteland (Norwegian University of Science and Technology (NTNU))

M. Erdős (TU Delft - Engineering Thermodynamics)

Othon Moultos (TU Delft - Engineering Thermodynamics)

Thijs J H Vlugt (TU Delft - Engineering Thermodynamics)

Sondre K. Schnell (Norwegian University of Science and Technology (NTNU))

Dick Bedeaux (Norwegian University of Science and Technology (NTNU))

S. Kjelstrup (Norwegian University of Science and Technology (NTNU))

Research Group
Engineering Thermodynamics
Copyright
© 2020 Michael T. Rauter, O. Galteland, M. Erdös, O. Moultos, T.J.H. Vlugt, Sondre K. Schnell, Dick Bedeaux, Signe Kjelstrup
DOI related publication
https://doi.org/10.3390/nano10040608
More Info
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Publication Year
2020
Language
English
Copyright
© 2020 Michael T. Rauter, O. Galteland, M. Erdös, O. Moultos, T.J.H. Vlugt, Sondre K. Schnell, Dick Bedeaux, Signe Kjelstrup
Research Group
Engineering Thermodynamics
Issue number
4
Volume number
10
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Abstract

It is known that thermodynamic properties of a system change upon confinement. To know how, is important for modelling of porous media. We propose to use Hill’s systematic thermodynamic analysis of confined systems to describe two-phase equilibrium in a nanopore. The integral pressure, as defined by the compression energy of a small volume, is then central. We show that the integral pressure is constant along a slit pore with a liquid and vapor in equilibrium, when Young and Young–Laplace’s laws apply. The integral pressure of a bulk fluid in a slit pore at mechanical equilibrium can be understood as the average tangential pressure inside the pore. The pressure at mechanical equilibrium, now named differential pressure, is the average of the trace of the mechanical pressure tensor divided by three as before. Using molecular dynamics simulations, we computed the integral and differential pressures, ̂p and p, respectively, analysing the data with a growing-core methodology. The value of the bulk pressure was confirmed by Gibbs ensemble Monte Carlo simulations. The pressure difference times the volume, V, is the subdivision potential of Hill, (p − ̂p)V = ɛ. The combined simulation results confirm that the integral pressure is constant along the pore, and that ɛ/V scales with the inverse pore width. This scaling law will be useful for prediction of thermodynamic properties of confined systems in more complicated geometries.