A computer simulation study of the effect of pressure on Mg diffusion in forsterite

Computer simulation techniques were used to investigate the effect of pressure on magnesium diffusionin forsterite between 0 and 10 GPa. We studied the diffusion path along the c crystallographic axis (we always refer to the Pbnm system) via a vacancy mechanism. Using a Mott-Littleton approach withi...

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Main Authors: Bejina, F., Blanchard, M., Wright, Kathleen, Price, D.
Format: Journal Article
Published: Elsevier 2009
Online Access:http://hdl.handle.net/20.500.11937/33239
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author Bejina, F.
Blanchard, M.
Wright, Kathleen
Price, D.
author_facet Bejina, F.
Blanchard, M.
Wright, Kathleen
Price, D.
author_sort Bejina, F.
building Curtin Institutional Repository
collection Online Access
description Computer simulation techniques were used to investigate the effect of pressure on magnesium diffusionin forsterite between 0 and 10 GPa. We studied the diffusion path along the c crystallographic axis (we always refer to the Pbnm system) via a vacancy mechanism. Using a Mott-Littleton approach withinthe code GULP, we were able to precisely map the diffusion path of a Mg vacancy and we found theactivation energy, E = 3.97 eV at 0 GPa (with Ef = 3.35 eV for the formation energy and Em = 0.62 eV for the migration) and E = 4.46 eV at 10 GPa (Ef = 3.81 eV and Em = 0.65 eV). Preliminary results using the supercell technique gave the same saddle point coordinates and energies. This saddle point of the Mg vacancy diffusion found with GULP was then introduced in an ab initio code, confirming the values of the migration energy both at 0 and 10 GPa. We were therefore able to estimate the activation volume (V) to be around 5 cm3/mol and d(V)/dP = 0. The effect of pressure applies mostly on defect formation and little on migration.
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spelling curtin-20.500.11937-332392017-09-13T16:07:59Z A computer simulation study of the effect of pressure on Mg diffusion in forsterite Bejina, F. Blanchard, M. Wright, Kathleen Price, D. Computer simulation techniques were used to investigate the effect of pressure on magnesium diffusionin forsterite between 0 and 10 GPa. We studied the diffusion path along the c crystallographic axis (we always refer to the Pbnm system) via a vacancy mechanism. Using a Mott-Littleton approach withinthe code GULP, we were able to precisely map the diffusion path of a Mg vacancy and we found theactivation energy, E = 3.97 eV at 0 GPa (with Ef = 3.35 eV for the formation energy and Em = 0.62 eV for the migration) and E = 4.46 eV at 10 GPa (Ef = 3.81 eV and Em = 0.65 eV). Preliminary results using the supercell technique gave the same saddle point coordinates and energies. This saddle point of the Mg vacancy diffusion found with GULP was then introduced in an ab initio code, confirming the values of the migration energy both at 0 and 10 GPa. We were therefore able to estimate the activation volume (V) to be around 5 cm3/mol and d(V)/dP = 0. The effect of pressure applies mostly on defect formation and little on migration. 2009 Journal Article http://hdl.handle.net/20.500.11937/33239 10.1016/j.pepi.2008.04.008 Elsevier fulltext
spellingShingle Bejina, F.
Blanchard, M.
Wright, Kathleen
Price, D.
A computer simulation study of the effect of pressure on Mg diffusion in forsterite
title A computer simulation study of the effect of pressure on Mg diffusion in forsterite
title_full A computer simulation study of the effect of pressure on Mg diffusion in forsterite
title_fullStr A computer simulation study of the effect of pressure on Mg diffusion in forsterite
title_full_unstemmed A computer simulation study of the effect of pressure on Mg diffusion in forsterite
title_short A computer simulation study of the effect of pressure on Mg diffusion in forsterite
title_sort computer simulation study of the effect of pressure on mg diffusion in forsterite
url http://hdl.handle.net/20.500.11937/33239