Stability of K-montmorillonite hydrates: Hybrid MC simulations

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dc.creatorOdriozola, G.
dc.creatorAguilar, J. F.
dc.date2005-11-09
dc.date.accessioned2026-07-07T06:52:16Z
dc.date.available2026-07-07T06:52:16Z
dc.descriptionNPzzT and MuPzzT simulations of K-montmorillonite hydrates were performed employing hybrid Monte Carlo simulations. Two condition sets were studied, P=1 atm and T= 300 K (ground level conditions), and P=600 atm and T= 394 K; this last condition mimics a burial depth close to 4 km. For these conditions, swelling curves as a function of the reservoir water vapor pressure were built. We found the single layer K-montmorillonite hydrate stable for high vapor pressures for both, burial and ground level conditions. A simple explanation for this high stability is given.
dc.description11 pages, 11 figures
dc.identifierhttps://arxiv.org/abs/physics/0511081
dc.identifierhttp://arxiv.org/abs/physics/0511081
dc.identifier.urihttp://salesiana.dossiersoluciones.com/handle/123456789/105251
dc.subjectChemical Physics
dc.titleStability of K-montmorillonite hydrates: Hybrid MC simulations
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