Molecular Dynamics of Equilibrium and Pressure-Driven Transport Properties of Water through LTA-Type Zeolites

Handle URI:
http://hdl.handle.net/10754/598874
Title:
Molecular Dynamics of Equilibrium and Pressure-Driven Transport Properties of Water through LTA-Type Zeolites
Authors:
Turgman-Cohen, Salomon; Araque, Juan C.; Hoek, Eric M. V.; Escobedo, Fernando A.
Abstract:
We consider an atomistic model to investigate the flux of water through thin Linde type A (LTA) zeolite membranes with differing surface chemistries. Using molecular dynamics, we have studied the flow of water under hydrostatic pressure through a fully hydrated LTA zeolite film (∼2.5 nm thick) capped with hydrophilic and hydrophobic moieties. Pressure drops in the 50-400 MPa range were applied across the membrane, and the flux of water was monitored for at least 15 ns of simulation time. For hydrophilic membranes, water molecules adsorb at the zeolite surface, creating a highly structured fluid layer. For hydrophobic membranes, a depletion of water molecules occurs near the water/zeolite interface. For both types of membranes, the water structure is independent of the pressure drop established in the system and the flux through the membranes is lower than that observed for the bulk zeolitic material; the latter allows an estimation of surface barrier effects to pressure-driven water transport. Mechanistically, it is observed that (i) bottlenecks form at the windows of the zeolite structure, preventing the free flow of water through the porous membrane, (ii) water molecules do not move through a cage in a single-file fashion but rather exhibit a broad range of residence times and pronounced mixing, and (iii) a periodic buildup of a pressure difference between inlet and outlet cages takes place which leads to the preferential flow of water molecules toward the low-pressure cages. © 2013 American Chemical Society.
Citation:
Turgman-Cohen S, Araque JC, Hoek EMV, Escobedo FA (2013) Molecular Dynamics of Equilibrium and Pressure-Driven Transport Properties of Water through LTA-Type Zeolites. Langmuir 29: 12389–12399. Available: http://dx.doi.org/10.1021/la402895h.
Publisher:
American Chemical Society (ACS)
Journal:
Langmuir
KAUST Grant Number:
KUS-C1-018-02
Issue Date:
8-Oct-2013
DOI:
10.1021/la402895h
PubMed ID:
24024745
Type:
Article
ISSN:
0743-7463; 1520-5827
Sponsors:
This publication was based on work supported by Award KUS-C1-018-02, made by King Abdullah University of Science and Technology (KAUST). The authors are also grateful to computer cycles supplied by the Extreme Science and Engineering Discovery Environment (XSEDE) which is supported by National Science Foundation Grant OCI-1053575
Appears in Collections:
Publications Acknowledging KAUST Support

Full metadata record

DC FieldValue Language
dc.contributor.authorTurgman-Cohen, Salomonen
dc.contributor.authorAraque, Juan C.en
dc.contributor.authorHoek, Eric M. V.en
dc.contributor.authorEscobedo, Fernando A.en
dc.date.accessioned2016-02-25T13:42:52Zen
dc.date.available2016-02-25T13:42:52Zen
dc.date.issued2013-10-08en
dc.identifier.citationTurgman-Cohen S, Araque JC, Hoek EMV, Escobedo FA (2013) Molecular Dynamics of Equilibrium and Pressure-Driven Transport Properties of Water through LTA-Type Zeolites. Langmuir 29: 12389–12399. Available: http://dx.doi.org/10.1021/la402895h.en
dc.identifier.issn0743-7463en
dc.identifier.issn1520-5827en
dc.identifier.pmid24024745en
dc.identifier.doi10.1021/la402895hen
dc.identifier.urihttp://hdl.handle.net/10754/598874en
dc.description.abstractWe consider an atomistic model to investigate the flux of water through thin Linde type A (LTA) zeolite membranes with differing surface chemistries. Using molecular dynamics, we have studied the flow of water under hydrostatic pressure through a fully hydrated LTA zeolite film (∼2.5 nm thick) capped with hydrophilic and hydrophobic moieties. Pressure drops in the 50-400 MPa range were applied across the membrane, and the flux of water was monitored for at least 15 ns of simulation time. For hydrophilic membranes, water molecules adsorb at the zeolite surface, creating a highly structured fluid layer. For hydrophobic membranes, a depletion of water molecules occurs near the water/zeolite interface. For both types of membranes, the water structure is independent of the pressure drop established in the system and the flux through the membranes is lower than that observed for the bulk zeolitic material; the latter allows an estimation of surface barrier effects to pressure-driven water transport. Mechanistically, it is observed that (i) bottlenecks form at the windows of the zeolite structure, preventing the free flow of water through the porous membrane, (ii) water molecules do not move through a cage in a single-file fashion but rather exhibit a broad range of residence times and pronounced mixing, and (iii) a periodic buildup of a pressure difference between inlet and outlet cages takes place which leads to the preferential flow of water molecules toward the low-pressure cages. © 2013 American Chemical Society.en
dc.description.sponsorshipThis publication was based on work supported by Award KUS-C1-018-02, made by King Abdullah University of Science and Technology (KAUST). The authors are also grateful to computer cycles supplied by the Extreme Science and Engineering Discovery Environment (XSEDE) which is supported by National Science Foundation Grant OCI-1053575en
dc.publisherAmerican Chemical Society (ACS)en
dc.titleMolecular Dynamics of Equilibrium and Pressure-Driven Transport Properties of Water through LTA-Type Zeolitesen
dc.typeArticleen
dc.identifier.journalLangmuiren
dc.contributor.institutionCornell University, Ithaca, United Statesen
dc.contributor.institutionUniversity of California, Los Angeles, Los Angeles, United Statesen
kaust.grant.numberKUS-C1-018-02en
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