Sangam: A Confluence of Knowledge Streams

Framework water capacity and infiltration pressure of MFI zeolites

Show simple item record

dc.contributor Massachusetts Institute of Technology. Department of Mechanical Engineering
dc.contributor Wang, Evelyn N.
dc.contributor Humplik, Thomas
dc.contributor Raj, Rishi
dc.contributor Maroo, Shalabh
dc.contributor Laoui, Tahar
dc.contributor Wang, Evelyn
dc.creator Humplik, Thomas
dc.creator Raj, Rishi
dc.creator Maroo, Shalabh
dc.creator Laoui, Tahar
dc.creator Wang, Evelyn
dc.date 2017-04-13T18:05:09Z
dc.date 2017-04-13T18:05:09Z
dc.date 2014-01
dc.date 2013-12
dc.date.accessioned 2023-03-01T18:10:36Z
dc.date.available 2023-03-01T18:10:36Z
dc.identifier 1387-1811
dc.identifier http://hdl.handle.net/1721.1/108123
dc.identifier Humplik, Thomas; Raj, Rishi; Maroo, Shalabh C.; Laoui, Tahar and Wang, Evelyn N. “Framework Water Capacity and Infiltration Pressure of MFI Zeolites.” Microporous and Mesoporous Materials 190 (May 2014): 84–91. © 2014 Elsevier Inc
dc.identifier https://orcid.org/0000-0001-9482-2547
dc.identifier https://orcid.org/0000-0001-7045-1200
dc.identifier.uri http://localhost:8080/xmlui/handle/CUHPOERS/279037
dc.description The high specific surface area and sub-nanometer to nanometer pore dimensions of microporous materials (pores <2 nm) can be exploited to improve a variety of applications such as separation technologies, energy storage, and fuel cells. For example, the ≈5.5 Å diameter pore of MFI (Mobil Five) zeolites has been proposed as a molecular sieve for water-based separation techniques. However, results from past experimental and simulation studies have been inconsistent, even for basic quantities such as the framework water capacity and the pressure at which the MFI zeolite pores become water-saturated (infiltration pressure). In this work, we elucidate the underlying mechanisms behind such discrepancies via combined water adsorption and high-pressure infiltration (or intrusion) experiments on various MFI zeolites where the characteristic crystal dimension was varied from nano (≈10 nm) to micro (≈10 μm) scales. Detailed characterization techniques were utilized to demonstrate the presence of non-crystalline silica regions in <100 nm zeolites. Accordingly, an estimated decrease of up to 50% in the framework water capacity was observed for these zeolites when compared to the fully-crystallized larger zeolites, where 35 ± 2 water molecules were required to saturate a unit cell. On the other hand, the water infiltration pressure for all of the zeolites was ≈95–100 MPa despite the differences in the synthesis procedure, indicating uniformity in the crystallized pore structure and surface chemistry. These results are an essential first step towards investigating water transport mechanisms within the sub-nanometer pores and can be used to validate and improve upon existing molecular simulations in order to obtain design guidelines for practical applications such as water-based separation technologies.
dc.description National Science Foundation (U.S.) (ECS-0335765)
dc.format application/pdf
dc.language en_US
dc.publisher Elsevier
dc.relation http://dx.doi.org/10.1016/j.micromeso.2014.01.026
dc.relation Microporous and Mesoporous Materials
dc.rights Creative Commons Attribution-NonCommercial-NoDerivs License
dc.rights http://creativecommons.org/licenses/by-nc-nd/4.0/
dc.source Prof. Evelyn Wang
dc.title Framework water capacity and infiltration pressure of MFI zeolites
dc.type Article
dc.type http://purl.org/eprint/type/JournalArticle


Files in this item

Files Size Format View
Wang_Framework water.pdf 1.557Mb application/pdf View/Open

This item appears in the following Collection(s)

Show simple item record

Search DSpace


Advanced Search

Browse