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Tunable High-Pressure Field Operating on a Cationic Biphenyl Derivative Intercalated in Clay Minerals
We propose a methodology for applying a pseudo uniaxial pressure to an organic molecule under ordinary temperature and pressure, namely by intercalation into smectites. The pseudo pressure on a biphenyl derivative (BP) was estimated from the averaged dihedral angle around the central bond of BP. In...
Autores principales: | , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2017
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5550449/ https://www.ncbi.nlm.nih.gov/pubmed/28794416 http://dx.doi.org/10.1038/s41598-017-08064-0 |
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author | Tominaga, Makoto Nishioka, Yukihiro Tani, Seiji Suzuki, Yasutaka Kawamata, Jun |
author_facet | Tominaga, Makoto Nishioka, Yukihiro Tani, Seiji Suzuki, Yasutaka Kawamata, Jun |
author_sort | Tominaga, Makoto |
collection | PubMed |
description | We propose a methodology for applying a pseudo uniaxial pressure to an organic molecule under ordinary temperature and pressure, namely by intercalation into smectites. The pseudo pressure on a biphenyl derivative (BP) was estimated from the averaged dihedral angle around the central bond of BP. In a high hydrostatic pressure field, biphenyl takes a planar conformation. In the interlayer space of synthetic saponite (SSA), the averaged dihedral angle of BP at a loading level of 27% versus the cation exchange capacity was ~26.3°, which indicates that the pseudo pressure applied to BP in the SSA interlayer space corresponds to 0.99 GPa. The high pseudo-pressure field in the interlayer space of SSA was also confirmed by absorption measurements. The dihedral angle around the central bond of the biphenyl moiety decreased to enhance the planarity of the molecule, mainly in response to the electrostatic force that operates between the negatively charged SSA layer and the interlayer cation. The pseudo pressure operating on BP in the smectite interlayer space could be controlled by varying the smectite layer charge density and/or the BP loading level. By using this methodology, controllable pseudo high-pressure properties of organic molecules can be obtained at ordinary temperatures and pressures. |
format | Online Article Text |
id | pubmed-5550449 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2017 |
publisher | Nature Publishing Group UK |
record_format | MEDLINE/PubMed |
spelling | pubmed-55504492017-08-11 Tunable High-Pressure Field Operating on a Cationic Biphenyl Derivative Intercalated in Clay Minerals Tominaga, Makoto Nishioka, Yukihiro Tani, Seiji Suzuki, Yasutaka Kawamata, Jun Sci Rep Article We propose a methodology for applying a pseudo uniaxial pressure to an organic molecule under ordinary temperature and pressure, namely by intercalation into smectites. The pseudo pressure on a biphenyl derivative (BP) was estimated from the averaged dihedral angle around the central bond of BP. In a high hydrostatic pressure field, biphenyl takes a planar conformation. In the interlayer space of synthetic saponite (SSA), the averaged dihedral angle of BP at a loading level of 27% versus the cation exchange capacity was ~26.3°, which indicates that the pseudo pressure applied to BP in the SSA interlayer space corresponds to 0.99 GPa. The high pseudo-pressure field in the interlayer space of SSA was also confirmed by absorption measurements. The dihedral angle around the central bond of the biphenyl moiety decreased to enhance the planarity of the molecule, mainly in response to the electrostatic force that operates between the negatively charged SSA layer and the interlayer cation. The pseudo pressure operating on BP in the smectite interlayer space could be controlled by varying the smectite layer charge density and/or the BP loading level. By using this methodology, controllable pseudo high-pressure properties of organic molecules can be obtained at ordinary temperatures and pressures. Nature Publishing Group UK 2017-08-09 /pmc/articles/PMC5550449/ /pubmed/28794416 http://dx.doi.org/10.1038/s41598-017-08064-0 Text en © The Author(s) 2017 Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/. |
spellingShingle | Article Tominaga, Makoto Nishioka, Yukihiro Tani, Seiji Suzuki, Yasutaka Kawamata, Jun Tunable High-Pressure Field Operating on a Cationic Biphenyl Derivative Intercalated in Clay Minerals |
title | Tunable High-Pressure Field Operating on a Cationic Biphenyl Derivative Intercalated in Clay Minerals |
title_full | Tunable High-Pressure Field Operating on a Cationic Biphenyl Derivative Intercalated in Clay Minerals |
title_fullStr | Tunable High-Pressure Field Operating on a Cationic Biphenyl Derivative Intercalated in Clay Minerals |
title_full_unstemmed | Tunable High-Pressure Field Operating on a Cationic Biphenyl Derivative Intercalated in Clay Minerals |
title_short | Tunable High-Pressure Field Operating on a Cationic Biphenyl Derivative Intercalated in Clay Minerals |
title_sort | tunable high-pressure field operating on a cationic biphenyl derivative intercalated in clay minerals |
topic | Article |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5550449/ https://www.ncbi.nlm.nih.gov/pubmed/28794416 http://dx.doi.org/10.1038/s41598-017-08064-0 |
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