Fluorine chemistry at extreme conditions: Possible synthesis of HgF4

By irradiating a pressurized mixture of a fluorine-bearing compound (XeF2) and HgF2 with synchrotron hard x-rays (>7 keV) inside a diamond anvil cell, we have observed dramatic changes in the far-infrared spectrum within the 30-35 GPa pressure range which suggest that we may have formed HgF4 in t...

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Main Authors: Michael G. Pravica, Sarah Schyck, Blake Harris, Petrika Cifligu, Eunja Kim, Brant Billinghurst
Format: Article
Language:English
Published: Papers in Physics 2019-02-01
Series:Papers in Physics
Subjects:
Online Access:https://www.papersinphysics.org/papersinphysics/article/view/478/278
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spelling doaj-fc1a8320895d4b878a59ef00ac2d0b992020-11-25T00:52:15ZengPapers in PhysicsPapers in Physics1852-42491852-42492019-02-011111000110.4279/pip.110001Fluorine chemistry at extreme conditions: Possible synthesis of HgF4Michael G. PravicaSarah SchyckBlake HarrisPetrika CifliguEunja KimBrant BillinghurstBy irradiating a pressurized mixture of a fluorine-bearing compound (XeF2) and HgF2 with synchrotron hard x-rays (>7 keV) inside a diamond anvil cell, we have observed dramatic changes in the far-infrared spectrum within the 30-35 GPa pressure range which suggest that we may have formed HgF4 in the following way: XeF2hv−→Xe+F2 (photochemically) and HgF2+F2→HgF4 (30 GPa < P < 35 GPa). This lends credence to recent theoretical calculations by Botana et al. that suggest that Hg may behave as a transition metal at high pressure in an environment with an excess of molecular fluorine. The spectral changes were observed to be reversible during pressure cycling above and below the above mentioned pressure range until a certain point when we suspect that molecular fluorine diffused out of the sample at lower pressure. Upon pressure release, HgF2 and trace XeF2 were observed to be remaining in the sample chamber suggesting that much of the Xe and F2 diffused and leaked out from the sample chamber.https://www.papersinphysics.org/papersinphysics/article/view/478/278fluorine chemistry at extreme conditionsmercury transition metal behaviordiamond anvil cellhigh pressureinfrared spectroscopy
collection DOAJ
language English
format Article
sources DOAJ
author Michael G. Pravica
Sarah Schyck
Blake Harris
Petrika Cifligu
Eunja Kim
Brant Billinghurst
spellingShingle Michael G. Pravica
Sarah Schyck
Blake Harris
Petrika Cifligu
Eunja Kim
Brant Billinghurst
Fluorine chemistry at extreme conditions: Possible synthesis of HgF4
Papers in Physics
fluorine chemistry at extreme conditions
mercury transition metal behavior
diamond anvil cell
high pressure
infrared spectroscopy
author_facet Michael G. Pravica
Sarah Schyck
Blake Harris
Petrika Cifligu
Eunja Kim
Brant Billinghurst
author_sort Michael G. Pravica
title Fluorine chemistry at extreme conditions: Possible synthesis of HgF4
title_short Fluorine chemistry at extreme conditions: Possible synthesis of HgF4
title_full Fluorine chemistry at extreme conditions: Possible synthesis of HgF4
title_fullStr Fluorine chemistry at extreme conditions: Possible synthesis of HgF4
title_full_unstemmed Fluorine chemistry at extreme conditions: Possible synthesis of HgF4
title_sort fluorine chemistry at extreme conditions: possible synthesis of hgf4
publisher Papers in Physics
series Papers in Physics
issn 1852-4249
1852-4249
publishDate 2019-02-01
description By irradiating a pressurized mixture of a fluorine-bearing compound (XeF2) and HgF2 with synchrotron hard x-rays (>7 keV) inside a diamond anvil cell, we have observed dramatic changes in the far-infrared spectrum within the 30-35 GPa pressure range which suggest that we may have formed HgF4 in the following way: XeF2hv−→Xe+F2 (photochemically) and HgF2+F2→HgF4 (30 GPa < P < 35 GPa). This lends credence to recent theoretical calculations by Botana et al. that suggest that Hg may behave as a transition metal at high pressure in an environment with an excess of molecular fluorine. The spectral changes were observed to be reversible during pressure cycling above and below the above mentioned pressure range until a certain point when we suspect that molecular fluorine diffused out of the sample at lower pressure. Upon pressure release, HgF2 and trace XeF2 were observed to be remaining in the sample chamber suggesting that much of the Xe and F2 diffused and leaked out from the sample chamber.
topic fluorine chemistry at extreme conditions
mercury transition metal behavior
diamond anvil cell
high pressure
infrared spectroscopy
url https://www.papersinphysics.org/papersinphysics/article/view/478/278
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