High Pressure Behavior of Mascagnite from Single Crystal Synchrotron X-ray Diffraction Data
High-pressure synchrotron X-ray diffraction was carried out on a single crystal of mascagnite, compressed in a diamond anvil cell. The sample maintained its crystal structure up to ~18 GPa. The volume–pressure data were fitted by a third-order Birch–Murnaghan equation of state (BM3-EOS) yielding K&l...
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doaj-914b233990ff49689f22965936d9b7812021-08-26T13:39:35ZengMDPI AGCrystals2073-43522021-08-011197697610.3390/cryst11080976High Pressure Behavior of Mascagnite from Single Crystal Synchrotron X-ray Diffraction DataPaola Comodi0Maximiliano Fastelli1Giacomo Criniti2Konstantin Glazyrin3Azzurra Zucchini4Dipartimento di Fisica e Geologia, Università Degli Studi di Perugia, 06123 Perugia, ItalyDipartimento di Fisica e Geologia, Università Degli Studi di Perugia, 06123 Perugia, ItalyBayerisches Geoinstitut, University of Bayreuth, 95440 Bayreuth, GermanyDeutsches Elektronen Synchrotron DESY, Notke Street 85, 22607 Hamburg, GermanyDipartimento di Fisica e Geologia, Università Degli Studi di Perugia, 06123 Perugia, ItalyHigh-pressure synchrotron X-ray diffraction was carried out on a single crystal of mascagnite, compressed in a diamond anvil cell. The sample maintained its crystal structure up to ~18 GPa. The volume–pressure data were fitted by a third-order Birch–Murnaghan equation of state (BM3-EOS) yielding K<sub>0</sub> = 20.4(7) GPa, K’<sub>0</sub> = 6.1(2), and V<sub>0</sub> = 499(1) Å<sup>3</sup>, as suggested by the F-f plot. The axial compressibilities, calculated with BM3-EOS, were K<sub>0<i>a</i></sub> = 35(3), K’<sub>0<i>a</i></sub> = 7.7(7), K<sub>0<i>b</i></sub> = 10(3), K’<sub>0<i>b</i></sub> = 7(1), K<sub>0<i>c</i></sub> = 25(1), and K’<sub>0<i>c</i></sub> = 4.3(2) The axial <i>moduli</i> measured using a BM2-EOS and fixing K’<sub>0</sub> equal to 4, were K<sub>0<i>a</i></sub> = 52(2), K<sub>0<i>b</i></sub> = 20 (1), and K<sub>0<i>c</i></sub> = 29.6(4) GPa, and the anisotropic ratio of K<sub>0<i>a</i></sub>:K<sub>0<i>b</i></sub>:K<sub>0<i>c</i></sub> = 1:0.4:0.5. The evolution of crystal lattice and geometrical parameters indicated no phase transition until 17.6 GPa. Sulphate polyhedra were incompressible and the density increase of 30% compared to investigated pressure should be attributed to the reduction of weaker hydrogen bonds. In contrast, some of them, directed along [100], were very short at room temperature, below 2 Å, and showed a very low compressibility. This configuration explains the anisotropic compressional behavior and the lowest compressibility of the <i>a</i> axis.https://www.mdpi.com/2073-4352/11/8/976mascagnitehigh pressurecrystal structureammonium sulphates |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Paola Comodi Maximiliano Fastelli Giacomo Criniti Konstantin Glazyrin Azzurra Zucchini |
spellingShingle |
Paola Comodi Maximiliano Fastelli Giacomo Criniti Konstantin Glazyrin Azzurra Zucchini High Pressure Behavior of Mascagnite from Single Crystal Synchrotron X-ray Diffraction Data Crystals mascagnite high pressure crystal structure ammonium sulphates |
author_facet |
Paola Comodi Maximiliano Fastelli Giacomo Criniti Konstantin Glazyrin Azzurra Zucchini |
author_sort |
Paola Comodi |
title |
High Pressure Behavior of Mascagnite from Single Crystal Synchrotron X-ray Diffraction Data |
title_short |
High Pressure Behavior of Mascagnite from Single Crystal Synchrotron X-ray Diffraction Data |
title_full |
High Pressure Behavior of Mascagnite from Single Crystal Synchrotron X-ray Diffraction Data |
title_fullStr |
High Pressure Behavior of Mascagnite from Single Crystal Synchrotron X-ray Diffraction Data |
title_full_unstemmed |
High Pressure Behavior of Mascagnite from Single Crystal Synchrotron X-ray Diffraction Data |
title_sort |
high pressure behavior of mascagnite from single crystal synchrotron x-ray diffraction data |
publisher |
MDPI AG |
series |
Crystals |
issn |
2073-4352 |
publishDate |
2021-08-01 |
description |
High-pressure synchrotron X-ray diffraction was carried out on a single crystal of mascagnite, compressed in a diamond anvil cell. The sample maintained its crystal structure up to ~18 GPa. The volume–pressure data were fitted by a third-order Birch–Murnaghan equation of state (BM3-EOS) yielding K<sub>0</sub> = 20.4(7) GPa, K’<sub>0</sub> = 6.1(2), and V<sub>0</sub> = 499(1) Å<sup>3</sup>, as suggested by the F-f plot. The axial compressibilities, calculated with BM3-EOS, were K<sub>0<i>a</i></sub> = 35(3), K’<sub>0<i>a</i></sub> = 7.7(7), K<sub>0<i>b</i></sub> = 10(3), K’<sub>0<i>b</i></sub> = 7(1), K<sub>0<i>c</i></sub> = 25(1), and K’<sub>0<i>c</i></sub> = 4.3(2) The axial <i>moduli</i> measured using a BM2-EOS and fixing K’<sub>0</sub> equal to 4, were K<sub>0<i>a</i></sub> = 52(2), K<sub>0<i>b</i></sub> = 20 (1), and K<sub>0<i>c</i></sub> = 29.6(4) GPa, and the anisotropic ratio of K<sub>0<i>a</i></sub>:K<sub>0<i>b</i></sub>:K<sub>0<i>c</i></sub> = 1:0.4:0.5. The evolution of crystal lattice and geometrical parameters indicated no phase transition until 17.6 GPa. Sulphate polyhedra were incompressible and the density increase of 30% compared to investigated pressure should be attributed to the reduction of weaker hydrogen bonds. In contrast, some of them, directed along [100], were very short at room temperature, below 2 Å, and showed a very low compressibility. This configuration explains the anisotropic compressional behavior and the lowest compressibility of the <i>a</i> axis. |
topic |
mascagnite high pressure crystal structure ammonium sulphates |
url |
https://www.mdpi.com/2073-4352/11/8/976 |
work_keys_str_mv |
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