High-pressure behavior of the crystal structure of the fullerene molecular complex with ferrocene C60·{Fe(C5H5)2}2

2019 ◽  
Vol 28 (4) ◽  
pp. 295-298
Author(s):  
A. V. Kuzmin ◽  
S. S. Khasanov ◽  
K. P. Meletov ◽  
D. V. Konarev
2004 ◽  
Vol 89 (1) ◽  
pp. 189-196 ◽  
Author(s):  
Fabrizio Nestola ◽  
Mario Tribaudino ◽  
Tiziana Boffa Ballaran

2014 ◽  
Vol 70 (a1) ◽  
pp. C49-C49
Author(s):  
Elena Bykova ◽  
Maxim Bykov ◽  
Vitali Prakapenka ◽  
Zuzana Konôpková ◽  
Hanns-Peter Liermann ◽  
...  

High pressure behavior of Fe2O3has been a long-standing subject of research due to its high importance for understanding Earth's interiors. At pressures from 40 to 60 GPa it undergoes a series of transformations, such as structural changes with a large volume discontinuity (~10 %), a drop of the resistivity, a spin crossover of Fe3+, and a disappearance of the ordered magnetic state. The crystal structure of the phase(s) observed on compression at ambient temperature above 50 GPa is still under question since only powder X-ray diffraction (XRD) data were available so far. Mössbauer and Raman spectroscopy studies cannot provide definitive structural information. Applying laser heating to Fe2O3, compressed up to 70 GPa and above, results in a distinct reconstructive phase transition to the CaIrO3-type structure, according to powder XRD. Poverty of the available structural data encouraged us to perform a series of high-pressure and high-temperature XRD experiments on single crystals of Fe2O3in diamond anvil cells. We have studied the behavior of Fe2O3at pressures up to 100 GPa and temperatures up to 2500 K. Here we report crystal structures of two novel high-pressure Fe2O3polymorphs, as well as the relations between a spin state of iron atoms and the crystal chemistry of the iron compound. In our compression experiments initially hematite-structured Fe2O3transformed to a new phase at ~54 GPa with 10 % of the volume reduction. This phase has a triclinic distorted perovskite-type structure. The second reconstructive transition occurred at 66–70 GPa with 3 % of the volume discontinuity and resulted in formation of an orthorhombic phase. Laser heating to ~21001100 K at pressures above 70 GPa promoted a transition to a Cmcm CaIrO3-type phase, whose crystal structure was refined by means of single crystal XRD to R1~ 9.7 %. Decompression experiments showed that the Cmcm phase transforms back to hematite at pressures between ~25 and 15 GPa.


CrystEngComm ◽  
2011 ◽  
Vol 13 (1) ◽  
pp. 99-102 ◽  
Author(s):  
Hiroshi Fujihisa ◽  
Kazumasa Honda ◽  
Shigeaki Obata ◽  
Hiroshi Yamawaki ◽  
Satoshi Takeya ◽  
...  

CrystEngComm ◽  
2013 ◽  
Vol 15 (1) ◽  
pp. 192-198 ◽  
Author(s):  
Mariana Derzsi ◽  
Armand Budzianowski ◽  
Viktor V. Struzhkin ◽  
Przemysław J. Malinowski ◽  
Piotr J. Leszczyński ◽  
...  

Author(s):  
H. Sowa

AbstractSingle-crystal structure refinements of the low-temperature quartz modification of GaPOThe refinements were carried out in space groupThe high pressure behavior of GaPOAs in the case of other quartz-type structures, the high-pressure behavior of GaPO


2020 ◽  
Author(s):  
Keishiro Yamashita ◽  
Kazuki Komatsu ◽  
Hiroyuki Kagi

An crystal-growth technique for single crystal x-ray structure analysis of high-pressure forms of hydrogen-bonded crystals is proposed. We used alcohol mixture (methanol: ethanol = 4:1 in volumetric ratio), which is a widely used pressure transmitting medium, inhibiting the nucleation and growth of unwanted crystals. In this paper, two kinds of single crystals which have not been obtained using a conventional experimental technique were obtained using this technique: ice VI at 1.99 GPa and MgCl<sub>2</sub>·7H<sub>2</sub>O at 2.50 GPa at room temperature. Here we first report the crystal structure of MgCl2·7H2O. This technique simultaneously meets the requirement of hydrostaticity for high-pressure experiments and has feasibility for further in-situ measurements.


2019 ◽  
Vol 74 (4) ◽  
pp. 357-363
Author(s):  
Daniela Vitzthum ◽  
Hubert Huppertz

AbstractThe mixed cation triel borate Ga4In4B15O33(OH)3 was synthesized in a Walker-type multianvil apparatus at high-pressure/high-temperature conditions of 12.5 GPa and 1300°C. Although the product could not be reproduced in further experiments, its crystal structure could be reliably determined via single-crystal X-ray diffraction data. Ga4In4B15O33(OH)3 crystallizes in the tetragonal space group I41/a (origin choice 2) with the lattice parameters a = 11.382(2), c = 15.244(2) Å, and V = 1974.9(4) Å3. The structure of the quaternary triel borate consists of a complex network of BO4 tetrahedra, edge-sharing InO6 octahedra in dinuclear units, and very dense edge-sharing GaO6 octahedra in tetranuclear units.


RSC Advances ◽  
2019 ◽  
Vol 9 (7) ◽  
pp. 3577-3581 ◽  
Author(s):  
Nursultan Sagatov ◽  
Pavel N. Gavryushkin ◽  
Talgat M. Inerbaev ◽  
Konstantin D. Litasov

We carried out ab initio calculations on the crystal structure prediction and determination of P–T diagrams within the quasi-harmonic approximation for Fe7N3 and Fe7C3.


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