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Yang L, Li J, Zhang D, Liu Y, Hu Q. Deviatoric stress-induced metallization, layer reconstruction and collapse of van der Waals bonded zirconium disulfide. Commun Chem 2024; 7:141. [PMID: 38909153 PMCID: PMC11193816 DOI: 10.1038/s42004-024-01223-1] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 11/10/2023] [Accepted: 06/12/2024] [Indexed: 06/24/2024] Open
Abstract
In contrast to two-dimensional (2D) monolayer materials, van der Waals layered transition metal dichalcogenides exhibit rich polymorphism, making them promising candidates for novel superconductor, topological insulators and electrochemical catalysts. Here, we highlight the role of hydrostatic pressure on the evolution of electronic and crystal structures of layered ZrS2. Under deviatoric stress, our electrical experiments demonstrate a semiconductor-to-metal transition above 30.2 GPa, while quasi-hydrostatic compression postponed the metallization to 38.9 GPa. Both X-ray diffraction and Raman results reveal structural phase transitions different from those under hydrostatic pressure. Under deviatoric stress, ZrS2 rearranges the original ZrS6 octahedra into ZrS8 cuboids at 5.5 GPa, in which the unique cuboids coordination of Zr atoms is thermodynamically metastable. The structure collapses to a partially disordered phase at 17.4 GPa. These complex phase transitions present the importance of deviatoric stress on the highly tunable electronic properties of ZrS2 with possible implications for optoelectronic devices.
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Affiliation(s)
- Linfei Yang
- Center for High Pressure Science and Technology Advanced Research, 100193, Beijing, China
- School of Materials Science and Engineering, Jingdezhen Ceramic University, Jingdezhen, 333403, Jiangxi, China
| | - Junwei Li
- Center for High Pressure Science and Technology Advanced Research, 100193, Beijing, China
| | - Dongzhou Zhang
- Hawai'i Institute of Geophysics and Planetology, School of Ocean and Earth Science and Technology, University of Hawai'i at Manoa, Honolulu, HI, 96822, USA
| | - Yuegao Liu
- CAS Key Laboratory for Experimental Study under Deep-sea Extreme Conditions, Institute of Deep-sea Science and Engineering, Chinese Academy of Sciences, Sanya, 572000, China
| | - Qingyang Hu
- Center for High Pressure Science and Technology Advanced Research, 100193, Beijing, China.
- Shanghai Advanced Research in Physical Sciences (SHARPS), Shanghai, 201203, China.
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Glazyrin K, Aslandukov A, Aslandukova A, Fedotenko T, Khandarkhaeva S, Laniel D, Bykov M, Dubrovinsky L. High-pressure reactions between the pnictogens: the rediscovery of BiN. Front Chem 2023; 11:1257942. [PMID: 37901158 PMCID: PMC10602720 DOI: 10.3389/fchem.2023.1257942] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 07/13/2023] [Accepted: 09/22/2023] [Indexed: 10/31/2023] Open
Abstract
We explore chemical reactions within pnictogens with an example of bismuth and nitrogen under extreme conditions. Understanding chemical reactions between Bi and N, elements representing the first and the last stable elements of the nitrogen group, and the physical properties of their compounds under ambient and high pressure is far from being complete. Here, we report the high-pressure high-temperature synthesis of orthorhombic Pbcn BiN (S.G. #60) from Bi and N2 precursors at pressures above 40 GPa. Using synchrotron single-crystal X-ray diffraction on the polycrystalline sample, we solved and refined the compound's structure and studied its behavior and compressibility on decompression to ambient pressure. We confirm the stability of Pbcn BiN to pressures as low as 12.5(4) GPa. Below that pressure value, a group-subgroup phase transformation occurs, resulting in the formation of a non-centrosymmetric BiN solid with a space group Pca21 (S.G. #29). We use ab initio calculations to characterize the polymorphs of BiN. They also provide support and explanation for our experimental observations, in particular those corresponding to peculiar Bi-N bond evolution under pressure, resulting in a change in the coordination numbers of Bi and N as a function of pressure within the explored stability field of Pbcn BiN.
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Affiliation(s)
- K. Glazyrin
- Deutsches Elektronen-Synchrotron DESY, Hamburg, Germany
| | - A. Aslandukov
- Material Physics and Technology at Extreme Conditions, Laboratory of Crystallography, University of Bayreuth, Bayreuth, Germany
- Bayerisches Geoinstitut, University of Bayreuth, Bayreuth, Germany
| | - A. Aslandukova
- Bayerisches Geoinstitut, University of Bayreuth, Bayreuth, Germany
| | - T. Fedotenko
- Deutsches Elektronen-Synchrotron DESY, Hamburg, Germany
| | - S. Khandarkhaeva
- Bayerisches Geoinstitut, University of Bayreuth, Bayreuth, Germany
| | - D. Laniel
- Centre for Science at Extreme Conditions, School of Physics and Astronomy, University of Edinburgh, Edinburgh, United Kingdom
| | - M. Bykov
- Institute of Inorganic Chemistry, University of Cologne, Cologne, Germany
| | - L. Dubrovinsky
- Bayerisches Geoinstitut, University of Bayreuth, Bayreuth, Germany
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High-pressure synthesis of seven lanthanum hydrides with a significant variability of hydrogen content. Nat Commun 2022; 13:6987. [DOI: 10.1038/s41467-022-34755-y] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 08/12/2022] [Accepted: 11/04/2022] [Indexed: 11/18/2022] Open
Abstract
AbstractThe lanthanum-hydrogen system has attracted significant attention following the report of superconductivity in LaH10 at near-ambient temperatures and high pressures. Phases other than LaH10 are suspected to be synthesized based on both powder X-ray diffraction and resistivity data, although they have not yet been identified. Here, we present the results of our single-crystal X-ray diffraction studies on this system, supported by density functional theory calculations, which reveal an unexpected chemical and structural diversity of lanthanum hydrides synthesized in the range of 50 to 180 GPa. Seven lanthanum hydrides were produced, LaH3, LaH~4, LaH4+δ, La4H23, LaH6+δ, LaH9+δ, and LaH10+δ, and the atomic coordinates of lanthanum in their structures determined. The regularities in rare-earth element hydrides unveiled here provide clues to guide the search for other synthesizable hydrides and candidate high-temperature superconductors. The hydrogen content variability in lanthanum hydrides and the samples’ phase heterogeneity underline the challenges related to assessing potentially superconducting phases and the nature of electronic transitions in high-pressure hydrides.
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Myint PC, Shi EL, Hamel S, Cynn H, Jenei Z, Lipp MJ, Evans WJ, Akin MC. Two-phase equation of state for lithium fluoride. J Chem Phys 2019; 150:074506. [PMID: 30795652 DOI: 10.1063/1.5079758] [Citation(s) in RCA: 9] [Impact Index Per Article: 1.8] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 01/25/2023] Open
Abstract
We present an equation of state for the solid and liquid phases of lithium fluoride that covers a wide range of conditions from ambient pressure and temperature to the high pressures and temperatures exhibited in shock- and ramp-compression studies. The particular solid phase we have focused on in this work is the B1 phase. We have followed an approach where the pressure and heat-capacity functions of both phases are fit to experimental data and our own quantum molecular dynamics simulations and are then integrated in a thermodynamically consistent way to obtain the corresponding free-energy functions. This approach yields a two-phase equation of state that provides better overall agreement with experimental data than other equations of state for lithium fluoride, such as SESAME 7271v3, LEOS 2240, and the model presented by Smirnov. The last of these is a three-phase equation of state that predicts a B1-B2 transition along the shock Hugoniot at a pressure of about 140 GPa. This solid-solid transition has been a topic of speculation and debate in the literature for over 50 years, culminating in the work of Smirnov, who has developed the only potentially viable equation of state that allows for this transition. We explain why the proposed B1-B2 transition at 140 GPa is not consistent with recent velocimetry data.
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Affiliation(s)
- Philip C Myint
- Lawrence Livermore National Laboratory, Livermore, California 94550, USA
| | - Eric L Shi
- Lawrence Livermore National Laboratory, Livermore, California 94550, USA
| | - Sebastien Hamel
- Lawrence Livermore National Laboratory, Livermore, California 94550, USA
| | - Hyunchae Cynn
- Lawrence Livermore National Laboratory, Livermore, California 94550, USA
| | - Zsolt Jenei
- Lawrence Livermore National Laboratory, Livermore, California 94550, USA
| | - Magnus J Lipp
- Lawrence Livermore National Laboratory, Livermore, California 94550, USA
| | - William J Evans
- Lawrence Livermore National Laboratory, Livermore, California 94550, USA
| | - Minta C Akin
- Lawrence Livermore National Laboratory, Livermore, California 94550, USA
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Du Z, Gu T, Dobrosavljevic V, Weir ST, Falabella S, Lee KKM. Using stepped anvils to make even insulation layers in laser-heated diamond-anvil cell samples. THE REVIEW OF SCIENTIFIC INSTRUMENTS 2015; 86:095103. [PMID: 26429476 DOI: 10.1063/1.4929667] [Citation(s) in RCA: 2] [Impact Index Per Article: 0.2] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/05/2023]
Abstract
We describe a method to make even insulation layers for high-pressure laser-heated diamond-anvil cell samples using stepped anvils. The method works for both single-sided and double-sided laser heating using solid or fluid insulation. The stepped anvils are used as matched pairs or paired with a flat culet anvil to make gasket insulation layers and not actually used at high pressures; thus, their longevity is ensured. We compare the radial temperature gradients and Soret diffusion of iron between self-insulating samples and samples produced with stepped anvils and find that less pronounced Soret diffusion occurs in samples with even insulation layers produced by stepped anvils.
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Affiliation(s)
- Zhixue Du
- Department of Geology and Geophysics, Yale University, New Haven, Connecticut 06520, USA
| | - Tingting Gu
- Department of Geology and Geophysics, Yale University, New Haven, Connecticut 06520, USA
| | | | - Samuel T Weir
- Lawrence Livermore National Laboratory, Livermore, California 94550, USA
| | - Steve Falabella
- Lawrence Livermore National Laboratory, Livermore, California 94550, USA
| | - Kanani K M Lee
- Department of Geology and Geophysics, Yale University, New Haven, Connecticut 06520, USA
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Zhao J, Ross NL. Non-hydrostatic behavior of KBr as a pressure medium in diamond anvil cells up to 5.63 GPa. JOURNAL OF PHYSICS. CONDENSED MATTER : AN INSTITUTE OF PHYSICS JOURNAL 2015; 27:185402. [PMID: 25880344 DOI: 10.1088/0953-8984/27/18/185402] [Citation(s) in RCA: 3] [Impact Index Per Article: 0.3] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/04/2023]
Abstract
Non-hydrostatic stresses of KBr acting as a pressure-transmitting medium have been investigated by examining their effect on a single crystal of quartz in a diamond anvil cell (DAC). The lattice strains or distortions were measured by single-crystal x-ray diffraction methods, and the non-hydrostatic deviatoric stresses for KBr were determined up to 5.63(2) GPa. The experimental results show that differences between axial stress components in the direction normal to the DAC culet face and the radial stress components in directions parallel to the DAC culet face are about 0.063(24) GPa at pressures below 2.14 GPa, and the pressure-transmitting medium can therefore be considered as quasi-hydrostatic up to this pressure. However above 2.14 GPa, after the phase transition pressure of KBr during which it converts from the B1 phase to the B2 phase, the deviatoric stresses constantly increase with increasing pressure. At the maximum pressure of this study, 5.63(2) GPa, the difference between axial stress and radial stress components reaches 0.93(9) GPa. Different variations in the non-hydrostatic deviatoric stresses were observed during both compression and decompression of the DAC, and are mainly ascribed to the phase-transition-induced volume change of KBr.
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Affiliation(s)
- Jing Zhao
- Virginia Tech Crystallography Laboratory, Department of Geosciences, Virginia Polytechnic Institute and State University, Blacksburg, VA 24061, USA
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