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Synchrotron-based high-pressure research in materials science

Published online by Cambridge University Press:  08 June 2016

Bin Chen
Affiliation:
Center for High Pressure Science & Technology Advanced Research, China; and Advanced Light Source, Lawrence Berkeley National Laboratory, USA; chenbin@hpstar.ac.cn and bchen@lbl.gov
Jung-Fu Lin
Affiliation:
Center for High Pressure Science & Technology Advanced Research, China; and Department of Geological Sciences, The University of Texas at Austin, USA; linjf@hpstar.ac.cn
Jiuhua Chen
Affiliation:
Mechanical and Materials Engineering Department, Florida International University, USA; and Center for High Pressure Science & Technology Advanced Research, China; chenjh@hpstar.ac.cn
Hengzhong Zhang
Affiliation:
Center for High Pressure Science & Technology Advanced Research, China; hengzhong.zhang@hpstar.ac.cn
Qiaoshi Zeng
Affiliation:
Center for High Pressure Science & Technology Advanced Research, China; zengqs@hpstar.ac.cn

Abstract

The integration of synchrotron and high-pressure techniques has significantly advanced research in materials science, giving rise to many important discoveries in physics, chemistry, environmental science, and many other fields of physical and engineering sciences. The relevant frontier work in multiple disciplines is reviewed. The selected studies include high-pressure superconductivity, lattice dynamics of materials, plastic deformation of nanomaterials, polyamorphic transitions and devitrification in metallic glass, rheology of minerals, and high-pressure chemistry probing.

Information

Type
Research Article
Copyright
Copyright © Materials Research Society 2016 
Figure 0

Figure 1. Pressure scale in the universe and pressure generation capabilities of lab devices.1

Figure 1

Figure 2. Integration of synchrotron techniques with pressurizing, heating, cooling, and electrical/magnetic transport probing techniques. Courtesy of Ho-Kwang Mao. Note: DAC, diamond anvil cell.

Figure 2

Figure 3. Magnetic and structural transition diagram of BaFe2As2 (solid lines) and SrFe2As2 (dashed lines) pnictides at high-pressure low-temperature. TS: tetragonal-orthorhombic transition temperature based on x-ray diffraction results; TN: paramagnetic-antiferromagnetic transition temperature based on Mössbauer results.27,28 Note: Tc, superconducting critical temperature.

Figure 3

Figure 4. Sketch of principles of three synchrotron-based creep experiments. (a) Deformation-diamond synthesis (D-DIA): The confining pressure is achieved by advancing the six anvils in a DIA module simultaneously toward the cubic pressure medium with a cylindrical sample orientated vertically. Metallic foils are placed at each end of the sample as strain markers. Deforming forces, delivered by two differential rams, apply additional stress to the sample through the top and bottom anvils (black arrows) to induce creep at the confining pressure. (b) Rotational Drickamer apparatus: The confining pressure is achieved by advancing the opposed anvils toward a disc pressure medium with a ring-shape sample embedded inside. A metallic foil pressure marker is placed in the sample (orange) as shown. (c) Deformation-Tcup: The confining pressure is achieved by advancing the eight second-stage cubes in a Kawai-type module toward the octahedral pressure medium with a cylindrical sample orientated vertically. Metallic foils are placed at each end of the sample as strain markers. Deforming forces are delivered by two differential rams applying additional stress to the sample through the top and bottom cubes to induce creep at the confining pressure.

Figure 4

Figure 5. Change in chemical bonding in graphite under compression. (a) X-ray diffraction peaks broaden due to distortion of graphite basal planes under pressure. (b) Inelastic x-ray scattering (IXS) spectra showing one-half of the interplane carbon π bonds changed to σ bonds. Adapted with permission from Reference 7.© AAAS 2003. Note: a, lattice parameter; c, lattice parameter; θ, scattering angle; A, stacking layer; B, stacking layer; black sphere, layer-bridging carbon; gray sphere, nonbridging carbon; horizontal, IXS taken in the horizontal direction to probe carbon bonding in the a-plane; vertical, IXS taken in the vertical direction to probe carbon bonding in the c-plane.