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The electrical conductivity of aqueous fluids is critical for interpreting the electrical anomalies observed by magnetotellurics in the Earth's crust. Conductivity measurements of fluids at high temperature and pressure were mainly conducted in cold-sealed pressure vessels, hydrothermal diamond anvil cells, and piston-cylinder apparatus, by using precious metals, such as Pt-Rh or Au-Pd as sample capsules. However, this research has never been performed in a multi-anvil apparatus. In addition, metal capsules employed in previous studies were costly and difficult to manufacture mechanically in the laboratory. In this study, we designed a novel, economical, chemical inertness, and tractable sample capsule made of polytetrafluoroethylene (PTFE), and by using this capsule, we successfully measured the conductivity of NaCl solutions in a multi-anvil apparatus under conditions of 323-598 K and 0.5-1.0 GPa. Our results are consistent with those from diamond anvil cells and piston-cylinder apparatus. Besides being used in conductivity measurement, the new and low-cost method has potential applications for investigating other physicochemical properties, such as rock-water interactions and fluid sound velocity under shallow crustal conditions. Furthermore, higher temperature and pressure can be realized by replacing the PTFE components with metallic materials, enabling more extensive exploration of fluid behavior in the Earth's deep interior.
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http://dx.doi.org/10.1063/5.0231628 | DOI Listing |
Proc Natl Acad Sci U S A
June 2025
Center for High Pressure Science and Technology Advanced Research (Shanghai), Shanghai 201203, China.
Seismic low-velocity layers (LVLs), frequently attributed to hydrous-silicate melts, are detected globally but exhibit lateral discontinuities. Geophysical and laboratory studies of water content in the mantle transition zone (MTZ) and upper mantle solubility limits suggest these layers likely form through global dehydration melting near the 410 km discontinuity (D410). A key hypothesis posits that melts form globally but are preserved only where melt stability permits retention.
View Article and Find Full Text PDFRev Sci Instrum
May 2025
Key Laboratory of High-Temperature and High-Pressure Study of the Earth's Interior, Institute of Geochemistry, Chinese Academy of Sciences, Guizhou 550081, China.
The electrical conductivity of aqueous fluids is critical for interpreting the electrical anomalies observed by magnetotellurics in the Earth's crust. Conductivity measurements of fluids at high temperature and pressure were mainly conducted in cold-sealed pressure vessels, hydrothermal diamond anvil cells, and piston-cylinder apparatus, by using precious metals, such as Pt-Rh or Au-Pd as sample capsules. However, this research has never been performed in a multi-anvil apparatus.
View Article and Find Full Text PDFRev Sci Instrum
July 2024
HPCAT, X-ray Science Division, Argonne National Laboratory, Lemont, Illinois 60439, USA.
The diamond anvil cell (DAC) has been widely used in high-pressure research. Despite significant progress over the past five decades, the opposed anvil geometry in the DAC inevitably leads to a disk-shaped sample configuration at high pressure. This intrinsic limitation is largely responsible for the large pressure and temperature gradients in the DAC, which often compromise precise experiments and their characterizations.
View Article and Find Full Text PDFChemphyschem
May 2024
Bayerisches Geoinstitut, University of Bayreuth, Universitätsstraße 30, 95447, Bayreuth, German.
We have performed in situ X-ray diffraction measurements of cubic silicon carbide (SiC) with a zinc-blende crystal structure (B3) at high pressures and temperatures using multi-anvil apparatus. The ambient volume inferred from the compression curves is smaller than that of the starting material. Using the 3-order Birch-Murnaghan equation of state and the Mie-Grüneisen-Debye model, we have determined the thermoelastic parameters of the B3-SiC to be K=228±3 GPa, K',=4.
View Article and Find Full Text PDFInorg Chem
March 2023
CNR - IMEM, 43124 Parma, Italy.
We present a new method to synthesize bulk indium nitride by means of a simple solid-state chemical reaction carried out under hydrostatic high-pressure/high-temperature conditions in a multi-anvil apparatus, not involving gases or solvents during the process. The reaction occurs between the binary oxide InO and the highly reactive LiN as the nitrogen source, in the powder form. The formation of the hexagonal phase of InN, occurring at 350 °C and ≥ 3 GPa, was successfully confirmed by powder X-ray diffraction, with the presence of LiO as a unique byproduct.
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