Large volume torsion (LVT) apparatuses for rock deformation at high pressure and temperature

Laboratory studies of rock rheology rely on purpose-built devices that can apply planetarily relevant pressures, temperatures, and non-hydrostatic stresses. Generating these pressures and stresses requires the application of large forces over small specimen areas. However, because rocks are generally polymineralic and deformation microstructures form across many length scales, it is advantageous to study relatively large (millimetric) specimens. In addition, many microstructures continue to evolve with progressive strain, so it is vital that some apparatus are able to generate enough shear strain to study these deformation phenomena. This contribution describes two new rock deformation apparatus-the Large Volume Torsion apparatus-at Washington University in St. Louis, which are capable of deforming geological specimens at high pressure and temperature (P = 3 GPa; T = 1800 K). Deformation is imposed in a torsional geometry, which enables the generation of extremely large shear strains (γ > 100) relevant to Earth's plate boundaries and convecting mantle. A large specimen (diameter up to 4.2 mm) permits detailed postmortem microstructural analysis. Apparatus design, calibration, experimental procedures, and some examples of applications are reviewed.

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Publication Details

Journal
Review of Scientific Instruments
Published
2025-02-01
DOI
https://doi.org/10.1063/5.0221218
Citations
1
Primary Topic
High-pressure geophysics and materials
Type
article
Field-Weighted Citation Impact
1.87

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Large volume torsion (LVT) apparatuses for rock deformation at high pressure and temperature

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1 citations
Review of Scientific Instruments
High-pressure geophysics and materials
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article

Large volume torsion (LVT) apparatuses for rock deformation at high pressure and temperature

Andrew Cross, Joshua A. H. Littleton, H. Couvy, Caroline Bollinger, Philip Skemer
article en
1 citations

Abstract

Laboratory studies of rock rheology rely on purpose-built devices that can apply planetarily relevant pressures, temperatures, and non-hydrostatic stresses. Generating these pressures and stresses requires the application of large forces over small specimen areas. However, because rocks are generally polymineralic and deformation microstructures form across many length scales, it is advantageous to study relatively large (millimetric) specimens. In addition, many microstructures continue to evolve with progressive strain, so it is vital that some apparatus are able to generate enough shear strain to study these deformation phenomena. This contribution describes two new rock deformation apparatus-the Large Volume Torsion apparatus-at Washington University in St. Louis, which are capable of deforming geological specimens at high pressure and temperature (P = 3 GPa; T = 1800 K). Deformation is imposed in a torsional geometry, which enables the generation of extremely large shear strains (γ > 100) relevant to Earth's plate boundaries and convecting mantle. A large specimen (diameter up to 4.2 mm) permits detailed postmortem microstructural analysis. Apparatus design, calibration, experimental procedures, and some examples of applications are reviewed.

Review of Scientific InstrumentsVol. 96(2)
Washington University in St. Louis (US), University of Manchester (GB), Woods Hole Oceanographic Institution (US)
National Science Foundation, Washington University in St. Louis, Directorate for Geosciences
Openalex Percentile: Top 22%
High-pressure geophysics and materials
1.87
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