Book contents
- Static and Dynamic High Pressure Mineral Physics
- Static and Dynamic High Pressure Mineral Physics
- Copyright page
- Contents
- Contributors
- 1 Introduction to Static and Dynamic High-Pressure Mineral Physics
- 2 Development of Static High-Pressure Techniques and the Study of the Earth’s Deep Interior in the Last 50 Years and Its Future
- 3 Applications of Synchrotron and FEL X-Rays in High-Pressure Research
- 4 Development of Large-Volume Diamond Anvil Cell for Neutron Diffraction: The Neutron Diamond Anvil Cell Project at ORNL
- 5 Light-Source Diffraction Studies of Planetary Materials under Dynamic Loading
- 6 New Analysis of Shock-Compression Data for Selected Silicates
- 7 Scaling Relations for Combined Static and Dynamic High-Pressure Experiments
- 8 Equations of State of Selected Solids for High-Pressure Research and Planetary Interior Density Models
- 9 Elasticity at High Pressure with Implication for the Earth’s Inner Core
- 10 Multigrain Crystallography at Megabar Pressures
- 11 Deformation and Plasticity of Materials under Extreme Conditions
- 12 Synthesis of High-Pressure Silicate Polymorphs Using Multi-Anvil Press
- 13 Investigation of Chemical Interaction and Melting Using Laser-Heated Diamond Anvil Cell
- 14 Molecular Compounds under Extreme Conditions
- 15 Superconductivity at High Pressure
- 16 Thermochemistry of High-Pressure Phases
- Index
7 - Scaling Relations for Combined Static and Dynamic High-Pressure Experiments
Published online by Cambridge University Press: 03 August 2023
- Static and Dynamic High Pressure Mineral Physics
- Static and Dynamic High Pressure Mineral Physics
- Copyright page
- Contents
- Contributors
- 1 Introduction to Static and Dynamic High-Pressure Mineral Physics
- 2 Development of Static High-Pressure Techniques and the Study of the Earth’s Deep Interior in the Last 50 Years and Its Future
- 3 Applications of Synchrotron and FEL X-Rays in High-Pressure Research
- 4 Development of Large-Volume Diamond Anvil Cell for Neutron Diffraction: The Neutron Diamond Anvil Cell Project at ORNL
- 5 Light-Source Diffraction Studies of Planetary Materials under Dynamic Loading
- 6 New Analysis of Shock-Compression Data for Selected Silicates
- 7 Scaling Relations for Combined Static and Dynamic High-Pressure Experiments
- 8 Equations of State of Selected Solids for High-Pressure Research and Planetary Interior Density Models
- 9 Elasticity at High Pressure with Implication for the Earth’s Inner Core
- 10 Multigrain Crystallography at Megabar Pressures
- 11 Deformation and Plasticity of Materials under Extreme Conditions
- 12 Synthesis of High-Pressure Silicate Polymorphs Using Multi-Anvil Press
- 13 Investigation of Chemical Interaction and Melting Using Laser-Heated Diamond Anvil Cell
- 14 Molecular Compounds under Extreme Conditions
- 15 Superconductivity at High Pressure
- 16 Thermochemistry of High-Pressure Phases
- Index
Summary
Waste heat – the pressure-volume area between the Rayleigh line and Hugoniot – offers a simple means of quantifying energy dissipation upon dynamic compression, confirming that (i) maximum compression on shock loading corresponds to the conditions at which all the shock energy goes into heating rather than compression; (ii) breaking a single shock into two shocks reduces heating, an effect optimized by the intermediate compression being about half the final compression; and (iii) static precompression further reduces heating upon shock loading to a given final compression. Combined static-dynamic experiments can thus maximize material compression by tuning dissipation.
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- Static and Dynamic High Pressure Mineral Physics , pp. 135 - 146Publisher: Cambridge University PressPrint publication year: 2022