Related Experiment Video
Updated: Jun 21, 2025

06:04
Simulation of the Planetary Interior Differentiation Processes in the Laboratory
Published on: November 15, 2013
11.5K
Near-infrared focused heating method for the rotational diamond anvil cell
Shintaro Azuma1, Keishi Okazaki2,3, Kentaro Uesugi4
1Department of Earth and Planetary Sciences, Tokyo Institute of Technology, 2-12-1 Ookayama, Meguro, Tokyo 152-8550, Japan.
The Review of Scientific Instruments
|July 11, 2024
Summary
A new near-infrared heating system (IRrDAC) was developed for diamond anvil cell experiments. This system successfully achieved silver melting and antigorite dehydration, proving its capability for deep Earth rheology studies.
Area of Science:
- Geophysics
- Mineral Physics
- High-Pressure Experimental Science
Background:
- Understanding deep Earth rheology requires high-pressure deformation experiments.
- Existing heating systems face limitations in achieving stable, homogeneous temperatures at extreme pressures.
Purpose of the Study:
- To introduce and validate a novel near-infrared focused heating system (IRrDAC) for rotational diamond anvil cell experiments.
- To demonstrate the system's capability in conducting annealing tests relevant to deep Earth conditions.
Main Methods:
- Development of the IRrDAC system for focused near-infrared heating.
- Annealing experiments on silver and antigorite using the IRrDAC system within a rotational diamond anvil cell at SPring-8 (BL47XU).
- Analysis of experimental results to confirm temperature control and material phase changes.
Main Results:
- Successful demonstration of silver melting and antigorite dehydration under high-pressure conditions.
- Confirmation of reproducible temperature-input power relationships, indicating precise thermal control.
- Validation of the IRrDAC system's capability for deformation experiments at lower mantle pressures.
Conclusions:
- The IRrDAC system enables homogeneous and stable high-temperature deformation experiments at lower mantle pressures.
- This technology is expected to significantly advance the study of deep Earth rheology.
- The system's performance was validated through successful annealing tests on silver and antigorite.

