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High Pressure Single Crystal Diffraction at PX^2
Published on: January 16, 2017
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Direct tomography imaging for inelastic X-ray scattering experiments at high pressure
Ch J Sahle1, A D Rosa1, M Rossi1
1European Synchrotron Radiation Facility, 71 Avenue des Martyrs, 38000 Grenoble, France.
Journal of Synchrotron Radiation
|December 24, 2016
Summary
This study introduces a new method to isolate sample signals from diamond anvil cell (DAC) interference in X-ray scattering experiments. This technique enables clearer high-pressure measurements and reveals a phase transition in quartz.
Area of Science:
- Materials Science
- Condensed Matter Physics
- Spectroscopy
Background:
- High-pressure experiments using diamond anvil cells (DACs) often suffer from interfering signals from the cell components.
- Parasitic scattering from diamonds, gaskets, and pressure media can obscure sample signals, hindering analysis.
- Absorption edge overlaps between sample and DAC materials complicate inelastic X-ray measurements like X-ray Raman scattering spectroscopy.
Purpose of the Study:
- To develop a method for separating non-resonant inelastic X-ray scattering signals from the sample and the high-pressure sample environment.
- To overcome limitations imposed by parasitic signals in high-pressure X-ray scattering experiments.
- To demonstrate the technique's effectiveness for analyzing compressed materials.
Main Methods:
- Utilizing spatially resolved detection of scattered X-rays to distinguish sample signals from diamond anvil cell (DAC) contributions.
- Employing simple machine learning algorithms to identify detector pixels corresponding to the sample signal.
- Acquiring high-quality X-ray Raman scattering spectra of compressed α-quartz.
Main Results:
- Successfully separated sample signals from spurious scattering originating from the DAC without restricting detection angles.
- Achieved unprecedented spectral quality for the Si L2,3-edge and O K-edge of compressed α-quartz.
- Observed clear evidence of a pressure-induced phase transition in α-quartz between 10 and 24 GPa.
Conclusions:
- The developed spatially resolved X-ray scattering technique effectively isolates sample signals in high-pressure DAC experiments.
- Machine learning aids in processing the spatially resolved data, simplifying analysis.
- The method provides high-quality spectra, enabling the detection of pressure-induced phase transitions in materials like α-quartz.
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