A CO2 laser heating system for in situ high pressure-temperature experiments at HPCAT

被引:16
|
作者
Smith, Dean [1 ,2 ]
Smith, Jesse S. [3 ]
Childs, Christian [1 ,2 ]
Rod, Eric [3 ]
Hrubiak, Rostislav [3 ]
Shen, Guoyin [3 ]
Salamat, Ashkan [1 ,2 ]
机构
[1] Univ Nevada, Dept Phys & Astron, Las Vegas, NV 89154 USA
[2] Univ Nevada, HiPSEC, Las Vegas, NV 89154 USA
[3] Carnegie Inst Sci, Geophys Lab, High Pressure Collaborat Access Team, Argonne, IL 60439 USA
来源
REVIEW OF SCIENTIFIC INSTRUMENTS | 2018年 / 89卷 / 08期
关键词
DIAMOND-ANVIL CELL; X-RAY-DIFFRACTION; EQUATION-OF-STATE; LOWER MANTLE; EXTREME CONDITIONS; MGSIO3; PEROVSKITE; CORE MATERIALS; SPECTROSCOPY; POLYMORPHS; TRANSITION;
D O I
10.1063/1.5040508
中图分类号
TH7 [仪器、仪表];
学科分类号
0804 ; 080401 ; 081102 ;
摘要
We present a CO2 laser heating setup for synchrotron x-ray diffraction inside a diamond anvil cell, situated at HPCAT (Sector 16, Advanced Photon Source, Argonne National Lab, Illinois, USA), which is modular and portable between the HPCAT experiment hutches. The system allows direct laser heating of wide bandgap insulating materials to thousands of degrees at static high pressures up to the Mbar regime. Alignment of the focused CO2 laser spot is performed using a mid-infrared microscope, which addressed past difficulties with aligning the invisible radiation. The implementation of the mid-infrared microscope alongside a mirror pinhole spatial filter system allows precise alignment of the heating laser spot and optical pyrometry measurement location to the x-ray probe. A comparatively large heating spot (similar to 50 mu m) relative to the x-ray beam (<10 mu m) reduces the risk of temperature gradients across the probed area. Each component of the heating system and its diagnostics have been designed with portability in mind and compatibility with the various experimental hutches at the HPCAT beamlines. We present measurements on ZrO2 at 5.5 GPa which demonstrate the improved room-temperature diffraction data quality afforded by annealing with the CO2 laser. We also present in situ measurements at 5.5 GPa up to 2800 K in which we do not observe the postulated fluorite ZrO2 structure, in agreement with recent findings. Published by AIP Publishing.
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页数:6
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