Graphite resistive heated diamond anvil cell for simultaneous high-pressure and high-temperature diffraction experiments

Author:

Hwang Huijeong12ORCID,Bang Yoonah3ORCID,Choi Jinhyuk3ORCID,Cynn Hyunchae4ORCID,Jenei Zsolt4ORCID,Evans William J.4ORCID,Ehnes Anita1ORCID,Schwark Iris1ORCID,Glazyrin Konstantin1ORCID,Gatta G. Diego5ORCID,Lotti Paolo5ORCID,Sanloup Chrystèle6ORCID,Lee Yongjae3ORCID,Liermann Hanns-Peter1ORCID

Affiliation:

1. Deutsches Elektronen-Synchrotron DESY 1 , Notkestr. 85, 22607 Hamburg, Germany

2. School of Earth Sciences and Environmental Engineering, Gwangju Institute of Science and Technology 2 , 123 Cheomdan-Gwagiro, Gwangju 61005, Republic of Korea

3. Earth System Sciences, Yonsei University 3 , 50 Yonsei-ro, Seodaemun-gu, Seoul 03722, Republic of Korea

4. Lawrence Livermore National Laboratory 4 , 7000 East Avenue, Livermore, California 94550, USA

5. Dipartimento di Scienze della Terra ‘Ardito Desio’, Università degli Studi di Milano 5 , Via Botticelli 23, Milan 20133, Italy

6. Institut de Minéralogie, de Physique des Matériaux et de Cosmochimie (IMPMC), Sorbonne Université, Muséum National d'Histoire Naturelle, UMR CNRS 7590, IRD UR206 6 , 75005 Paris, France

Abstract

High-pressure and high-temperature experiments using a resistively heated diamond anvil cell have the advantage of heating samples homogeneously with precise temperature control. Here, we present the design and performance of a graphite resistive heated diamond anvil cell (GRHDAC) setup for powder and single-crystal x-ray diffraction experiments developed at the Extreme Conditions Beamline (P02.2) at PETRA III, Hamburg, Germany. In the GRHDAC, temperatures up to 2000 K can be generated at high pressures by placing it in a water-cooled vacuum chamber. Temperature estimates from thermocouple measurements are within +/−35 K at the sample position up to 800 K and within +90 K between 800 and 1400 K when using a standard seat combination of cBN and WC. Isothermal compression at high temperatures can be achieved by employing a remote membrane control system. The advantage of the GRHDAC is demonstrated through the study of geophysical processes in the Earth’s crust and upper mantle region.

Funder

Alexander von Humboldt Foundation

Korean Ministry of Science and ICT

U.S. Department of Energy

GIST Research Institute Grant

Deutsches Elektronen Synchrotron (DESY), a member of the Helmholtz Association

Publisher

AIP Publishing

Subject

Instrumentation

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