| People | Locations | Statistics |
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| Naji, M. |
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| Motta, Antonella |
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| Aletan, Dirar |
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| Mohamed, Tarek |
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| Ertürk, Emre |
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| Taccardi, Nicola |
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| Kononenko, Denys |
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| Petrov, R. H. | Madrid |
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| Alshaaer, Mazen | Brussels |
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| Bih, L. |
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| Casati, R. |
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| Muller, Hermance |
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| Kočí, Jan | Prague |
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| Šuljagić, Marija |
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| Kalteremidou, Kalliopi-Artemi | Brussels |
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| Azam, Siraj |
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| Ospanova, Alyiya |
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| Blanpain, Bart |
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| Ali, M. A. |
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| Popa, V. |
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| Rančić, M. |
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| Ollier, Nadège |
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| Azevedo, Nuno Monteiro |
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| Landes, Michael |
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| Rignanese, Gian-Marco |
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Lotti, Paolo
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Publications (8/8 displayed)
- 2024Crystallographic mechanism of the elastic behaviour of synthetic bütschliite K2Ca(CO3)2 on compression to 20 GPa
- 2023Graphite resistive heated diamond anvil cell for simultaneous high-pressure and high-temperature diffraction experimentscitations
- 2023Graphite resistive heated diamond anvil cell for simultaneous high-pressure and high-temperature diffraction experimentscitations
- 2023Graphite resistive heated diamond anvil cell for simultaneous high-pressure and high-temperature diffraction experimentscitations
- 2022High-pressure behavior and crystal-fluid interaction in natural erionite-Kcitations
- 2019A multi-methodological study of kurnakovite: A potential B-rich aggregatecitations
- 2019Thermal stability and high-temperature behavior of the natural borate colemanite: An aggregate in radiation-shielding concretescitations
- 2017Unraveling the Peculiarities in the Temperature-Dependent Structural Evolution of Black Phosphoruscitations
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article
Graphite resistive heated diamond anvil cell for simultaneous high-pressure and high-temperature diffraction experiments
Abstract
<jats:p>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.</jats:p>