24-28 Sep 2017 Saint Malo (France)
Yield strength of rocksalt structures at high-pressure using Raman piezometry
Bruno Reynard  1, *@  , Razvan Caracas  1@  , Hervé Cardon  1@  , Gilles Montagnac  2@  , Sébastien Merkel  3, 4@  
1 : Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement [Lyon]  (LGL-TPE)
École Normale Supérieure - Lyon, Université Claude Bernard Lyon 1, Institut national des sciences de l\'Univers, Centre National de la Recherche Scientifique : UMR5276, Institut national des sciences de l\'Univers, Institut national des sciences de l\'Univers
69364 Lyon cedex 07 -  France
2 : Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement  (LGL-TPE)  -  Website
CNRS : UMR5276, INSU, Université Claude Bernard - Lyon I, Ecole Normale Supérieure de Lyon
3 : Unité Matériaux et Transformations  (UMET)
CNRS : UMR8207, Université de Lille
Villeneuve d'Ascq -  France
4 : Institut Universitaire de France  (IUF)  -  Website
Ministère de l'Enseignement Supérieur et de la Recherche Scientifique
Maison des Universités, 103 Boulevard Saint-Michel, 75005 Paris -  France
* : Corresponding author

Measuring yield strengths of condensed materials under non-hydrostatic compression provides essential constrains on their behavior under extreme mechanical efforts ranging from those encountered in planetary interiors to those in boundary lubrication. Raman frequencies of quartz are used to evaluate deviatoric stresses in rocksalt-structure media in diamond-anvil cell experiments to pressures up to 20 GPa. The piezospectroscopic effect in quartz is modeled by first-principles calculations. Non-hydrostatic stresses measured in halogen salts give yield strength estimates in the B1 (NaCl), and B2 structure (KCl and KBr). Raman measurements in MgO show that yield strength is consistent with former radial X-ray diffraction measurements. Radial pressure and deviatoric stress distribution in the DAC is mapped and used to discuss applicability of former determinations of yield strength.


Online user: 1 RSS Feed