Asymmetrical friction in a piston-cylinder device and the effect on the melting curves of indium and bismuth
- 1 July 1980
- journal article
- research article
- Published by AIP Publishing in Review of Scientific Instruments
- Vol. 51 (7) , 959-964
- https://doi.org/10.1063/1.1136354
Abstract
The melting curves of indium and bismuth were determined in a piston‐cylinder device. A comparison of the results obtained by differential thermal analysis and volumetric techniques confirms the existence of an asymmetric friction component. Transition pressures are overestimated if allowance is not made for asymmetric friction. The application of Mirwald’s ’’zero friction’’ technique for talc and NaCl assemblies indicated that only symmetrical and not asymmetrical friction is eliminated.Keywords
This publication has 14 references indexed in Scilit:
- Study of the piston-rotation technique for piston-cylinder devicesReview of Scientific Instruments, 1978
- Low-friction cell for piston-cylinder high-pressure apparatusJournal of Geophysical Research, 1975
- High-Pressure Calibration: A Critical ReviewJournal of Physical and Chemical Reference Data, 1972
- Strength of solid pressure media and implications for high pressure apparatusContributions to Mineralogy and Petrology, 1971
- Investigation of phase transformations at elevated temperatures and pressures by differential thermal analysis in piston-cylinder apparatusJournal of Physics and Chemistry of Solids, 1966
- Melting curves of the potassium halides at high pressuresJournal of Physics and Chemistry of Solids, 1965
- Phase Diagrams of Arsenic, Antimony, and Bismuth at Pressures up to 70 kbarsPhysical Review B, 1963
- Fusion curves and polymorphic transitions of the group III elements—Aluminum, gallium, indium and thallium—At high pressuresJournal of Physics and Chemistry of Solids, 1963
- Experimental Fusion Curves of Indium and Tin to 105 000 AtmospheresPhysical Review B, 1960
- Apparatus for phase-equilibrium measurements at pressures up to 50 kilobars and temperatures up to 1750°CJournal of Geophysical Research, 1960