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Abstract
The melting curve of Sn initially rises steeply as a function of pressure but exhibits a decrease in slope (dTm/dP)
above 40 GPa to become nearly flat above 50 GPa. Previous studies have
argued that a body-centered tetragonal (bct) to cubic (bcc) phase
transition occurs in this range at room temperature. However, our
investigations have shown that the phase behavior is more complex in
this region with orthorhombic (bco) splitting of reflections occurring
in the x-ray diffraction pattern above 32 GPa and coexisting diffraction
signatures of bco and bcc structures are observed between 40 and 70
GPa. Here we have documented the simultaneous presence of bco and bcc
reflections up to the melting point, negating the possibility that their
coexistence might indicate a kinetically hindered first-order phase
transformation. In this paper we have extended the observation of Sn
melting relations into the megabar (P>100
GPa) range using the appearance of liquid diffuse scattering in x-ray
diffraction patterns and discontinuities during thermal signal
processing to diagnose the occurrence of melting. Both techniques yield
consistent results that indicate the melting line maintains the same low
slope up to the highest pressure examined and does not flatten. The
results below approximately 40 GPa agree well with the melting relations
produced recently using a multiphase equation of state fitted to
available or assumed data. Above this pressure the experimental melting
points lie increasingly below the predicted crystal-liquid phase
boundary, but above the flat melting from past studies, indicating that
the thermodynamic properties of the body-centered “γ”-Sn structure remain to be clarified.
Original language | English |
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Article number | 054102 |
Number of pages | 8 |
Journal | Physical Review B |
Volume | 95 |
Issue number | 5 |
DOIs | |
Publication status | Published - 3 Feb 2017 |
Research Groups and Themes
- PetrologyGroup
- PetrologyLabs
Fingerprint
Dive into the research topics of 'High-pressure melting behavior of tin up to 105 GPa'. Together they form a unique fingerprint.Projects
- 2 Finished
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Diffusion in the DAC: Probing the physical state of the Earth's inner core
Lord, O. T. (Principal Investigator)
30/09/13 → 30/09/16
Project: Research
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Profiles
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Dr Oliver T Lord
- School of Earth Sciences - Royal Society University Research Fellow and Proleptic Senior Lecturer
- Geophysics
- Petrology (formerly BEEST)
Person: Academic , Member