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Abstract
The phase diagram of NiSi has been determined using in situ
synchrotron X-ray powder diffraction multi-anvil experiments to 19 GPa,
with further preliminary results in the laser-heated diamond cell
reported to 60 GPa. The low-pressure MnP-structured phase transforms to
two different high-pressure phases depending on the temperature: the
ε-FeSi structure is stable at temperatures above ∼1100 K and a
previously reported distorted-CuTi structure (with Pmmn
symmetry) is stable at lower temperature. The invariant point is located
at 12.8 ± 0.2 GPa and 1100 ± 20 K. At higher pressures, ε
-FeSi-structured NiSi transforms to the CsCl structure with CsCl-NiSi as
the liquidus phase above 30 GPa. The Clapeyron slope of this transition
is -67 MPa/K. The phase boundary between the ε -FeSi and Pmmn
structured phases is nearly pressure independent implying there will be a
second sub-solidus invariant point between CsCl, ε -FeSi and Pmmn
structures at higher pressure than attained in this study. In addition
to these stable phases, the MnP structure was observed to spontaneously
transform at room temperature to a new orthorhombic structure (also with
Pnma symmetry) which had been detailed in previous ab initio simulations. This new phase of NiSi is shown here to be metastable.
Original language | English |
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Pages (from-to) | 196–206 |
Number of pages | 11 |
Journal | Physics of the Earth and Planetary Interiors |
Volume | 261 Part B |
Early online date | 14 Oct 2016 |
DOIs | |
Publication status | Published - Dec 2016 |
Research Groups and Themes
- PetrologyGroup
- PetrologyLabs
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Dive into the research topics of 'The phase diagram of NiSi under the conditions of small planetary interiors'. Together they form a unique fingerprint.Projects
- 1 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