Experimental study of the bcc-fcc phase transformations in the Fe-rich system Fe-Si at high pressures |
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Authors: | J. Zhang F. Guyot |
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Affiliation: | (1) CHiPR and Department of Geosciences, State University of New York at Stony Brook, Stony Brook, NY 11794, USA e-mail: zhang@sbmp04.ess.sunysb.edu, US;(2) Laboratoire de Mineralogie-Crystallographie and IPGP, Tour 16, Case 115, 4 Place Jussieu, F-75252 Paris Cedex 05, France, FR |
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Abstract: | In situ X-ray diffraction experiments at high pressure were carried out up to 8.9 GPa and 1100 °C to study phase transformations of iron and two iron-silicon alloys Fe0.91Si0.09 and Fe0.83Si0.17. For iron, the transformation from the bcc phase to the fcc phase was observed at pressures 3.8–8.2 GPa and temperatures that are consistent with previous in situ X-ray diffraction studies. Reversal of the transformation of iron was found to be sensitive to temperature; hysteresis of the transformation increased from 25 °C at 3.8 GPa to 100 °C at 7.0 GPa, primarily because the bcc-fcc phase boundary has a negative Clayperon slope. In the binary system Fe-Si, the observations of the present study indicate that the ferrite (bcc phase)-stabilizing behavior of silicon persists at high pressures and that the maximum solubility of silicon in the fcc phase increases with increasing pressure: (1) the transformation from the bcc phase to the fcc phase was observed in Fe0.91Si0.09 at 6.0, 7.4 and 8.9 GPa and the temperatures measured at the onset of the transformations were 300 °C higher than those in iron at similar pressures, (2) the transformation rate in Fe0.91Si0.09 was extremely sluggish compared to that of iron, and (3) the bcc-fcc phase transformation was not observed in Fe0.91Si0.09 at 4.7 GPa up to 1000 °C and in Fe0.83Si0.17 at 8.2 GPa and 1100 °C. Received: 1 June 1998 / Revised, accepted: 9 October 1998 |
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Keywords: | Iron Fe-Si alloys X-ray diffraction Phase transformation |
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