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The effect of ferromagnetism on the equation of state of Fe3C studied by first-principles calculations |
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| Authors: | Lidunka Vo?adlo John BrodholtDavid P Dobson KS Knight WG MarshallGDavid Price Ian G Wood |
| Institution: | a Department of Geological Sciences, University College London, Gower Street, London WC1E 6BT, UK b Bayerisches Geoinstitut, Universität Bayreuth, D-95440 Bayreuth, Germany c ISIS Facility, Rutherford Appleton Laboratory, Chilton, Didcot, Oxon OX11 0QX, UK d Department of Mineralogy, The Natural History Museum, Cromwell Road, London SW7 5BD, UK |
| Abstract: | First-principles calculations have been used to determine the equation of state of Fe3C in both its low-pressure magnetically ordered and high-pressure non-magnetically ordered states; at 0 K the ferromagnetic transition was found to occur at about 60 GPa. In the high pressure, non-magnetically ordered regime at 0 K the material may be described by a Birch-Murnaghan third-order equation of state with V0=8.968(7) Å3 per atom, K0=316.62(2) GPa and K′=4.30(2). At atmospheric pressure the ferromagnetic phase transition in Fe3C occurs at ∼483 K; preliminary measurements of the thermal expansion by powder neutron diffraction show that this transition produces a large effect on thermoelastic properties. The volumetric thermal expansion coefficient in the paramagnetic phase was found to be 4.34×10−5 K−1 at T∼550 K. By applying a thermal expansion correction to the calculated equation of state at 0 K, predicted values for the density and adiabatic incompressibility of this material at core pressures and temperatures were obtained. These results appear to be sufficiently different from seismological data so as to preclude Fe3C as the major inner core-forming phase. |
| Keywords: | carbides iron-rich composition equations of state magnetic properties inner core |
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