Research output: Contribution to journal › Article › peer-review
New high-pressure phases of Fe7N3 and Fe7C3 stable at Earth's core conditions: evidences for carbon-nitrogen isomorphism in Fe-compounds. / Sagatov, Nursultan; Gavryushkin, Pavel N.; Inerbaev, Talgat M. et al.
In: RSC Advances, Vol. 9, No. 7, 29.01.2019, p. 3577-3581.Research output: Contribution to journal › Article › peer-review
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TY - JOUR
T1 - New high-pressure phases of Fe7N3 and Fe7C3 stable at Earth's core conditions: evidences for carbon-nitrogen isomorphism in Fe-compounds
AU - Sagatov, Nursultan
AU - Gavryushkin, Pavel N.
AU - Inerbaev, Talgat M.
AU - Litasov, Konstantin D.
N1 - We thank Prof Chris Pickard for his help with AIRSS code. We are grateful to the Supercomputer Center, Novosibirsk State University, for access to the resources of the cluster. This work was supported by the Russian Science Foundation (project no. 17-17-01177).
PY - 2019/1/29
Y1 - 2019/1/29
N2 - We carried out ab initio calculations on the crystal structure prediction and determination of P-T diagrams within the quasi-harmonic approximation for Fe7N3 and Fe7C3. Two new isostructural phases Fe7N3-C2/m and Fe7C3-C2/m which are dynamically and thermodynamically stable under the Earth's core conditions were predicted. The Fe7C3-C2/m phase stabilizes preferentially to the known h-Fe7C3 at 253-344 GPa in the temperature range of 0-5000 K, and the Fe7N3-C2/m stabilizes preferentially relative to the β-Fe7N3-at ∼305 GPa over the entire temperature range. This indicate that carbon and nitrogen can mutually coexist and replace each other in the Earth's and other planetary cores similarly to low pressure phases of the same compounds.
AB - We carried out ab initio calculations on the crystal structure prediction and determination of P-T diagrams within the quasi-harmonic approximation for Fe7N3 and Fe7C3. Two new isostructural phases Fe7N3-C2/m and Fe7C3-C2/m which are dynamically and thermodynamically stable under the Earth's core conditions were predicted. The Fe7C3-C2/m phase stabilizes preferentially to the known h-Fe7C3 at 253-344 GPa in the temperature range of 0-5000 K, and the Fe7N3-C2/m stabilizes preferentially relative to the β-Fe7N3-at ∼305 GPa over the entire temperature range. This indicate that carbon and nitrogen can mutually coexist and replace each other in the Earth's and other planetary cores similarly to low pressure phases of the same compounds.
KW - CRYSTAL-STRUCTURE PREDICTION
KW - TOTAL-ENERGY CALCULATIONS
KW - EQUATION-OF-STATE
KW - IRON NITRIDES
KW - CARBIDE
KW - GPA
UR - http://www.scopus.com/inward/record.url?scp=85061086894&partnerID=8YFLogxK
U2 - 10.1039/c8ra09942a
DO - 10.1039/c8ra09942a
M3 - Article
C2 - 35518092
AN - SCOPUS:85061086894
VL - 9
SP - 3577
EP - 3581
JO - RSC Advances
JF - RSC Advances
SN - 2046-2069
IS - 7
ER -
ID: 18488291