Crystal chemistry of FeO at high pressure and temperature
Crystal chemistry of FeO at high pressure and temperature
复制标题
高温高压下 Fe3O 的晶体化学
DOI:
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发表时间:
2014
期刊:
影响因子:
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通讯作者:
M. Schaefer
中科院分区:
文献类型:
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作者:
M. Dyar;M. Schaefer
AhstractThe phase relations and equations of state of Fe,O have been studied up to a pressure of 100 GPa and a temperature of 1100 K, using a high-temperature diamond-anvil cell combined with synchrotron x-ray diffraction. Under a hydrostatic environment, Fe.O transforms from the NaCl-type cubic structure (Bl) to a rhombohedral structure at 16 GPa and 300 K. The transition pressures increase as a function of temperature with a pressure-temperature slope of 0.070(±0.003) GPalK. No significant effect of non stoichiometry on the transition boundary was observed. The transition occurs at lower pressure under nonhydrostatic conditions. The rhombohedral phase increases its distortion with increasing pressure. Further distortions from the rhombohedral cell to a lower symmetry phase were observed at pressures above 40 GPa at room temperature. Upon heating at high pressure, the NiAs-type hexagonal phase (BS) forms at 90 GPa and 600 K. Least-squares fits of the hydrostatic compression data yielded the room-temperature bulk modulus K TO = 146(±2) GPa with its pressure derivative (8KTOI8P)T = 4 for the NaCI-type cubic phase (Bl). The effect of degree of nonstoichiometry on the bulk moduli is small, within the uncertainty of the experiments. Although the bulk modulus for the rhombohedral phase cannot be determined accurately, by comparing the structurally related interplanar d spacings it is evident that the rhombohedral phase is less compressible than the cubic phase. The bulk modulus and its pressure derivative for the NiAs-type hexagonal phase (BS), derived from the static compression data, are 172 GPa and 4.3 at 900 K, respectively.