Science. 1964 Jul 31;145(3631):483-6. doi: 10.1126/science.145.3631.483.
An x-ray diffraction study of iron under pressure has shown that alpha-iron (body-centered cubic) transforms to hexagonal-close-packing (designated epsilon-iron) at 130 kb, room temperature. The volume change for the transformation is -0.20 +/- 0.03 cm2/ mole. The slope for the gamma-epsilon phase boundary has been calculated to be 2 +/- 1 degrees C/kb. The molar volume of iron decreases from 7.10 cm3/mole (density = 7.85 g/cm(3)) at room pressure to 6.10 +/- 0.08 cm(3)/mole (density = 9.1 +/- 0.1 g/cm(3)) at 200 kb and room temperature. The extrapolation of the gamma-epsilon phase boundary, consistent with shock wave data, suggests that it may have an influence on the properties of the earth's core.
一项关于铁在高压下的 X 射线衍射研究表明,α-铁(体心立方)在 130kb、室温下转变为六方密堆积(指定为ε-铁)。转变的体积变化为-0.20±0.03cm2/mol。γ-ε 相界的斜率已计算为 2±1°C/kb。铁的摩尔体积从室温下的 7.10cm3/mol(密度=7.85g/cm3)降低到 200kb 和室温下的 6.10±0.08cm3/mol(密度=9.1±0.1g/cm3)。γ-ε 相界的外推与激波数据一致,表明它可能对地球核心的性质有影响。