The equation of state for -Fe2SiO4 was determined by single-crystal X-ray diffraction up to 10.2 GPa at room temperature. The pressure–volume data, measured at 10 different pressures, do not show any evidence of a phase transformation and were fit by a third-order Birch–Murnaghan equation of state. The following coefficients were refined simultaneously: V0 = 559.44(6) ˚A3, KT0 = 187.3(1.7) GPa, and K = 5.5(4). This result implies that the Mg/Fe substitution along the -Fo–Fa join does not significantly affect the bulk modulus. The sample shows higher K than other compositions along the Fo–Fa join, which generally have K ∼4. Based on our results we can calculate the sound bulk velocity of -Fe2SiO4 up to the pressures of the Transition Zone. Due to the larger K of -Fe2SiO4, the difference in bulk sound velocity between the two end-members decreases with increasing pressure.
New accurate compression data for gamma-Fe2SiO4
NESTOLA, FABRIZIO;SECCO, LUCIANO;
2010
Abstract
The equation of state for -Fe2SiO4 was determined by single-crystal X-ray diffraction up to 10.2 GPa at room temperature. The pressure–volume data, measured at 10 different pressures, do not show any evidence of a phase transformation and were fit by a third-order Birch–Murnaghan equation of state. The following coefficients were refined simultaneously: V0 = 559.44(6) ˚A3, KT0 = 187.3(1.7) GPa, and K = 5.5(4). This result implies that the Mg/Fe substitution along the -Fo–Fa join does not significantly affect the bulk modulus. The sample shows higher K than other compositions along the Fo–Fa join, which generally have K ∼4. Based on our results we can calculate the sound bulk velocity of -Fe2SiO4 up to the pressures of the Transition Zone. Due to the larger K of -Fe2SiO4, the difference in bulk sound velocity between the two end-members decreases with increasing pressure.
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