In situ Ultrasonic Velocity Measurements Across the Olivine-spinel Transformation in Fe2Si04
Compressional (P) and shear (S) wave velocities across the olivine-spinel transformation in Fe{sub 2}SiO{sub 4} were investigated in situ using combined synchrotron X-ray diffraction, X-ray imaging, and ultrasonic interferometry up to 5.5 GPa along the 1173 K isotherm. The onset of the spinel to olivine transformation at 4.5 GPa and olivine to spinel transition for Fe{sub 2}SiO{sub 4} at 4.8 GPa was concurrently observed from X-ray diffraction, the amplitude of the ultrasonic signals, the calculated velocities, and the ratio of P and S wave velocities (v{sub P}/v{sub S}). No velocity softening was observed prior to the fayalite to spinel transition. The velocity contrasts across the Fe{sub 2}SiO{sub 4} spinel to fayalite phase transition are derived directly from the measured velocities, which are 13 and 12% for P and S waves, respectively, together with a density contrast of 9.4%. A comparison with literature data indicates that the changes in compressional-wave velocity and density across the olivine-spinel transformation in Fe{sub 2}SiO{sub 4} are comparable to those with different iron concentrations in the (Mg,Fe){sub 2}SiO{sub 4} solid solution, whereas the shear wave velocity contrast decreases slightly with increasing iron concentration.
- Research Organization:
- Brookhaven National Laboratory (BNL) National Synchrotron Light Source
- Sponsoring Organization:
- DOE - OFFICE OF SCIENCE
- DOE Contract Number:
- AC02-98CH10886
- OSTI ID:
- 1019701
- Report Number(s):
- BNL--95547-2011-JA
- Journal Information:
- American Mineralogist, Journal Name: American Mineralogist Journal Issue: 7 Vol. 95; ISSN AMMIAY; ISSN 0003-004X
- Country of Publication:
- United States
- Language:
- English
Similar Records
Compressional and Shear Wave velocities of Fe2SiO4 Spinel at High Pressure and High Temperature
Surface energy of fayalite and its effect on Fe-Si-O oxygen buffers and the olivine-spinel transition
Tracking silica in Earth’s upper mantle using new sound velocity data for coesite to 5.8 GPa and 1073 K
Journal Article
·
Mon Dec 31 23:00:00 EST 2007
· High Pressure Research
·
OSTI ID:980075
Surface energy of fayalite and its effect on Fe-Si-O oxygen buffers and the olivine-spinel transition
Journal Article
·
Sun Sep 30 20:00:00 EDT 2018
· American Mineralogist
·
OSTI ID:1567001
Tracking silica in Earth’s upper mantle using new sound velocity data for coesite to 5.8 GPa and 1073 K
Journal Article
·
Fri Aug 11 20:00:00 EDT 2017
· Geophysical Research Letters
·
OSTI ID:1409631