Abstract
The additional work we have done using our new laser heating in the diamond anvil cell system since the publication of Andrault et al. (Phys Chem Mineral 47(2), 2020) leads us to the conclusion that there was a systematic bias in the determination of temperature. First, the temperature of the W-lamp used for the calibration of the optical system was overestimated by ~ 22 K at 2273 K. Then, we made the assumption that hot SiO2 was a grey-body (constant emissivity ε(λ)), while the available measurements suggest instead that ε(λ) of SiO2 is similar to that of tungsten. Applying these two corrections lowers the SiO2 melting temperatures significantly. In LMV, we performed a new experimental determination of the SiO2 melting temperature, at 5000 (200) K and ~ 70 (4) GPa, which is well compatible with the amplitude of the correction proposed. The reevaluation of the melting temperature profile does not affect largely the interpretations or the main conclusions presented in Andrault et al. (Phys Chem Mineral 47(2), 2020). Within the stability field of stishovite, the melting curve still presents a relatively sharp change of slope at P–T recalculated as ~ 40 GPa and ~ 4800 K. It is related to a change of the melt structure. At higher pressures, the melting curve is almost flat up to the subsolidus transition from stishovite to the CaCl2-form around 85 GPa, where the slope of the melting curve increases again up to ~ 120 GPa. We present corrected figures and tables of the original publication.
References
Akins JA, Ahrens TJ (2002) Dynamic compression of SiO2: a new interpretation. Geophys Res Lett 29(10):1394
Andrault D, Morard G, Garbarino G, Mezouar M, Bouhifd MA, Kawamoto T (2020) Melting behavior of SiO2 up to 120 GPa. Phys Chem Mineral 47(2):10
Belonoshko AB, Dubrovinsky LS (1995) Molecular-dynamics of stishovite melting. Geochim Cosmochim Acta 59(9):1883–1889
Devos JC (1954) A new determination of the emissivity of tungsten ribbon. Physica 20(9):690–700
Dubrovinsky LS, Saxena SK (1997) Thermal expansion of periclase (MgO) and tungsten (W) to melting temperatures. Phys Chem Mineral 24(8):547–550
Giampaoli R, Kantor I, Mezouar M, Boccato S, Rosa AD, Torchio R, Garbarino G, Mathon O, Pascarelli S (2018) Measurement of temperature in the laser heated diamond anvil cell: comparison between reflective and refractive optics. High Pressure Res 38(3):250–269
Holtgrewe N, Greenberg E, Prescher C, Prakapenka VB, Goncharov AF (2019) Advanced integrated optical spectroscopy system for diamond anvil cell studies at GSECARS. High Pressure Res 39(3):457–470
Keppler H, Dubrovinsky LS, Narygina O, Kantor IY (2008) Optical absorption and radiative thermal conductivity of silicate perovskite to 125 gigapascals. Science 322(5907):1529–1532
Larrabee RD (1959) Spectral emissivity of tungsten. J Opt Soc Am 49(6):619–625
Mezouar M et al (2005) Development of a new state-of-the-art beamline optimized for monochromatic single-crystal and powder X-ray diffraction under extreme conditions at the ESRF. J Synchr Rad 12:559–664
Miiller AP, Cezairliyan A (1990) Thermal-expansion of tungsten in the range 1500–3600-K by a transient interferometric-technique. Int J Thermophys 11(4):619–628
Richet P, Gillet P, Pierre A, Bouhifd MA, Daniel I, Fiquet G (1993) Raman spectroscopy, x-ray diffraction, and phase relationship determinations with a versatile heating cell for measurements up to 3600-K (or 2700-K in air). J Appl Phys 74(9):5451–5456
Schultz E et al (2005) Double-sided laser heating system for in situ high pressure-high temperature monochromatic X-ray diffraction at the ESRF. High Pressure Res 25(1):71–83
Shen G, Lazor P (1995) Measurement of melting temperatures of some minerals under lower mantle conditions. J Geophys Res 100(B9):17699–17713
Trukhin AN, Smits K, Sharakosky A, Chikvaidze G, Dyuzheva TI, Lityagina LM (2011) Luminescence of dense, octahedral structured crystalline silicon dioxide (stishovite). J Lumin 131(11):2273–2278
Usui Y, Tsuchiya T (2010) Ab initio two-phase molecular dynamics on the melting curve of SiO2. J Earth Sci 21(5):801–810
Acknowledgements
We thank P. Asimow, F. Datchi, N. Guignot, J.A. Hernandez, R. Pierru and G. Weck for fruitful discussions about temperature determination based on thermal emission spectra.
Author information
Authors and Affiliations
Corresponding author
Additional information
Publisher's Note
Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
Rights and permissions
About this article
Cite this article
Andrault, D., Pison, L., Morard, G. et al. Comment on: Melting behavior of SiO2 up to 120 GPa (Andrault et al. 2020). Phys Chem Minerals 49, 3 (2022). https://doi.org/10.1007/s00269-021-01174-2
Received:
Accepted:
Published:
DOI: https://doi.org/10.1007/s00269-021-01174-2