Beryl-II, a high-pressure phase of beryl: Raman and luminescence spectroscopy to 16.4 GPa
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作者:
O'Bannon, Earl, III
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Univ Calif Santa Cruz, Dept Earth & Planetary Sci, 1156 High St, Santa Cruz, CA 95064 USAUniv Calif Santa Cruz, Dept Earth & Planetary Sci, 1156 High St, Santa Cruz, CA 95064 USA
O'Bannon, Earl, III
[1
]
Williams, Quentin
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Univ Calif Santa Cruz, Dept Earth & Planetary Sci, 1156 High St, Santa Cruz, CA 95064 USAUniv Calif Santa Cruz, Dept Earth & Planetary Sci, 1156 High St, Santa Cruz, CA 95064 USA
Williams, Quentin
[1
]
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[1] Univ Calif Santa Cruz, Dept Earth & Planetary Sci, 1156 High St, Santa Cruz, CA 95064 USA
The Raman and Cr3+ and V2+ luminescence spectra of beryl and emerald have been characterized up to 15.0 and 16.4 GPa, respectively. The Raman spectra show that an E (1g) symmetry mode at 138 cm(-1) shifts negatively by -4.57 (+/- 0.55) cm(-1)/GPa, and an extrapolation of the pressure dependence of this mode indicates that a soft-mode transition should occur near 12 GPa. Such a transition is in accord with prior theoretical results. Dramatic changes in Raman mode intensities and positions occur between 11.2 and 15.0 GPa. These changes are indicative of a phase transition that primarily involves tilting and mild distortion of the Si6O18 rings. New Raman modes are not observed in the high-pressure phase, which indicates that the local bonding environment is not altered dramatically across the transition (e.g., changes in coordination do not occur). Both sharp line and broadband luminescence are observed for both Cr3+ and V2+ in emerald under compression to 16.4 GPa. The R-lines of both Cr3+ and V2+ shift to lower energy (longer wavelength) under compression. Both R-lines of Cr3+ split at similar to 13.7 GPa, and the V2+ R-1 slope changes at this pressure and shifts more rapidly up to similar to 16.4 GPa. The Cr3+ R-line splitting and FWHM show more complex behavior, but also shift in behavior at similar to 13.7 GPa. These changes in the pressure dependency of the Cr3+ and V2+ R-lines and the changes in R-line splitting and FWHM at similar to 13.7 GPa further demonstrate that a phase transition occurs at this pressure, in good agreement with our Raman results. The high-pressure phase of beryl appears to have two Al sites that become more regular under compression. Hysteresis is not observed in our Raman or luminescence spectra on decompression, suggesting that this transition is second order in nature: The occurrence of a second-order transition near this pressure is also in accord with prior theoretical results. We speculate that the high-pressure phase (beryl-II) might be a mildly modulated structure, and/or that extensive twinning occurs across this transition.
机构:
Sichuan Univ, Inst Atom & Mol Phys, Chengdu 610065, Peoples R China
Ehime Univ, Geodynam Res Ctr, Matsuyama, Ehime 7908577, JapanSichuan Univ, Inst Atom & Mol Phys, Chengdu 610065, Peoples R China
Lei, Li
Ohfuji, Hiroaki
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Ehime Univ, Geodynam Res Ctr, Matsuyama, Ehime 7908577, JapanSichuan Univ, Inst Atom & Mol Phys, Chengdu 610065, Peoples R China
Ohfuji, Hiroaki
Qin, Jiaqian
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Ehime Univ, Geodynam Res Ctr, Matsuyama, Ehime 7908577, Japan
Chulalongkorn Univ, Met & Mat Sci Res Inst, Bangkok 10330, ThailandSichuan Univ, Inst Atom & Mol Phys, Chengdu 610065, Peoples R China
Qin, Jiaqian
Zhang, Xinyu
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Yanshan Univ, State Key Lab Metastable Mat Sci & Technol, Qinhuangdao 066004, Peoples R ChinaSichuan Univ, Inst Atom & Mol Phys, Chengdu 610065, Peoples R China
Zhang, Xinyu
Wang, Fulong
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Ehime Univ, Geodynam Res Ctr, Matsuyama, Ehime 7908577, JapanSichuan Univ, Inst Atom & Mol Phys, Chengdu 610065, Peoples R China
Wang, Fulong
Irifune, Tetsuo
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Ehime Univ, Geodynam Res Ctr, Matsuyama, Ehime 7908577, JapanSichuan Univ, Inst Atom & Mol Phys, Chengdu 610065, Peoples R China
机构:
Chinese Acad Sci, Inst Geochem, Key Lab High Temp & High Pressure Study Earths Int, Guiyang, Peoples R China
Univ Chinese Acad Sci, Beijing, Peoples R ChinaChinese Acad Sci, Inst Geochem, Key Lab High Temp & High Pressure Study Earths Int, Guiyang, Peoples R China
Hong, Meiling
Dai, Lidong
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Chinese Acad Sci, Inst Geochem, Key Lab High Temp & High Pressure Study Earths Int, Guiyang, Peoples R ChinaChinese Acad Sci, Inst Geochem, Key Lab High Temp & High Pressure Study Earths Int, Guiyang, Peoples R China
Dai, Lidong
Hu, Haiying
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Chinese Acad Sci, Inst Geochem, Key Lab High Temp & High Pressure Study Earths Int, Guiyang, Peoples R ChinaChinese Acad Sci, Inst Geochem, Key Lab High Temp & High Pressure Study Earths Int, Guiyang, Peoples R China
Hu, Haiying
Zhang, Xinyu
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Chinese Acad Sci, Inst Geochem, Key Lab High Temp & High Pressure Study Earths Int, Guiyang, Peoples R China
Univ Chinese Acad Sci, Beijing, Peoples R ChinaChinese Acad Sci, Inst Geochem, Key Lab High Temp & High Pressure Study Earths Int, Guiyang, Peoples R China
Zhang, Xinyu
Li, Chuang
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Chinese Acad Sci, Inst Geochem, Key Lab High Temp & High Pressure Study Earths Int, Guiyang, Peoples R China
Univ Chinese Acad Sci, Beijing, Peoples R ChinaChinese Acad Sci, Inst Geochem, Key Lab High Temp & High Pressure Study Earths Int, Guiyang, Peoples R China
机构:
Univ Calif Santa Cruz, Dept Earth & Planetary Sci, Santa Cruz, CA 95064 USAUniv Calif Santa Cruz, Dept Earth & Planetary Sci, Santa Cruz, CA 95064 USA
Vennari, Cara E.
Williams, Quentin
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Univ Calif Santa Cruz, Dept Earth & Planetary Sci, Santa Cruz, CA 95064 USAUniv Calif Santa Cruz, Dept Earth & Planetary Sci, Santa Cruz, CA 95064 USA