H at High Temperature
Updated 2/22/2020 by GR Rossman
1985
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1996 - Libowitzky E, Rossman GR (1996) FTIR spectroscopy of lawsonite between 82 and 325 K. American
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1997 - Libowitzky E, Rossman GR (1997) IR spectroscopy of
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1999 - Suzuki S, Nakashima S (1999) In-situ IR
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2007 - Zhang M, Salje EKH, Carpenter MA, Wang JY, Groat
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2010
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2011 - Yang X, Keppler H - In-situ infrared spectra of OH in olivine to 1100 C. American Mineralogist 96, 451-454
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2013 - Ingrin
J, Liu J, Depecker C, Kohn SC, Balan E, Grant KJ (2013) Low
temperature evolution of OH bands in synthetic forsterite, implication
for the nature of H defects at high pressure. Physics and Chemistry of Minerals 40, 499–510.
2014 - Yang X, Keppler H, Dubrovinsky L, Kurnosov A - In-situ infrared spectra
of hydroxyl in wadsleyite and ringwoodite at high pressure and high
temperature. American Mineralogist 99, 724-729
2015 - Yang Y, Xia Q, Zhang P (2015) Evolutions of OH groups in diopside and feldspars with temperature. European Journal of Mineralogy 27, 185–192.
2016 - Zhang M, Tarantino SC, Su W, Lou X, Ren
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OH vibrations, and structural modifications of phlogopite at high
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2019 - Yang Y, Ingrin J, Xia QK, Liu WD (2019)
Nature of hydrogen defects in clinopyroxenes from room temperature up
to 1000 °C: Implication for the preservation of hydrogen in the upper
mantle and impact on electricalconductivity. American Mineralogist 104, 79–93.
- Yang
Y, Liu W, Qi Z, Wang ZP, Smyth JR, Xia Q (2019) Re-configuration and
interaction of hydrogen sites in olivine at high temperature and high
pressure. American
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