An infrared spectroscopic study of the OH stretching frequencies of talc and 10-A phase to 10 GPa

被引:32
作者
Parry, Stephen A.
Pawley, Alison R.
Jones, Ray L.
Clark, Simon M.
机构
[1] Univ Manchester, Sch Earth Atmospher & Environm Sci, Manchester M13 9PL, Lancs, England
[2] Daresbury Lab, Warrington WA4 4AD, Cheshire, England
[3] Lawrence Berkeley Natl Lab, Adv Light Source, Berkeley, CA 94720 USA
关键词
talc; 10-A phase; high-pressure studies; IR spectroscopy;
D O I
10.2138/am.2007.2211
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The effects of pressure on the OH stretching frequencies of natural talc and two samples of synthetic 10-angstrom phase have been measured using a diamond-anvil cell and a synchrotron infrared source. The 10-A phase was synthesized at 6.0-6.5 GPa, 600 degrees C for 46 hours (sample 10 angstrom-46) and 160 hours (10 angstrom-160). Spectra were collected up to 9.0 GPa (talc), 9.9 GPa (10 angstrom-46), and 9.6 GPa (10 angstrom-160). The OH stretching vibration of Mg3OH groups in talc occurs at 3677 cm(-1) at ambient pressure, and increases linearly with pressure at 0.97(2) cm(-1) GPa(-1). The same vibration occurs in 10-angstrom phase, but shows negligible pressure shift up to 2 GPa, above which the frequency increases linearly to the maximum pressure studied, at a rate of 0.96(3) cm(-1) GPa(-1) (10 angstrom-46) and 0.87(3) cm(-1) GPa(-1) (10 angstrom-160). Two other prominent bands in the 10-angstrom phase spectrum are suggested to be due to stretching of interlayer H2O, hydrogen-bonded to the nearest tetrahedral sheet. These bands also show little change over the first 2 GPa of compression, as most of the compression of the structure is taken up by closing non-hydrogen bonded gaps between interlayer H2O and tetrahedral sheets. Between 2 and 4 GPa, changes in band intensities suggest a rearrangement of the interlayer H2O.
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页码:525 / 531
页数:7
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