Calibration of the infrared molar absorption coefficients for H in olivine, clinopyroxene and rhyolitic glass by elastic recoil detection analysis

被引:35
作者
Aubaud, Cyril [1 ]
Bureau, Helene [2 ]
Raepsaet, Caroline [2 ]
Khodja, Hicham [2 ]
Withers, Anthony C. [3 ]
Hirschmann, Marc M. [3 ]
Bell, David R. [4 ]
机构
[1] Inst Phys Globe, Lab Geochim Isotopes Stables, Equipe Physicochim Fluides Geol, UMR7154, F-75251 Paris 05, France
[2] CEA Saclay, UMR9956, CNRS, Lab Pierre Sue, F-91191 Gif Sur Yvette, France
[3] Univ Minnesota, Dept Geol & Geophys, Minneapolis, MN 55455 USA
[4] Arizona State Univ, Dept Chem & Biochem, Tempe, AZ 85282 USA
关键词
Water; Volcanic glasses; Nominally anhydrous minerals; Infrared spectroscopy; Elastic recoil detection analysis; NOMINALLY ANHYDROUS MINERALS; SILICATE-GLASSES; MANTLE OLIVINE; NUCLEAR MICROPROBE; WATER; OH; HYDROGEN; HYDROXYL; KIMBERLITE; PRESSURE;
D O I
10.1016/j.chemgeo.2009.01.001
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
We use a nuclear microbeam technique (Elastic Recoil Detection Analysis or ERDA) to measure the H content in 2 rhyolitic glasses, 4 olivines, 4 orthopyroxenes, and 7 clinopyroxenes. These samples have been characterized previously for their CH absorption spectra by infrared (FTIR) spectroscopy. We use ERDA and FTIR data to calibrate the infrared molar absorption coefficients. The blank level of the ERDA method is 102 +/- 81 ppm H2O, too great for the analysis of many natural nominally anhydrous minerals (NAMs) from the upper mantle, but applicable to H-rich glasses, natural and synthetic NAMs. Calibration of the molar absorption coefficient epsilon with the ERDA results gives 95 +/- 81 mol(-1) cm(-1) for rhyolitic glasses (peak height), 34,515 +/- 7050 l mol(-1) cm(-2) for olivine and 46,103 +/- 5300 l mol(-1) cm(-2) for clinopyroxene (integrated area). The olivine calibration of the present study is intermediate between that of Bell et al. [Bell, D.R., Rossman, G.R., Maldener, J., Endisch, D. and Rauch, F, 2003. Hydroxide in olivine: a quantitative determination of the absolute amount and calibration of the IR spectrum. journal of Geophysical Research, 108(132). doi:10.1029/2001JB000679] and that of Libowitzky and Rossman [Libowitzky, E. and Rossman, G.R., 1997. An IR absorption calibration for water in minerals. American Mineralogist, 82: 1111-1115]. For clinopyroxene, the best agreement with the ERDA data is obtained for the Libowitzky and Rossman [Libowitzky, E. and Rossman, G.R., 1997. An IR absorption calibration for water in minerals. American Mineralogist, 82: 1111-1115] calibration (5% lower than the ERDA data). The present calibration also confirms that the Paterson [Paterson, M.S., 1982. The determination of hydroxyl by infrared absorption in quartz, silicate glasses and similar materials. Bulletin de Mineralogie, 105: 20-29] calibration systematically underestimates the CH content in olivine. (C) 2009 Elsevier B.V. All rights reserved.
引用
收藏
页码:78 / 86
页数:9
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