TC/EA-MS online determination of hydrogen isotope composition and water concentration in eclogitic garnet

被引:143
作者
Gong, Bing [1 ]
Zheng, Yong-Fei [1 ]
Chen, Ren-Xu [1 ]
机构
[1] Univ Sci & Technol China, CAS Key Lab Crust Mantle Mat & Environm, Sch Earth & Space Sci, Hefei 230026, Peoples R China
关键词
nominally anhydrous mineral; hydrous mineral; hydrogen isotopes; water concentration; analytical technique; NOMINALLY ANHYDROUS MINERALS; RATIO MASS-SPECTROMETRY; CONVERSION ELEMENTAL ANALYZER; PRESSURE METAMORPHIC ROCKS; OXYGEN-ISOTOPE; UPPER-MANTLE; SILICATE-GLASSES; UHP METAMORPHISM; FLUID INCLUSION; STABLE ISOTOPES;
D O I
10.1007/s00269-007-0184-4
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
A continuous flow method, by a combination of thermal conversion elemental analyzer (TC/EA) with isotope ratio mass spectrometry (MS), is presented for determination of both H isotope composition and H(2)O concentration of garnet from eclogite. Together with biotite NBS-30, the garnet was tested by preheating mineral grains at different temperatures. Preheating at 90 degrees C for 12 h was found to be capable of eliminating adsorption water on sample surface. This results in constant delta D values and total H(2)O contents for the garnet, with weighted means of -93 +/- 2 parts per thousand and 522 +/- 11 ppm (wt), respectively. The garnet that was preheated at 350 degrees C for 4 h also gave constant delta D values of -86 +/- 6 degrees and H(2)O contents of 281 +/- 13 ppm (wt). The latter result for the H(2)O contents agrees with the H(2)O contents 271 +/- 58 ppm (wt) measured by Fourier transform infrared spectroscopy for quantitative analysis of structural hydroxyl in the same garnet. Stepwise-heating TC/EA-MS analyses for the garnet show that the molecular H(2)O are depleted in D relative to the structural OH and has higher mobility than the structural OH. Therefore, the TC/EA-MS method can be used not only for quantitative determination of both H isotope composition and H(2)O concentration of hydrous and anhydrous minerals, but also for the concentration of structural hydroxyl after high-T dehydration.
引用
收藏
页码:687 / 698
页数:12
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