Determination of the total oxygen isotopic composition of nitrate and the calibration of a Δ17O nitrate reference material

被引:94
作者
Michalski, G [1 ]
Savarino, J
Böhlke, JK
Thiemens, M
机构
[1] Univ Calif San Diego, Dept Chem & Biochem, La Jolla, CA 92093 USA
[2] Univ Grenoble 1, Lab Glaciol & Geophys Environm, F-38402 St Martin Dheres, France
[3] US Geol Survey, Natl Ctr 431, Reston, VA 20192 USA
关键词
D O I
10.1021/ac0256282
中图分类号
O65 [分析化学];
学科分类号
070302 ; 081704 ;
摘要
A thermal decomposition method was developed and tested for the simultaneous determination of delta(18)O and delta(17)O in nitrate. The thermal decomposition of AgNO3 allows for the rapid and accurate determination of O-18/ O-16 and O-17/O-16 isotopic ratios with a precision of +/-1.5parts per thousand for delta(18)O and +/-0.11parts per thousand for Delta(17)O (Delta(17)O = delta(17)O - 0.52 x delta(18)O). The international nitrate isotope reference material IAEA-NO3 yielded a delta(18)O value of +23.6parts per thousand and Delta(17)O of -0.2parts per thousand, consistent with normal terrestrial mass-dependent isotopic ratios. In contrast, a large sample of NaNO3 from the Atacama Desert Chile, was found to have Delta(17)O = 21.56 +/- 0.11parts per thousand and delta(18)O = 54.9 +/- 1.5parts per thousand, demonstrating a substantial mass-independent isotopic composition consistent with the proposed atmospheric origin of the desert nitrate. It is suggested that this sample (designated USGS-35) can be used to generate other gases (CO2, CO, N2O, O-2) with the same Delta(17)O to serve as measurement references for a variety of applications involving mass-independent isotopic compositions in environmental studies.
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页码:4989 / 4993
页数:5
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