Triple oxygen isotope analysis of nitrate using the denitrifier method and thermal decomposition of N2O

被引:200
作者
Kaiser, Jan
Hastings, Meredith G.
Houlton, Benjamin Z.
Roeckmann, Thomas
Sigman, Daniel M.
机构
[1] Princeton Univ, Dept Geosci, Princeton, NJ 08544 USA
[2] Max Planck Inst Nucl Phys, Atmospher Phys Div, D-69117 Heidelberg, Germany
基金
英国自然环境研究理事会;
关键词
D O I
10.1021/ac061022s
中图分类号
O65 [分析化学];
学科分类号
070302 ; 081704 ;
摘要
Interaction with ozone transfers its anomalous (non-mass-dependent) O-17 enrichment to atmospheric nitrogen oxides and nitrate. The O-17 anomaly (Delta O-17) in nitrate can be used to identify atmospheric nitrate inputs into terrestrial and aquatic environments as well as to study the role of ozone in the atmosphere's reactive nitrogen cycle. We report here on an online method for analysis of the O-17 anomaly, using a strain of denitrifiers to convert nitrate to N2O, which decomposes quantitatively to N-2 and O-2 in a gold furnace at 800 degrees C, followed by gas chromatographic separation and isotope analysis of O-2. This method requires similar to 50 nmol of nitrate, 2-3 orders of magnitude less than previous offline thermal decomposition methods to achieve a similar analytical precision of 0.5% for Delta O-17. There is no significant memory effect, but calibration via nitrate or N2O reference materials is required for scale normalization. The N2O decomposition method is shown to be well-suited for nitrate analysis in freshwater and seawater samples from various environments.
引用
收藏
页码:599 / 607
页数:9
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