Révész Kinga M, Landwehr Jurate M
U.S. Geological Survey, 431 National Center, Reston, VA 20192, USA.
Rapid Commun Mass Spectrom. 2002;16(22):2102-14. doi: 10.1002/rcm.833.
A new method was developed to analyze the stable carbon and oxygen isotope ratios of small samples (400 +/- 20 micro g) of calcium carbonate. This new method streamlines the classical phosphoric acid/calcium carbonate (H(3)PO(4)/CaCO(3)) reaction method by making use of a recently available Thermoquest-Finnigan GasBench II preparation device and a Delta Plus XL continuous flow isotope ratio mass spectrometer. Conditions for which the H(3)PO(4)/CaCO(3) reaction produced reproducible and accurate results with minimal error had to be determined. When the acid/carbonate reaction temperature was kept at 26 degrees C and the reaction time was between 24 and 54 h, the precision of the carbon and oxygen isotope ratios for pooled samples from three reference standard materials was </=0.1 and </=0.2 per mill or per thousand, respectively, although later analysis showed that materials from one specific standard required reaction time between 34 and 54 h for delta(18)O to achieve this level of precision. Aliquot screening methods were shown to further minimize the total error. The accuracy and precision of the new method were analyzed and confirmed by statistical analysis. The utility of the method was verified by analyzing calcite from Devils Hole, Nevada, for which isotope-ratio values had previously been obtained by the classical method. Devils Hole core DH-11 recently had been re-cut and re-sampled, and isotope-ratio values were obtained using the new method. The results were comparable with those obtained by the classical method with correlation = +0.96 for both isotope ratios. The consistency of the isotopic results is such that an alignment offset could be identified in the re-sampled core material, and two cutting errors that occurred during re-sampling then were confirmed independently. This result indicates that the new method is a viable alternative to the classical reaction method. In particular, the new method requires less sample material permitting finer resolution and allows automation of some processes resulting in considerable time savings.
开发了一种新方法来分析碳酸钙小样本(400±20微克)的稳定碳和氧同位素比率。这种新方法通过使用最近可用的赛默飞世尔科技-菲尼根气体预浓缩仪II制备装置和Delta Plus XL连续流同位素比率质谱仪,简化了经典的磷酸/碳酸钙(H₃PO₄/CaCO₃)反应方法。必须确定H₃PO₄/CaCO₃反应产生可重复且准确结果且误差最小的条件。当酸/碳酸盐反应温度保持在26℃且反应时间在24至54小时之间时,来自三种参考标准物质的合并样本的碳和氧同位素比率的精度分别≤0.1‰和≤0.2‰,不过后来的分析表明,来自一种特定标准的物质,其δ¹⁸O达到此精度水平所需的反应时间在34至54小时之间。等分试样筛选方法可进一步将总误差降至最低。通过统计分析对新方法的准确性和精度进行了分析和确认。通过分析内华达州魔鬼洞的方解石验证了该方法的实用性,此前已通过经典方法获得了其同位素比率值。魔鬼洞岩芯DH - 11最近进行了重新切割和重新采样,并使用新方法获得了同位素比率值。结果与通过经典方法获得的结果具有可比性,两种同位素比率的相关性均为+0.96。同位素结果的一致性使得能够在重新采样的岩芯材料中识别出校准偏移,随后独立确认了重新采样过程中发生的两个切割误差。这一结果表明,新方法是经典反应方法的可行替代方法。特别是,新方法所需的样本材料更少,允许更高的分辨率,并实现了一些过程的自动化,从而节省了大量时间。