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首页> 外文期刊>Rapid Communications in Mass Spectrometry: RCM >Determination of the triple oxygen and carbon isotopic composition of CO2 from atomic ion fragments formed in the ion source of the 253 Ultra high-resolution isotope ratio mass spectrometer
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Determination of the triple oxygen and carbon isotopic composition of CO2 from atomic ion fragments formed in the ion source of the 253 Ultra high-resolution isotope ratio mass spectrometer

机译:从253超高分辨率同位素比率质谱仪的离子源中形成的原子离子片段的三重氧和碳同位素组合物的测定

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Rationale Determination of delta O-17 values directly from CO2 with traditional gas source isotope ratio mass spectrometry is not possible due to isobaric interference of (COO)-C-13-O-16-O-16 on (COO)-C-12-O-17-O-16. The methods developed so far use either chemical conversion or isotope equilibration to determine the delta O-17 value of CO2. In addition, delta C-13 measurements require correction for the interference from (COO)-C-12-O-17-O-16 on (COO)-C-13-O-16-O-16 since it is not possible to resolve the two isotopologues. Methods We present a technique to determine the delta O-17, delta O-18 and delta C-13 values of CO2 from the fragment ions that are formed upon electron ionization in the ion source of the Thermo Scientific 253 Ultra high-resolution isotope ratio mass spectrometer (hereafter 253 Ultra). The new technique is compared with the CO2-O-2 exchange method and the O-17-correction algorithm for delta O-17 and delta C-13 values, respectively. Results The scale contractions for delta C-13 and delta O-18 values are slightly larger for fragment ion measurements than for molecular ion measurements. The delta O-17 and Delta O-17 values of CO2 can be measured on the O-17(+) fragment with an internal error that is a factor 1-2 above the counting statistics limit. The ultimate precision depends on the signal intensity and on the total time that the O-17(+) beam is monitored; a precision of 14 ppm (parts per million) (standard error of the mean) was achieved in 20 hours at the University of Gottingen. The Delta O-17 measurements with the O-fragment method agree with the CO2-O-2 exchange method over a range of Delta O-17 values of -0.3 to +0.7 parts per thousand. Conclusions Isotope measurements on atom fragment ions of CO2 can be used as an alternative method to determine the carbon and oxygen isotopic composition of CO2 without chemical processing or corrections for mass interferences.
机译:由于(COO)-C-13-O-16-O-16(COO)-C-12(COO)-C-12(COO)-C-12(COO)-C-12(COO)-C-12(COO)-C-12(COO)-C-12的异常干扰,不能测定具有传统气体源同位素比率的CO2的δO-17值的δO-17值的测定不可能-O-17-O-16。到目前为止所开发的方法使用化学转化或同位素平衡来确定CO2的δO-17值。此外,Delta C-13测量需要校正(COO)-C-12-O-17-O-16 ON(COO)-C-13-O-16-O-16的干扰,因为它是不可能的解决两种同位素。方法我们提出了一种方法来确定在热科学253超高分辨率同位素比的离子源上形成的电离中形成的片段离子的δO-17,ΔO-18和δc-13的δc-13值质谱仪(以下,253超)。将新技术与CO2-O-2 Exchange方法和ΔO-17和Delta C-13值的O-17校正算法进行比较。结果δC-13和Delta O-18值的比例收缩对于片段离子测量比分子离子测量略大。 CO2的Delta O-17和Delta O-17值可以在O-17(+)片段上,内部误差是计数统计限制的因子1-2。最终精度取决于信号强度,并监测O-17(+)光束的总时间;在Gottingen大学的20小时内实现了14ppm的精度(百万分之)(平均值的标准误差)。 ΔO-17测量与O形碎片方法的测量结果与CO2-O-2交换方法同意,在一系列-0.3至+0.7份的ΔO-17值范围内。结论CO2的原子片段离子的同位素测量可用作确定CO2的碳和氧同位素组成的替代方法,而无需化学加工或质量干扰的校正。

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