Standard-sample bracketing calibration method combined with Mg as an internal standard for silicon isotopic compositions using multi-collector inductively coupled plasma mass spectrometry

被引:0
作者
Honglin Yuan [1 ]
Cheng Cheng [1 ]
Kaiyun Chen [1 ]
Zhian Bao [1 ]
机构
[1] State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Collaborative Innovation Center of Continental Tectonics
基金
中国国家自然科学基金;
关键词
Si isotope; Mg internal standard; MC-ICPMS; Rock samples; High resolution;
D O I
暂无
中图分类号
P597 [同位素地质学与地质年代学];
学科分类号
070902 ;
摘要
Silicon isotope analysis traditionally uses a standard-sample bracketing(SSB) method that relies upon greater instrument stability than can be consistently expected. The following proposed method reduces the level of instrumental stability required for the analysis process and provides a valid solution for high-precision and accurate studies of Si isotopic compositions. Rock samples were dissolved by using alkali fusion and acidification.Silicon isotopes were purified with an ion exchange resin.Interfering peaks for isotopes were separated by using a Nu Plasma 1700 multi-collector inductively coupled plasma mass spectrometry(MS) system in high-resolution mode(M/DM [ 8000 RP). Two magnesium isotopes(Mg andMg) and three silicon isotopes(Si,Si, andSi) were analyzed in the same data collection cycle. Mg isotopes were used as an internal standard to calibrate the mass discrimination effects in MS analysis of Si isotopes in combination with the SSB method in order to reduce the effects of MS interference and instrumental mass discrimination on the accuracy of measurements. The conventional SSB method without the Mg internal standard and the proposed SSB method with Mg calibration delivered consistent results within two standard deviations.When Mg was used as an internal standard for calibration,the analysis precision was better than 0.05 % amu.
引用
收藏
页码:421 / 427
页数:7
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