多接收器等离子体质谱(MC-ICP-MS)测定Mg同位素方法研究
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国家自然科学基金重点资助项目(40331005);国家自然科学 基金资助项目(40473039,40673047)


High-precision measurement of magnesium isotopes using MC-ICP-MS
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    摘要:

    采用“样品-标准”交叉技术,以纯Mg试剂、水样和矿物岩石样品作为实验材料,尝试建立高精度多接收器等离子体质谱(MC-ICP-MS)测定Mg同位素方法. 应用质谱仪上窄的进样狭缝,将来自Ar载气、空气和酸中的C2+、C2H+、C2H2+、CN+、NaH+等分子对Mg同位素的影响减至最小. 当标准Mg浓度为3×10-6时,保持样品与标准的浓度比在0.5~2之间,对Mg同位素比值测量没有影响. 大量实验表明,不同基质的行为各异:Na、Fe和Al的基质效应使δ25Mg和δ26Mg偏负;Ca的基质效应使δ25Mg和δ26Mg偏正;Cr的基质效应使δ25Mg和δ26Mg波动. 控制[元素]/[Mg]的浓度比在0.05范围内,可以忽略同质异位素的干扰和基质效应. 通过对本实验室的两个工作标准CAGS1-Mg和CAGS2-Mg的长期测量,估计出Mg同位素测量的外精度(2SD)对于δ26Mg可达0.180‰,对于δ25Mg可达0.090‰. 在25Mg/24Mg 对26Mg/24Mg的同位素比值图上,所有样品的Mg同位素值都落在斜率约0.5的质量分馏线上,意味着建立的 MC-ICP-MS测定Mg同位素方法既精确又无干扰. 相对于DSM3国际标准,样品的Mg同位素组成大致变化范围是δ26Mg值为2.790‰,δ25Mg值为 1.282‰. 其中,CAGS1 -Mg的δ26Mg值最大,为0.399‰,来自新疆喀纳斯湖水 的δ26Mg值最小,为-2.091‰.

    Abstract:

    A method for Mg isotope measurement using MC-ICP-MS has been set up. T he authors tried to make a high-precision analysis of magnesium isotopes by MC-ICP-MS for Mg reagent, waters and minerals. The "sample-standard" bracketing technique was used to correct spectrometer mass-dependent fractionation. By arranging narrow entry slit on MC-ICP-MS, the interferences of such molecules as C2+, C2H+, C2H2+, CN+ and NaH+ from Ar gas, air and acid can be decreased to the minimum. Keeping the concentration of samples the same as that of the standard is a good way to obtain high-precision Mg measurement. Through a lot of experiments on matrix element interference, matrix effects on Mg measurement can be realized. Keeping[element]/[Mg]concentration ratio lower than 0.05 can minimize isobaric interference and matrix effects. External repeatability (2SD) of Mg isotope measurement estimated by the authors' laboratory standard CAGS1-Mg relative to CAGS2-Mg is 0.180‰for δ26Mg and 0.090‰ for δ25Mg in a long period. The data in three 25Mg/24Mg versus 26Mg/24Mg plots all fall on the mass-dependent fractionation line with a slope of ~0.5. This means the method put forward by the authors is of high precision and suffers no interference. Relative to DSM3, Mg isotope composition of samples changes at 2.790‰ for δ26Mg and 1.282‰ for δ25Mg. 0.399‰ of δ26Mg from CAGS1-Mg is the maximum, whereas -2.091‰ of δ26Mg from Kanansi lake water is the minimum.

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何学贤,朱祥坤,李世珍,等, 2008. 多接收器等离子体质谱(MC-ICP-MS)测定Mg同位素方法研究[J]. 岩石矿物学杂志, 27(5):441~448.
HE Xue-xian, ZHU Xiang-kun, LI Shi-zhen, et al, 2008. High-precision measurement of magnesium isotopes using MC-ICP-MS[J]. Acta Petrologica et Mineralogica, 27(5): 441~448.

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