首页|改进的法拉第杯结构及其在富稀土元素磷灰石激光原位Sr同位素分析中的应用

改进的法拉第杯结构及其在富稀土元素磷灰石激光原位Sr同位素分析中的应用

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稀土元素二价离子(REE2+)干扰校正是激光原位Sr同位素分析的难点.本研究将一种改进的MC-ICP-MS法拉第杯结构(能同步接收REE2+)与常规的干扰信号扣除法(RPSM)相结合,创新性实现了 REE2+干扰的准确校正.系统评估了改进的法拉第杯结构(IFCC)对REE2+信号同步性以及比值(r:166,168,170Er2+/167Er2+和170,172,174,176Yb2+/173Yb2+)的影响.在IFCC上没有观察到REE2+信号之间的脱耦现象,表明IFCC适合与RPSM结合用于REE2+干扰校正;REE2+信号比值(r)与Er和Yb的天然同位素丰度比值(R:166,168,170Er/167Er和170,172,174,176Yb/173Yb)近似相等(r/R≈1),指示在一定条件下可以使用R和测量的167Er2+和173Yb2+信号准确计算出166,168,170Er2+和170,172,174,176Yb2+信号强度,进而实现REE2+干扰校正.加标溶液的Sr同位素SN-MC-ICP-MS分析结果表明,与IFCC结合,常规的干扰信号扣除法(RPSM,使用R做干扰校正系数)可有效校正Sr/Er≥3样品中的REE2+干扰,而增强的干扰信号扣除法(EPSM,使用测量的REE2+信号比值做干扰校正系数)可有效校正Sr/Er≥ 1样品中的REE2+干扰.应用IFCC,使用LA-MC-ICP-MS对两个富稀土元素磷灰石标准物质Durango(Sr/Er=7.4)和 UWA-1(Sr/Er=2.8)进行了 Sr 同位素组成分析,87Sr/86Sr 的测定值分别为 0.706 27±0.000 14(2SD,n=19)和0.704 76±0.000 19(2SD,n=20),与报道的TIMS或MC-ICP-MS测定值在误差范围内一致,证实了该方法的可靠性.
An Improved Faraday Cup Configuration and Its Applying in Sr Isotopic Analysis of Rich-REE Apatite by LA-MC-ICP-MS
It is still difficult to accurately correct the interferences of REE2+in Sr isotopic analysis by LA-MC-ICP-MS.In this study,we corrected the interferences of REE2+by RPSM(Routine Peak Stripping Method)combining use of an improved cup configuration of MC-ICP-MS allowing for synchronic detection of REE2+signals.The effectiveness of IFCC(Improved Faraday Cup Configuration)was evaluated with respect to both the synchrony and the ratios of REE2+signals.With IFCC,no decoupling of REE2+signals was observed.This finding indicates that IFCC is well suited for RPSM to correct the interferences of REE2+.The ratios of REE2+signals(r:166,168,170Er2+/167Er2+和 170,172,174,176Yb2+/173Yb2+)are approximately equal to(r/R≈1)the natural isotopic abundant ratios of Er an Yb(R:166,168,170Er/167Er 和 170,172,174,176Yb/173Yb).This property cause IFCC to be well suited to correct interferences of REE2+with the R and the measured signals of 167Er2+and 173Yb2+.We also determined the Sr isotopic compositions of the Er and Yb-spiked 0.1 μg/g NBS987 Sr solutions by SN-MC-ICP-MS with IFCC,and the results attest that the interferences of REE2+in the solutions with Sr/Er≥3 can be corrected using the RPSM(R as the interference correction factor),and those in the solutions with Sr/Er≥1 can be corrected using the EPSM(Enhanced Peak Stripping Method,measured r as the interference correction factor).Sr isotopic compositions of two rich-REE reference materials(Durango with Sr/Er=7.4,and UWA-1 with Sr/Er=2.8)were determined by LA-MC-ICP-MS with IFCC,and the determined 87Sr/86Sr of the two reference materials are 0.706 27±0.000 14(2SD,n=19)and 0.704 76±0.000 19(2SD,n=20),respectively,both of which agree with previously published values(determined by TIMS or MC-ICP-MS)within uncertainties.

SrisotopesLA-MC-ICP-MSdouble-charged ions of rare earth elements(REE2+)apatitegeochemistry

童喜润、李小丹、邱啸飞、蔺洁、卢山松

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中国地质调查局武汉地质调查中心,湖北武汉 430205

中国地质调查局花岗岩成岩成矿地质研究中心,湖北武汉 430205

中国地质大学地球科学学院,地质过程与矿产资源国家重点实验室,湖北武汉 430074

Sr 同位素 LA-MC-ICP-MS 稀土元素二价离子 磷灰石 地球化学

2024

地球科学
中国地质大学

地球科学

CSTPCD北大核心
影响因子:1.447
ISSN:1000-2383
年,卷(期):2024.49(11)