Wei Hai-Zhen, Jiang Shao-Yong, Hemming N Gary, Yang Jing-Hong, Yang Tao, Wu He-Pin, Yang Tang-Li, Yan Xiong, Pu Wei
State Key Laboratory for Mineral Deposits Research, Department of Earth Sciences, Nanjing University, Nanjing 210093, PR China.
State Key Laboratory for Mineral Deposits Research, Department of Earth Sciences, Nanjing University, Nanjing 210093, PR China; State Key Laboratory of Geological Processes and Mineral Resources, Faculty of Earth Resources, China University of Geosciences, Wuhan, Hubei 430074, PR China.
Talanta. 2014 Jun;123:151-60. doi: 10.1016/j.talanta.2014.02.009. Epub 2014 Feb 11.
In order to eliminate boron loss and potential isotopic fractionation during chemical pretreatment of natural samples with complex matrices, a three-column ion-exchange separation/purification procedure has been modified, which ensures more than 98% recovery of boron from each step for a wide range of sample matrices, and is applicable for boron isotope analysis by both TIMS and MC-ICP-MS. The PTIMS-Cs2BO2(+)-static double collection method was developed, ensuring simultaneous collection of (133)Cs2(11)B(16)O2(+)(m/z 309) and (133)Cs2(10)B(16)O2(+) (m/z 308) ions in adjacent H3-H4 Faraday cups with typical zoom optics parameters (Focus Quad: 15 V, Dispersion Quad: -85 V). The external reproducibilities of the measured (11)B/(10)B ratios of the NIST 951 boron standard solutions of 1000 ng, 100 ng and 10 ng of boron by PTIMS method are ±0.06‰, ±0.16‰ and ±0.25‰, respectively, which indicates excellent precision can be achieved for boron isotope measurement at nanogram level boron in natural samples. An on-peak zero blank correction procedure was employed to correct the residual boron signals effect in MC-ICP-MS, which gives consistent δ(11)B values with a mean of 39.66±0.35‰ for seawater in the whole range of boron content from 5 ppb to 200 ppb, ensuring accurate boron isotope analysis in few ppb boron. With the improved protocol, consistent results between TIMS and MC-ICP-MS data were obtained in typical geological materials within a wide span of δ(11)B values ranging from -25‰ to +40‰.
为了消除复杂基体天然样品化学预处理过程中的硼损失和潜在的同位素分馏,对一种三柱离子交换分离/纯化程序进行了改进,该程序可确保在广泛的样品基体中,每一步硼的回收率超过98%,适用于热电离质谱(TIMS)和多接收电感耦合等离子体质谱(MC-ICP-MS)的硼同位素分析。开发了PTIMS-Cs2BO2(+)-静态双收集方法,通过典型的变焦光学参数(聚焦四极杆:15 V,色散四极杆:-85 V),确保在相邻的H3-H4法拉第杯中同时收集(133)Cs2(11)B(16)O2(+)(m/z 309)和(133)Cs2(10)B(16)O2(+)(m/z 308)离子。采用PTIMS方法对1000 ng、100 ng和10 ng硼的NIST 951硼标准溶液测量的(11)B/(10)B比值的外部重现性分别为±0.06‰、±0.16‰和±0.25‰,这表明对于天然样品中纳克级硼的硼同位素测量可实现优异的精度。采用峰上零空白校正程序校正MC-ICP-MS中的残留硼信号效应,对于硼含量在5 ppb至200 ppb范围内的海水,给出的δ(11)B值一致,平均值为39.66±0.35‰,确保了对几ppb硼进行准确的硼同位素分析。通过改进的方案,在δ(11)B值范围从-25‰至+40‰的典型地质材料中,TIMS和MC-ICP-MS数据之间获得了一致的结果。