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采用高灵敏度锥结合激光烧蚀 MC-ICP-MS 中添加氮的方法,对硫化物和元素硫中的原位硫同位素(δ(34)S 和 δ(33)S)进行分析。

In situ sulfur isotopes (δ(34)S and δ(33)S) analyses in sulfides and elemental sulfur using high sensitivity cones combined with the addition of nitrogen by laser ablation MC-ICP-MS.

机构信息

State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, PR China.

State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, PR China; The Beijing SHRIMP Center, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 102206, PR China.

出版信息

Anal Chim Acta. 2016 Mar 10;911:14-26. doi: 10.1016/j.aca.2016.01.026. Epub 2016 Jan 27.

Abstract

The sulfur isotope is an important geochemical tracer in diverse fields of geosciences. In this study, the effects of three different cone combinations with the addition of N2 on the performance of in situ S isotope analyses were investigated in detail. The signal intensities of S isotopes were improved by a factor of 2.3 and 3.6 using the X skimmer cone combined with the standard sample cone or the Jet sample cone, respectively, compared with the standard arrangement (H skimmer cone combined with the standard sample cone). This signal enhancement is important for the improvement of the precision and accuracy of in situ S isotope analysis at high spatial resolution. Different cone combinations have a significant effect on the mass bias and mass bias stability for S isotopes. Poor precisions of S isotope ratios were obtained using the Jet and X cones combination at their corresponding optimum makeup gas flow when using Ar plasma only. The addition of 4-8 ml min(-1) nitrogen to the central gas flow in laser ablation MC-ICP-MS was found to significantly enlarge the mass bias stability zone at their corresponding optimum makeup gas flow in these three different cone combinations. The polyatomic interferences of OO, SH, OOH were also significantly reduced, and the interference free plateaus of sulfur isotopes became broader and flatter in the nitrogen mode (N2 = 4 ml min(-1)). However, the signal intensity of S was not increased by the addition of nitrogen in this study. The laser fluence and ablation mode had significant effects on sulfur isotope fractionation during the analysis of sulfides and elemental sulfur by laser ablation MC-ICP-MS. The matrix effect among different sulfides and elemental sulfur was observed, but could be significantly reduced by line scan ablation in preference to single spot ablation under the optimized fluence. It is recommended that the d90 values of the particles in pressed powder pellets for accurate and precise S isotope analysis should be less than 10 μm. Under the selected optimized analytical conditions, excellent agreements between the determined values and the reference values were achieved for the IAEA-S series standard reference materials and a set of six well-characterized, isotopic homogeneous sulfide standards (PPP-1, MoS2, MASS-1, P-GBW07267, P-GBW07268, P-GBW07270), validating the capability of the developed method for providing high-quality in situ S isotope data in sulfides and elemental sulfur.

摘要

硫同位素是地球科学各领域中一种重要的地球化学示踪剂。在这项研究中,详细研究了在添加 N2 的情况下,三种不同的锥组合对原位 S 同位素分析性能的影响。与标准排列(H 滑流锥与标准样品锥结合)相比,使用 X 滑流锥与标准样品锥或喷气样品锥的组合,分别将 S 同位素的信号强度提高了 2.3 倍和 3.6 倍。这种信号增强对于提高高空间分辨率下原位 S 同位素分析的精度和准确性非常重要。不同的锥组合对 S 同位素的质量偏差和质量偏差稳定性有显著影响。仅使用 Ar 等离子体时,在 Jet 和 X 锥组合的相应最佳化妆气流下,S 同位素比值的精密度较差。在激光烧蚀 MC-ICP-MS 中,向中央气体流中添加 4-8 ml min(-1) 的氮气,发现这三种不同锥组合在其相应最佳化妆气流下,显著扩大了质量偏差稳定性区域。OO、SH、OOH 的多原子干扰也显著降低,硫同位素的无干扰平台变得更宽更平(N2 = 4 ml min(-1))。然而,在这项研究中,氮气的添加并没有增加 S 的信号强度。激光强度和烧蚀模式对激光烧蚀 MC-ICP-MS 分析硫化物和单质硫时的硫同位素分馏有显著影响。观察到不同硫化物和单质硫之间的基质效应,但通过线扫描烧蚀可以显著降低这种效应,优于单点烧蚀。建议压片粉末样品中颗粒的 d90 值应小于 10 μm,以便进行准确和精确的 S 同位素分析。在选择的优化分析条件下,对 IAEA-S 系列标准参考物质和一套 6 个具有良好特征、同位素均匀的硫化物标准物质(PPP-1、MoS2、MASS-1、P-GBW07267、P-GBW07268、P-GBW07270)进行了测定,结果与参考值吻合良好,验证了该方法在硫化物和单质硫中提供高质量原位 S 同位素数据的能力。

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