Linear error propagation and Monte Carlo simulation for MC-ICP-MS neodymium isotope ratios uncertainty analysis

IF 2.7 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY
Solid Earth Sciences Pub Date : 2026-03-01 Epub Date: 2026-02-05 DOI:10.1016/j.sesci.2026.100287
Tianyu Zhang , Qichao Yang , Haiou Gu , Dongyong Li
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引用次数: 0

Abstract

This study presents a comprehensive framework for uncertainty estimation in Nd isotope ratio analysis using both linear error propagation and Monte Carlo simulation. The developed model explicitly incorporates uncertainties from key analytical procedures—including baseline subtraction, isobaric interference correction, and exponential law mass fractionation normalization—providing more accurate theoretical precision limits. For the internally normalized 143Nd/144Nd ratio, predicted cycle-level uncertainties show excellent agreement with measured values, validating the accuracy of both approaches. Evaluation of two interference correction strategies—the natural 147Sm/144Sm ratio method and the iterative method—reveals that both yield comparable uncertainties when 147Sm/144Nd is below ∼5 × 10−3. Uncertainty in Nd isotope ratios exhibits a strong inverse dependence on beam intensity, with Johnson noise dominating below a 144Nd intensity threshold of ∼0.2 V and counting statistics prevailing at higher intensities. This threshold offers a clear criterion for selecting a 1013 Ω amplifier resistor to improve precision in low-signal regimes. Furthermore, baseline correction is shown to introduce Johnson noise derived uncertainty, with a more pronounced effect at lower beam intensities; our results provide specific guidance on baseline cycle number needed to control this contribution under different signal conditions. Monte Carlo simulations demonstrate robust performance when using at least 5 × 104 cycles per simulation, achieving results within 1 % of linear propagation estimates while maintaining computational efficiency (∼1.5 s/simulation). External reproducibility is primarily governed by Johnson noise and counting statistics, with secondary factors such as mass bias variations in the mass spectrometer contributing ∼10 % to the total measured external uncertainty. Finally, we demonstrate that diluting sample solution increases analytical uncertainty, especially at lower sample amounts, despite longer measurement times, whereas concentrating sample solution improves precision provided sample consumption during signal stabilization is accounted for. These findings provide a practical foundation for optimizing precision in Nd isotope analysis via uncertainty model based experimental design.
MC-ICP-MS钕同位素比不确定度分析的线性误差传播和蒙特卡罗模拟
本文采用线性误差传播和蒙特卡罗模拟,提出了Nd同位素比分析中不确定性估计的综合框架。开发的模型明确地纳入了关键分析程序的不确定性-包括基线减法,等压干涉校正和指数律质量分馏归一化-提供了更准确的理论精度极限。对于内部归一化的143Nd/144Nd比值,预测的周期水平不确定度与实测值非常吻合,验证了两种方法的准确性。对两种干涉校正策略(自然147Sm/144Sm比值法和迭代法)的评估表明,当147Sm/144Nd低于~ 5 × 10−3时,这两种方法产生的不确定性相当。Nd同位素比率的不确定性与光束强度呈强烈的反比关系,Johnson噪声在144Nd强度阈值(~ 0.2 V)以下占主导地位,计数统计在更高强度下占主导地位。该阈值为选择1013 Ω放大电阻提供了明确的标准,以提高低信号状态下的精度。此外,基线校正被证明会引入约翰逊噪声衍生的不确定性,在较低的光束强度下影响更明显;我们的结果提供了在不同信号条件下控制这种贡献所需的基线周期数的具体指导。当每次模拟使用至少5 × 104个周期时,蒙特卡罗模拟显示出稳健的性能,在保持计算效率(~ 1.5 s/模拟)的同时,在1%的线性传播估计范围内实现结果。外部可重复性主要由约翰逊噪声和计数统计控制,次要因素如质谱仪中的质量偏差变化对测量的总外部不确定度贡献约10%。最后,我们证明,尽管测量时间较长,但稀释样品溶液会增加分析不确定度,特别是在样品数量较低时,而浓缩样品溶液可以提高精度,前提是考虑到信号稳定期间的样品消耗。这些发现为基于不确定模型的实验设计优化Nd同位素分析精度提供了实践基础。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Solid Earth Sciences
Solid Earth Sciences GEOSCIENCES, MULTIDISCIPLINARY-
CiteScore
3.60
自引率
5.00%
发文量
20
审稿时长
103 days
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