U.S. Environmental Protection Agency, National Health and Environmental Effects Research Laboratory, 200 SW 35th Street, 97333, Corvallis, OR, USA.
Oecologia. 2001 Apr;127(2):171-179. doi: 10.1007/s004420000578. Epub 2001 Feb 21.
Stable isotope analyses are often used to quantify the contribution of multiple sources to a mixture, such as proportions of food sources in an animal's diet, or C3 and C4 plant inputs to soil organic carbon. Linear mixing models can be used to partition two sources with a single isotopic signature (e.g., δ(13)C) or three sources with a second isotopic signature (e.g., δ(15)N). Although variability of source and mixture signatures is often reported, confidence interval calculations for source proportions typically use only the mixture variability. We provide examples showing that omission of source variability can lead to underestimation of the variability of source proportion estimates. For both two- and three-source mixing models, we present formulas for calculating variances, standard errors (SE), and confidence intervals for source proportion estimates that account for the observed variability in the isotopic signatures for the sources as well as the mixture. We then performed sensitivity analyses to assess the relative importance of: (1) the isotopic signature difference between the sources, (2) isotopic signature standard deviations (SD) in the source and mixture populations, (3) sample size, (4) analytical SD, and (5) the evenness of the source proportions, for determining the variability (SE) of source proportion estimates. The proportion SEs varied inversely with the signature difference between sources, so doubling the source difference from 2‰ to 4‰ reduced the SEs by half. Source and mixture signature SDs had a substantial linear effect on source proportion SEs. However, the population variability of the sources and the mixture are fixed and the sampling error component can be changed only by increasing sample size. Source proportion SEs varied inversely with the square root of sample size, so an increase from 1 to 4 samples per population cut the SE in half. Analytical SD had little effect over the range examined since it was generally substantially smaller than the population SDs. Proportion SEs were minimized when sources were evenly divided, but increased only slightly as the proportions varied. The variance formulas provided will enable quantification of the precision of source proportion estimates. Graphs are provided to allow rapid assessment of possible combinations of source differences and source and mixture population SDs that will allow source proportion estimates with desired precision. In addition, an Excel spreadsheet to perform the calculations for the source proportions and their variances, SEs, and 95% confidence intervals for the two-source and three-source mixing models can be accessed at http://www.epa.gov/wed/pages/models.htm.
稳定同位素分析常用于量化混合物中多种来源的贡献,例如动物饮食中食物来源的比例,或 C3 和 C4 植物对土壤有机碳的输入。线性混合模型可用于划分具有单一同位素特征(例如 δ(13)C)的两个来源,或具有第二个同位素特征(例如 δ(15)N)的三个来源。尽管通常会报告源和混合物特征的可变性,但源比例的置信区间计算通常仅使用混合物的可变性。我们提供的示例表明,忽略源可变性可能导致对源比例估计值的可变性的低估。对于二源和三源混合模型,我们提供了用于计算方差、标准误差 (SE) 和源比例估计值置信区间的公式,这些公式考虑了源的同位素特征以及混合物中的可变性。然后,我们进行了敏感性分析,以评估以下因素的相对重要性:(1)源之间的同位素特征差异,(2)源和混合物群体中的同位素特征标准偏差 (SD),(3)样本量,(4)分析 SD,以及(5)源比例的均匀性,以确定源比例估计值的可变性 (SE)。比例 SE 与源之间的特征差异成反比,因此将源差异从 2‰增加到 4‰会将 SE 降低一半。源和混合物特征 SD 对源比例 SE 有很大的线性影响。然而,源和混合物的种群可变性是固定的,只能通过增加样本量来改变抽样误差分量。源比例 SE 与样本量的平方根成反比,因此从每个种群增加一个样本到四个样本,SE 减半。在检查的范围内,分析 SD 的影响很小,因为它通常远小于种群 SD。当源均匀分配时,比例 SE 最小,但当比例变化时,比例 SE 仅略有增加。提供的方差公式将能够量化源比例估计值的精度。提供的图表可快速评估源差异和源和混合物种群 SD 的可能组合,这些组合可实现具有所需精度的源比例估计值。此外,可以在 http://www.epa.gov/wed/pages/models.htm 访问用于执行两个源和三个源混合模型的源比例及其方差、SE 和 95%置信区间计算的 Excel 电子表格。